def run_post(conf):
FIXdir = conf.get("DEFAULT","FIXbwrf")
sfc_switch = conf.getint("post","plot_sfc")
cloud_switch = conf.getint("post","plot_clouds")
sfcdiags_switch = conf.getint("post","plot_sfcdiags")
xcdiags_switch = conf.getint("post","plot_xcdiags")
switch_700mb = conf.getint("post","plot_700mb")
switch_500mb = conf.getint("post","plot_500mb")
switch_300mb = conf.getint("post","plot_300mb")
# sfc_switch = 0
# cloud_switch = 0
# sfcdiags_switch = 0
# xcdiags_switch = 0
# switch_700mb = 0
# switch_500mb = 0
# switch_300mb = 0
blat = conf.getfloat("post","blat")
blon = conf.getfloat("post","blon")
dx = conf.getfloat("wrf","dx")
POSTwork = conf.get("DEFAULT","POSTwork")
os.chdir(POSTwork)
file_wrf = glob.glob("wrfout*")[0]
print("Processing "+file_wrf)
init_time = file_wrf[11:21]+" "+file_wrf[22:24]+"Z"
# Download the states and coastlines
states = cfeature.NaturalEarthFeature(category='cultural', scale='50m', facecolor='none',
name='admin_1_states_provinces_shp')
# Get counties.
reader = shpreader.Reader(FIXdir+'/shapefiles/countyp010g.shp')
counties = list(reader.geometries())
COUNTIES = cfeature.ShapelyFeature(counties, crs.PlateCarree())
# Open the NetCDF file
ncfile = Dataset(file_wrf)
# Get the times and convert to datetimes
times = getvar(ncfile, "Times", timeidx=ALL_TIMES, meta=False)
dtimes = [datetime.strptime(str(atime), '%Y-%m-%dT%H:%M:%S.000000000') for atime in times]
numTimes = len(times)
# Reflectivity
ref = getvar(ncfile, "REFL_10CM", timeidx=ALL_TIMES)
ref[0,0,0,0]=-21.0 # hack to plot a blank contour plot at the initial time
# Get upper-air quantities.
p = getvar(ncfile, "pressure", timeidx=ALL_TIMES)
z = getvar(ncfile, "z", units="dm", timeidx=ALL_TIMES)
u, v = getvar(ncfile, "uvmet", units="kt", timeidx=ALL_TIMES, meta=False)
w = getvar(ncfile, "wa", units="m s-1", timeidx=ALL_TIMES)*100. # m/s to cm/s
rh = getvar(ncfile, "rh", timeidx=ALL_TIMES)
wspeed = (u**2.0+v**2.0)**0.5
tc = getvar(ncfile, "tc", timeidx=ALL_TIMES)
dewT = getvar(ncfile, "td", units="degC", timeidx=ALL_TIMES)
cloudfrac = getvar(ncfile, "cloudfrac", low_thresh=20.,
mid_thresh=955., high_thresh=4500., timeidx=ALL_TIMES)
total_cloudfrac=np.max(cloudfrac,axis=0)
low_cloudfrac = cloudfrac[0,:,:,:]
mid_cloudfrac = cloudfrac[1,:,:,:]
high_cloudfrac = cloudfrac[2,:,:,:]
# Interpolate
z_500 = smooth2d(interplevel(z, p, 500), 3)
tc_500 = smooth2d(interplevel(tc, p, 500), 3)
u_500 = interplevel(u, p, 500)
v_500 = interplevel(v, p, 500)
wspeed_500 = interplevel(wspeed, p, 500)
z_300 = smooth2d(interplevel(z, p, 300), 3)
u_300 = interplevel(u, p, 300)
v_300 = interplevel(v, p, 300)
z_700 = interplevel(z, p, 700)
tc_700 = interplevel(tc, p, 700)
u_700 = interplevel(u, p, 700)
v_700 = interplevel(v, p, 700)
w_700 = interplevel(w, p, 700)
rh_700 = interplevel(rh, p, 700)
if switch_700mb == 1:
# Interpolate over NaNs.
for itime in range(numTimes):
z_700[itime,:,:] = interpnan(z_700[itime,:,:])
tc_700[itime,:,:] = interpnan(tc_700[itime,:,:])
rh_700[itime,:,:] = interpnan(rh_700[itime,:,:])
u_700[itime,:,:] = interpnan(u_700[itime,:,:])
v_700[itime,:,:] = interpnan(v_700[itime,:,:])
w_700[itime,:,:] = interpnan(w_700[itime,:,:])
z_700 = smooth2d(z_700, 3)
tc_700 = smooth2d(tc_700, 3)
w_700 = smooth2d(w_700, 3)
div_300 = smooth2d(divergence([u_300*0.514444, v_300*0.514444], dx), 3) # kt to m/s
# Get the sea level pressure
slp = getvar(ncfile, "slp", timeidx=ALL_TIMES)
# Get the wet bulb temperature
twb = getvar(ncfile, "twb", units="degC", timeidx=ALL_TIMES)
slp_levels=np.arange(980,1040,2)
z_levels=np.arange(504,620,3)
z_levels_300=np.arange(804,996,6)
z_levels_700=np.arange(285,351,3)
t2_levels=np.arange(-20,125,5)
tc_levels=np.arange(-40,30,2)
wspeed_levels=np.arange(40,150,10)
ref_levels=np.arange(-20,60,5)
rh_levels=np.arange(70,105,5)
cldfrac_levels=np.arange(0.,1.1,0.1)
twb_levels=np.arange(0,1,1)
wup_levels=np.arange(5,55,10)
wdown_levels=np.arange(-55,-5,10)
div_levels=np.arange(-110,120,10)
# Get the 10-m u and v wind components.
u_10m, v_10m = getvar(ncfile, "uvmet10", units="kt", timeidx=ALL_TIMES)
wind_10m = (u_10m**2.0+v_10m**2.0)**0.5
# Smooth the sea level pressure since it tends to be noisy near the mountains
smooth_slp = smooth2d(slp, 3)
twb=twb[:,0,:,:] # lowest model level
twb=smooth2d(twb,3)
# Get the latitude and longitude points
lats, lons = latlon_coords(slp)
# Get the cartopy mapping object
cart_proj = get_cartopy(slp)
if sfcdiags_switch == 1:
bx, by = ll_to_xy(ncfile, blat, blon, meta=False, as_int=True)
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "precip.png"
# should be variable ACSNOW
# accumulated_snow = getvar(ncfile, "SNOWNC", timeidx=ALL_TIMES)
liq_equiv = (getvar(ncfile, "RAINC", timeidx=ALL_TIMES) +
getvar(ncfile, "RAINNC", timeidx=ALL_TIMES))/25.4 # mm to inches
liq_equiv_bdu = liq_equiv[:,by,bx]
prate = np.zeros(numTimes)
for itime in range(numTimes):
if itime > 0 and itime < numTimes-1:
prate[itime] = 0.5*((liq_equiv_bdu[itime+1]+liq_equiv_bdu[itime]) -
(liq_equiv_bdu[itime-1]+liq_equiv_bdu[itime]))
elif itime == 0:
prate[0] = liq_equiv_bdu[0]
else:
prate[numTimes-1] = liq_equiv_bdu[numTimes-1]-liq_equiv_bdu[numTimes-2]
plt.bar(times, prate, width=0.0425, color="black")
plt.plot(times, liq_equiv_bdu, color="blue")
plt.xlim(min(times), max(times))
plt.title("Forecast Precipitation: Boulder, CO")
plt.xlabel("Time (UTC)")
plt.ylabel("Running total (line) and rate (bars, inches of liquid)")
plt.grid(b=True, which="major", axis="both", color="gray", linestyle="--")
fig.savefig("sfcdiags/"+fileout,bbox_inches='tight')
plt.close(fig)
# Create a figure
fig, ax1 = plt.subplots(figsize=(12,9))
fileout = "t2m_td2m_wind10m_prate.png"
t2m = 1.8*(getvar(ncfile, "T2", timeidx=ALL_TIMES)-273.15)+32.
td2m = getvar(ncfile, "td2", units="degF", timeidx=ALL_TIMES)
color = 'tab:blue'
ax1.bar(times, prate, width=0.0425, color="blue")
ax1.plot(times, liq_equiv_bdu, color="blue")
ax1.set_ylim(0.,max([max(prate)/0.1+0.01,max(liq_equiv_bdu)+0.1]))
ax1.set_xlabel("Time (UTC)")
ax1.set_ylabel("Precipitation liquid amount (in) and rate (bars, in/hr)", color=color)
ax1.tick_params(axis="y", labelcolor=color)
ax1.grid(b=True, which="major", axis="x", color="gray", linestyle="--")
ax2=ax1.twinx()
ax2.plot(times, wind_10m[:,by,bx], color="black")
ax2.barbs(times, wind_10m[:,by,bx], u_10m[:,by,bx], v_10m[:,by,bx])
ax2.plot(times, t2m[:,by,bx], color="red")
ax2.plot(times, td2m[:,by,bx], color="green")
ax2.set_xlim(min(times), max(times))
plt.title("Forecast near-surface variables: Boulder, CO")
ax2.set_ylabel("2-m T (red) and 2-m Td (green, degF), 10-m wind (black, kt)")
ax2.grid(b=True, which="major", axis="y", color="gray", linestyle="--")
fig.tight_layout()
fig.savefig("sfcdiags/"+fileout,bbox_inches='tight')
plt.close(fig)
if xcdiags_switch == 1:
zinterp = np.arange(550, 880, 10)
u_xc = vertcross(u, p, levels=zinterp, wrfin=ncfile,
stagger='u', pivot_point=CoordPair(lat=blat,lon=blon), angle=90., meta=False)
w_xc = vertcross(w, p, levels=zinterp, wrfin=ncfile,
stagger='u', pivot_point=CoordPair(lat=blat,lon=blon), angle=90., meta=False)
tc_xc = vertcross(tc, p, levels=zinterp, wrfin=ncfile,
stagger='u', pivot_point=CoordPair(lat=blat,lon=blon), angle=90., meta=False)
rh_xc = vertcross(rh, p, levels=zinterp, wrfin=ncfile,
stagger='u', pivot_point=CoordPair(lat=blat,lon=blon), angle=90., meta=False)
nx = np.shape(u_xc)[-1]
xinterp = np.arange(0,nx,1)
bx, by = ll_to_xy(ncfile, blat, blon, meta=False, as_int=True)
for itime in range(numTimes):
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "mtnwave_xc"+str(itime).zfill(2)+".png"
ax=plt.gca()
ax.set_facecolor("black")
plt.contourf(xinterp, zinterp, u_xc[itime,:,:],
cmap=get_cmap("seismic"), levels=np.arange(-50,55,5))
plt.colorbar(shrink=.62)
w_contour = plt.contour(xinterp, zinterp, w_xc[itime,:,:],
"--", levels=np.arange(-120,-20,20),colors="black")
plt.clabel(w_contour, inline=1, fontsize=10, fmt="%i")
w_contour = plt.contour(xinterp, zinterp, w_xc[itime,:,:],
levels=np.arange(20,120,20),colors="black")
plt.clabel(w_contour, inline=1, fontsize=10, fmt="%i")
t_contour = plt.contour(xinterp, zinterp, tc_xc[itime,:,:],
levels=[-20,-10,0], colors="yellow")
plt.clabel(t_contour, inline=1, fontsize=10, fmt="%i")
# Add location of Boulder to plot.
plt.scatter(bx,np.max(zinterp),c='r',marker='+')
plt.ylim([np.max(zinterp),np.min(zinterp)])
# plt.yscale("log")
# plt.xticks([np.arange(900,475,-25)], ["900", "875",
# "850", "825", "800", "775", "750", "725", "700", "675", "650",
# "625", "600", "575", "550", "525", "500"])
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": zonal wind (fill, kt), temp (yellow lines, degC), VV (black lines, cm/s)")
fig.savefig("xcdiags/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background xcdiags/mtnwave_xc*.png -loop 0 xcdiags/mtnwave_xc.gif")
for itime in range(numTimes):
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "mtnwave_xc_rh"+str(itime).zfill(2)+".png"
ax=plt.gca()
ax.set_facecolor("black")
plt.contourf(xinterp, zinterp, rh_xc[itime,:,:],
cmap=get_cmap("Greens"), levels=rh_levels, extend='both')
plt.colorbar(shrink=.62)
skip=2
plt.quiver(xinterp[::skip], zinterp[::skip], u_xc[itime,::skip,::skip], w_xc[itime,::skip,::skip]/2.,
scale=500, headwidth=3, color='black', pivot='middle')
t_contour = plt.contour(xinterp, zinterp, tc_xc[itime,:,:],
levels=[-20,-10,0], colors="yellow")
plt.clabel(t_contour, inline=1, fontsize=10, fmt="%i")
# Add location of Boulder to plot.
plt.scatter(bx,np.max(zinterp),c='r',marker='+')
plt.ylim([np.max(zinterp),np.min(zinterp)])
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": rh (fill), temp (yellow lines, degC), wind (arrows)")
fig.savefig("xcdiags_rh/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background xcdiags_rh/mtnwave_xc_rh*.png -loop 0 xcdiags_rh/mtnwave_xc_rh.gif")
zinterp = np.arange(150, 900, 25)
rh_xc = vertcross(rh, p, levels=zinterp, wrfin=ncfile,
stagger='u', pivot_point=CoordPair(lat=blat,lon=blon), angle=90., meta=False)
tc_xc = vertcross(tc, p, levels=zinterp, wrfin=ncfile,
stagger='u', pivot_point=CoordPair(lat=blat,lon=blon), angle=90., meta=False)
nx = np.shape(u_xc)[-1]
xinterp = np.arange(0,nx,1)
bx, by = ll_to_xy(ncfile, blat, blon, meta=False, as_int=True)
for itime in range(numTimes):
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "mtnwave_xc_rh_big"+str(itime).zfill(2)+".png"
ax=plt.gca()
ax.set_facecolor("black")
plt.contourf(xinterp, zinterp, rh_xc[itime,:,:],
cmap=get_cmap("Greens"), levels=rh_levels, extend='both')
plt.colorbar(shrink=.62)
t_contour = plt.contour(xinterp, zinterp, tc_xc[itime,:,:],
levels=[-20,-10,0], colors="yellow")
plt.clabel(t_contour, inline=1, fontsize=10, fmt="%i")
# Add location of Boulder to plot.
plt.scatter(bx,np.max(zinterp),c='r',marker='+')
plt.ylim([np.max(zinterp),np.min(zinterp)])
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": rh (fill), temp (yellow lines, degC)")
fig.savefig("xcdiags_rh_big/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background xcdiags_rh_big/mtnwave_xc_rh_big*.png -loop 0 xcdiags_rh_big/mtnwave_xc_rh_big.gif")
if sfc_switch == 1:
bx, by = ll_to_xy(ncfile, blat, blon, meta=False, as_int=True)
for itime in range(numTimes):
ps = p[itime,:,by,bx]
ps_temp = ps
T = tc[itime,:,by,bx]
Td = dewT[itime,:,by,bx]
us = u[itime,:,by,bx]
vs = v[itime,:,by,bx]
ps = ps[ps_temp >= 100.]
T = T[ps_temp >= 100.]
Td = Td[ps_temp >= 100.]
us = us[ps_temp >= 100.]
vs = vs[ps_temp >= 100.]
fig = plt.figure(figsize=(9, 9))
skew = SkewT(fig, rotation=45)
fileout = "sounding"+str(itime).zfill(2)+".png"
# Plot the data using normal plotting functions, in this case using
# log scaling in Y, as dictated by the typical meteorological plot.
skew.plot(ps, T, 'r')
skew.plot(ps, Td, 'g')
skew.plot_barbs(ps, us, vs)
skew.ax.set_ylim(1000, 100)
skew.ax.set_xlim(-40, 60)
# Calculate LCL height and plot as black dot. Because `p`'s first value is
# ~1000 mb and its last value is ~250 mb, the `0` index is selected for
# `p`, `T`, and `Td` to lift the parcel from the surface. If `p` was inverted,
# i.e. start from low value, 250 mb, to a high value, 1000 mb, the `-1` index
# should be selected.
lcl_pressure, lcl_temperature = mpcalc.lcl(ps[0], T[0], Td[0])
skew.plot(lcl_pressure, lcl_temperature, 'ko', markerfacecolor='black')
# Calculate full parcel profile and add to plot as black line
prof = mpcalc.parcel_profile(ps, T[0], Td[0]).to('degC')
skew.plot(ps, prof, 'k', linewidth=2)
# Shade areas of CAPE and CIN
# skew.shade_cin(ps, T, prof, Td)
[cape, cin] = mpcalc.cape_cin(ps, T, Td, prof)
# skew.shade_cape(ps, T, prof)
# An example of a slanted line at constant T -- in this case the 0
# isotherm
skew.ax.axvline(0, color='c', linestyle='--', linewidth=2)
# Add the relevant special lines
skew.plot_dry_adiabats()
skew.plot_moist_adiabats()
skew.plot_mixing_lines()
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": Boulder, CO, CAPE: "+str(round(cape.magnitude))+" J/kg CIN: "+str(round(cin.magnitude))+" J/kg")
fig.savefig("sounding/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background sounding/sounding*.png -loop 0 sounding/sounding.gif")
for itime in range(numTimes):
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "sfc_fhr"+str(itime).zfill(2)+".png"
# Set the GeoAxes to the projection used by WRF
ax = plt.axes(projection=cart_proj)
# Add the states and coastlines
ax.add_feature(states, linewidth=0.8, edgecolor='gray')
ax.add_feature(COUNTIES, linewidth=0.4, facecolor='none', edgecolor='gray')
ax.coastlines('50m', linewidth=0.8)
# Reflectivity at the lowest model level.
plt.contourf(to_np(lons), to_np(lats), to_np(ref[itime,0,:,:]), transform=crs.PlateCarree(),
cmap=get_cmap("jet"), levels=ref_levels)
# Add a color bar
plt.colorbar(ax=ax, shrink=.62)
# Contour the wetbulb temperature at 0 degC.
c_p = plt.contour(to_np(lons), to_np(lats), to_np(twb[itime,:,:]), transform=crs.PlateCarree(),
colors="red", levels=twb_levels)
plt.clabel(c_p, inline=1, fontsize=10, fmt="%i")
# Make the contour outlines and filled contours for the smoothed sea level pressure.
c_p = plt.contour(to_np(lons), to_np(lats), to_np(smooth_slp[itime,:,:]), transform=crs.PlateCarree(),
colors="black", levels=slp_levels)
plt.clabel(c_p, inline=1, fontsize=10, fmt="%i")
# Add location of Boulder to plot.
plt.scatter(blon,blat,c='r',marker='+',transform=crs.PlateCarree())
# Add the 10-m wind barbs, only plotting every other data point.
skip=2
plt.barbs(to_np(lons[::skip,::skip]), to_np(lats[::skip,::skip]), to_np(u_10m[itime, ::skip, ::skip]),
to_np(v_10m[itime, ::skip, ::skip]), transform=crs.PlateCarree(), length=5.25, linewidth=0.5)
# Set the map limits.
ax.set_xlim(cartopy_xlim(smooth_slp))
ax.set_ylim(cartopy_ylim(smooth_slp))
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": SLP (fill, hPa), 10-m wind (barbs, kt), LML Ref (fill, dBZ), LML WBT (red, degC)")
fig.savefig("sfc/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background sfc/sfc*.png -loop 0 sfc/sfc.gif")
for itime in range(numTimes):
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "sfc_temp_fhr"+str(itime).zfill(2)+".png"
# Set the GeoAxes to the projection used by WRF
ax = plt.axes(projection=cart_proj)
# Add the states and coastlines
ax.add_feature(states, linewidth=0.8, edgecolor='gray')
ax.add_feature(COUNTIES, linewidth=0.4, facecolor='none', edgecolor='gray')
ax.coastlines('50m', linewidth=0.8)
# 2-m air temperature
t2 = 1.8*(getvar(ncfile, "T2", timeidx=ALL_TIMES) - 273.15)+32.
plt.contourf(to_np(lons), to_np(lats), to_np(t2[itime,:,:]), transform=crs.PlateCarree(),
cmap=get_cmap("jet"), levels=t2_levels)
# Add a color bar
plt.colorbar(ax=ax, shrink=.62)
# Make the contour outlines and filled contours for the smoothed sea level pressure.
c_p = plt.contour(to_np(lons), to_np(lats), to_np(smooth_slp[itime,:,:]), transform=crs.PlateCarree(),
colors="black", levels=slp_levels)
plt.clabel(c_p, inline=1, fontsize=10, fmt="%i")
# Add location of Boulder to plot.
plt.scatter(blon,blat,c='r',marker='+',transform=crs.PlateCarree())
# Add the 10-m wind barbs, only plotting every other data point.
skip=2
plt.barbs(to_np(lons[::skip,::skip]), to_np(lats[::skip,::skip]), to_np(u_10m[itime, ::skip, ::skip]),
to_np(v_10m[itime, ::skip, ::skip]), transform=crs.PlateCarree(), length=5.25, linewidth=0.5)
# Set the map limits.
ax.set_xlim(cartopy_xlim(smooth_slp))
ax.set_ylim(cartopy_ylim(smooth_slp))
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": SLP (contours, hPa), 10-m wind (barbs, kt), 2-m T (fill, degF)")
fig.savefig("sfc_temp/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background sfc_temp/sfc_temp*.png -loop 0 sfc_temp/sfc_temp.gif")
if cloud_switch == 1:
for itime in range(numTimes):
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "cldfrac_fhr"+str(itime).zfill(2)+".png"
# Set the GeoAxes to the projection used by WRF
ax = plt.axes(projection=cart_proj)
# Add the states and coastlines
ax.add_feature(states, linewidth=0.8, edgecolor='gray')
ax.add_feature(COUNTIES, linewidth=0.4, facecolor='none', edgecolor='gray')
ax.coastlines('50m', linewidth=0.8)
# Compute and plot the total cloud fraction.
plt.contourf(to_np(lons), to_np(lats), to_np(total_cloudfrac[itime,:,:]), transform=crs.PlateCarree(),
cmap=get_cmap("Greys"), levels=cldfrac_levels, extend='both')
# Add a color bar
plt.colorbar(ax=ax, shrink=.62)
# Add location of Boulder to plot.
plt.scatter(blon,blat,c='r',marker='+',transform=crs.PlateCarree())
# Set the map limits.
ax.set_xlim(cartopy_xlim(cloudfrac))
ax.set_ylim(cartopy_ylim(cloudfrac))
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": Total cloud fraction (fill)")
fig.savefig("cldfrac/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background cldfrac/cldfrac*.png -loop 0 cldfrac/cldfrac.gif")
for itime in range(numTimes):
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "low_cldfrac_fhr"+str(itime).zfill(2)+".png"
# Set the GeoAxes to the projection used by WRF
ax = plt.axes(projection=cart_proj)
# Add the states and coastlines
ax.add_feature(states, linewidth=0.8, edgecolor='gray')
ax.add_feature(COUNTIES, linewidth=0.4, facecolor='none', edgecolor='gray')
ax.coastlines('50m', linewidth=0.8)
# Compute and plot the cloud fraction.
plt.contourf(to_np(lons), to_np(lats), to_np(low_cloudfrac[itime,:,:]), transform=crs.PlateCarree(),
cmap=get_cmap("Greys"), levels=cldfrac_levels, extend='both')
# Add a color bar
plt.colorbar(ax=ax, shrink=.62)
# Add location of Boulder to plot.
plt.scatter(blon,blat,c='r',marker='+',transform=crs.PlateCarree())
# Set the map limits.
ax.set_xlim(cartopy_xlim(cloudfrac))
ax.set_ylim(cartopy_ylim(cloudfrac))
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": Low cloud fraction (fill)")
fig.savefig("low_cldfrac/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background low_cldfrac/low_cldfrac*.png -loop 0 low_cldfrac/low_cldfrac.gif")
for itime in range(numTimes):
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "mid_cldfrac_fhr"+str(itime).zfill(2)+".png"
# Set the GeoAxes to the projection used by WRF
ax = plt.axes(projection=cart_proj)
# Add the states and coastlines
ax.add_feature(states, linewidth=0.8, edgecolor='gray')
ax.add_feature(COUNTIES, linewidth=0.4, facecolor='none', edgecolor='gray')
ax.coastlines('50m', linewidth=0.8)
# Compute and plot the cloud fraction.
plt.contourf(to_np(lons), to_np(lats), to_np(mid_cloudfrac[itime,:,:]), transform=crs.PlateCarree(),
cmap=get_cmap("Greys"), levels=cldfrac_levels, extend='both')
# Add a color bar
plt.colorbar(ax=ax, shrink=.62)
# Add location of Boulder to plot.
plt.scatter(blon,blat,c='r',marker='+',transform=crs.PlateCarree())
# Set the map limits.
ax.set_xlim(cartopy_xlim(cloudfrac))
ax.set_ylim(cartopy_ylim(cloudfrac))
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": Mid cloud fraction (fill)")
fig.savefig("mid_cldfrac/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background mid_cldfrac/mid_cldfrac*.png -loop 0 mid_cldfrac/mid_cldfrac.gif")
for itime in range(numTimes):
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "high_cldfrac_fhr"+str(itime).zfill(2)+".png"
# Set the GeoAxes to the projection used by WRF
ax = plt.axes(projection=cart_proj)
# Add the states and coastlines
ax.add_feature(states, linewidth=0.8, edgecolor='gray')
ax.add_feature(COUNTIES, linewidth=0.4, facecolor='none', edgecolor='gray')
ax.coastlines('50m', linewidth=0.8)
# Compute and plot the cloud fraction.
plt.contourf(to_np(lons), to_np(lats), to_np(high_cloudfrac[itime,:,:]), transform=crs.PlateCarree(),
cmap=get_cmap("Greys"), levels=cldfrac_levels, extend='both')
# Add a color bar
plt.colorbar(ax=ax, shrink=.62)
# Add location of Boulder to plot.
plt.scatter(blon,blat,c='r',marker='+',transform=crs.PlateCarree())
# Set the map limits.
ax.set_xlim(cartopy_xlim(cloudfrac))
ax.set_ylim(cartopy_ylim(cloudfrac))
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": High cloud fraction (fill)")
fig.savefig("high_cldfrac/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background high_cldfrac/high_cldfrac*.png -loop 0 high_cldfrac/high_cldfrac.gif")
if switch_500mb == 1:
for itime in range(numTimes):
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "500mb_fhr"+str(itime).zfill(2)+".png"
# Set the GeoAxes to the projection used by WRF
ax = plt.axes(projection=cart_proj)
# Add the states and coastlines
ax.add_feature(states, linewidth=0.8, edgecolor='gray')
ax.add_feature(COUNTIES, linewidth=0.4, facecolor='none', edgecolor='gray')
ax.coastlines('50m', linewidth=0.8)
# wind color fill
if np.max(wspeed_500[itime,:,:]) > np.min(wspeed_levels):
plt.contourf(to_np(lons), to_np(lats), to_np(wspeed_500[itime,:,:]), transform=crs.PlateCarree(),
cmap=get_cmap("rainbow"), levels=wspeed_levels)
# Make the 500 mb height contours.
c_z = plt.contour(to_np(lons), to_np(lats), to_np(z_500[itime,:,:]), transform=crs.PlateCarree(),
colors="black", levels=z_levels)
plt.clabel(c_z, inline=1, fontsize=10, fmt="%i")
# Make the 500 mb temp contours.
c_t = plt.contour(to_np(lons), to_np(lats), to_np(tc_500[itime,:,:]), transform=crs.PlateCarree(),
colors="red", levels=tc_levels)
plt.clabel(c_t, inline=1, fontsize=10, fontcolor="red", fmt="%i")
# Add a color bar
# plt.colorbar(ax=ax, shrink=.62)
# Add location of Boulder to plot.
plt.scatter(blon,blat,c='r',marker='+',transform=crs.PlateCarree())
# Add the 500mb wind barbs, only plotting every other data point.
skip=3
plt.barbs(to_np(lons[::skip,::skip]), to_np(lats[::skip,::skip]), to_np(u_500[itime, ::skip, ::skip]),
to_np(v_500[itime, ::skip, ::skip]), transform=crs.PlateCarree(), length=5.25, linewidth=0.5)
# Set the map limits.
ax.set_xlim(cartopy_xlim(z_500))
ax.set_ylim(cartopy_ylim(z_500))
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": 500-mb height (black, dm), temp (red, degC), and wind (fill/barbs, kt)")
fig.savefig("500mb/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background 500mb/500mb*.png -loop 0 500mb/500mb.gif")
if switch_700mb == 1:
for itime in range(numTimes):
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "700mb_fhr"+str(itime).zfill(2)+".png"
# Set the GeoAxes to the projection used by WRF
ax = plt.axes(projection=cart_proj)
# Add the states and coastlines
ax.add_feature(states, linewidth=0.8, edgecolor='gray')
ax.add_feature(COUNTIES, linewidth=0.4, facecolor='none', edgecolor='gray')
ax.coastlines('50m', linewidth=0.8)
# rh color fill
plt.contourf(to_np(lons), to_np(lats), to_np(rh_700[itime,:,:]), transform=crs.PlateCarree(),
cmap=get_cmap("Greens"), levels=rh_levels, extend='both')
# Add a color bar
plt.colorbar(ax=ax, shrink=.62)
# Make the 700 mb height contours.
c_z = plt.contour(to_np(lons), to_np(lats), to_np(z_700[itime,:,:]), transform=crs.PlateCarree(),
colors="black", levels=z_levels_700)
plt.clabel(c_z, inline=1, fontsize=10, fmt="%i")
# Make the 700 mb temp contours.
c_t = plt.contour(to_np(lons), to_np(lats), to_np(tc_700[itime,:,:]), transform=crs.PlateCarree(),
colors="red", levels=tc_levels)
plt.clabel(c_t, inline=1, fontsize=10, fontcolor="red", fmt="%i")
# Make the 700 mb VV contours.
c_d = plt.contour(to_np(lons), to_np(lats), to_np(w_700[itime,:,:]), transform=crs.PlateCarree(),
colors="magenta", levels=wup_levels, linewidths=0.9)
plt.clabel(c_d, inline=1, fontsize=10, fontcolor="magenta", fmt="%i")
c_c = plt.contour(to_np(lons), to_np(lats), to_np(w_700[itime,:,:]), transform=crs.PlateCarree(),
colors="blue", levels=wdown_levels, linewidths=0.9)
plt.clabel(c_c, inline=1, fontsize=10, fontcolor="blue", fmt="%i")
# Add location of Boulder to plot.
plt.scatter(blon,blat,c='r',marker='+',transform=crs.PlateCarree())
# Add the 700mb wind barbs, only plotting every other data point.
skip=3
plt.barbs(to_np(lons[::skip,::skip]), to_np(lats[::skip,::skip]), to_np(u_700[itime, ::skip, ::skip]),
to_np(v_700[itime, ::skip, ::skip]), transform=crs.PlateCarree(), length=5.25, linewidth=0.5)
# Set the map limits.
ax.set_xlim(cartopy_xlim(z_700))
ax.set_ylim(cartopy_ylim(z_700))
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": 700-mb hgt (black, dm), T (red, degC), wind (barbs, kt), VV (cm/s), rh (fill, %)")
fig.savefig("700mb/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background 700mb/700mb*.png -loop 0 700mb/700mb.gif")
if switch_300mb == 1:
for itime in range(numTimes):
# Create a figure
fig = plt.figure(figsize=(12,9))
fileout = "300mb_fhr"+str(itime).zfill(2)+".png"
# Set the GeoAxes to the projection used by WRF
ax = plt.axes(projection=cart_proj)
# Add the states and coastlines
ax.add_feature(states, linewidth=0.8, edgecolor='gray')
ax.add_feature(COUNTIES, linewidth=0.4, facecolor='none', edgecolor='gray')
ax.coastlines('50m', linewidth=0.8)
# 300 mb divergence
plt.contourf(to_np(lons), to_np(lats), to_np(div_300[itime,:,:]), transform=crs.PlateCarree(),
cmap=get_cmap("seismic"), levels=div_levels)
# Add a color bar
plt.colorbar(ax=ax, shrink=.62)
# Make the 300 mb height contours.
c_z = plt.contour(to_np(lons), to_np(lats), to_np(z_300[itime,:,:]), transform=crs.PlateCarree(),
colors="black", levels=z_levels_300)
plt.clabel(c_z, inline=1, fontsize=10, fmt="%i")
# Make the 300 mb divergence contours.
# c_d = plt.contour(to_np(lons), to_np(lats), to_np(div_300[itime,:,:]), transform=crs.PlateCarree(),
# colors="red", levels=div_levels, linewidths=0.8)
# plt.clabel(c_d, inline=1, fontsize=10, fontcolor="red", fmt="%i")
#
# c_c = plt.contour(to_np(lons), to_np(lats), to_np(div_300[itime,:,:]), transform=crs.PlateCarree(),
# colors="blue", levels=conv_levels, linewidths=0.8)
# plt.clabel(c_c, inline=1, fontsize=10, fontcolor="blue", fmt="%i")
# Add location of Boulder to plot.
plt.scatter(blon,blat,c='r',marker='+',transform=crs.PlateCarree())
# Add the 300mb wind barbs, only plotting every other data point.
skip=3
plt.barbs(to_np(lons[::skip,::skip]), to_np(lats[::skip,::skip]), to_np(u_300[itime, ::skip, ::skip]),
to_np(v_300[itime, ::skip, ::skip]), transform=crs.PlateCarree(), length=5.25, linewidth=0.5)
# Set the map limits.
ax.set_xlim(cartopy_xlim(z_300))
ax.set_ylim(cartopy_ylim(z_300))
plt_time=str(dtimes[itime])
plt_time=plt_time[0:13]
plt.title(plt_time+"Z fhr "+str(itime).zfill(2)+": 300-mb height (black, dm), wind (barbs, kt), and divergence x 10^5 (red/blue, s^-1)")
fig.savefig("300mb/"+fileout,bbox_inches='tight')
plt.close(fig)
os.system("convert -delay 90 -dispose background 300mb/300mb*.png -loop 0 300mb/300mb.gif")
def calculate_basic_thermo(self):
#Enclose in try, except because not every sounding will have a converging parcel path or CAPE.
try:
#Precipitable Water
self.pw = mc.precipitable_water(self.sounding["pres"],
self.sounding["dewp"])
#Lifting condensation level
self.lcl_pres, self.lcl_temp = mc.lcl(self.sounding["pres"][0],
self.sounding["temp"][0],
self.sounding["dewp"][0])
#Surface-based CAPE and CIN
self.parcel_path = mc.parcel_profile(self.sounding["pres"],
self.sounding["temp"][0],
self.sounding["dewp"][0])
self.sfc_cape, self.sfc_cin = mc.cape_cin(self.sounding["pres"],
self.sounding["temp"],
self.sounding["dewp"],
self.parcel_path)
#Do this when parcel path fails to converge
except Exception as e:
print("WARNING: No LCL, CAPE, or PW stats because:\n{}.".format(e))
self.parcel_path = numpy.nan
self.pw = numpy.nan
self.lcl_pres = numpy.nan
self.lcl_temp = numpy.nan
self.sfc_cape = numpy.nan
self.sfc_cin = numpy.nan
#Returning
return
def get_skewt_vars(p, tc, tdc, pro):
"""This function processes the dataset values and returns a string element
which can be used as a subtitle to replicate the styles of NCL Skew-T
Diagrams.
Args:
p (:class: `pint.quantity.build_quantity_class.<locals>.Quantity`):
Pressure level input from dataset
tc (:class: `pint.quantity.build_quantity_class.<locals>.Quantity`):
Temperature for parcel from dataset
tdc (:class: `pint.quantity.build_quantity_class.<locals>.Quantity`):
Dew point temperature for parcel from dataset
pro (:class: `pint.quantity.build_quantity_class.<locals>.Quantity`):
Parcel profile temperature converted to degC
Returns:
:class: 'str'
"""
# CAPE
cape = mpcalc.cape_cin(p, tc, tdc, pro)
cape = cape[0].magnitude
# Precipitable Water
pwat = mpcalc.precipitable_water(p, tdc)
pwat = (pwat.magnitude / 10) * units.cm # Convert mm to cm
pwat = pwat.magnitude
# Pressure and temperature of lcl
lcl = mpcalc.lcl(p[0], tc[0], tdc[0])
plcl = lcl[0].magnitude
tlcl = lcl[1].magnitude
# Showalter index
shox = showalter_index(p, tc, tdc)
shox = shox[0].magnitude
# Place calculated values in iterable list
vals = [plcl, tlcl, shox, pwat, cape]
vals = [round(num) for num in vals]
# Define variable names for calculated values
names = ['Plcl=', 'Tlcl[C]=', 'Shox=', 'Pwat[cm]=', 'Cape[J]=']
# Combine the list of values with their corresponding labels
lst = list(chain.from_iterable(zip(names, vals)))
lst = map(str, lst)
# Create one large string for later plotting use
joined = ' '.join(lst)
return joined
def test_cape_cin():
"""Tests the basic CAPE and CIN calculation."""
p = np.array([959., 779.2, 751.3, 724.3, 700., 269.]) * units.mbar
temperature = np.array([22.2, 14.6, 12., 9.4, 7., -38.]) * units.celsius
dewpoint = np.array([19., -11.2, -10.8, -10.4, -10., -53.2]) * units.celsius
parcel_prof = parcel_profile(p, temperature[0], dewpoint[0])
cape, cin = cape_cin(p, temperature, dewpoint, parcel_prof)
assert_almost_equal(cape, 58.0368212 * units('joule / kilogram'), 6)
assert_almost_equal(cin, -89.8073512 * units('joule / kilogram'), 6)
def test_cape_cin_no_el():
"""Tests that CAPE works with no EL."""
p = np.array([959., 779.2, 751.3, 724.3]) * units.mbar
temperature = np.array([22.2, 14.6, 12., 9.4]) * units.celsius
dewpoint = np.array([19., -11.2, -10.8, -10.4]) * units.celsius
parcel_prof = parcel_profile(p, temperature[0], dewpoint[0]).to('degC')
cape, cin = cape_cin(p, temperature, dewpoint, parcel_prof)
assert_almost_equal(cape, 0.08750805 * units('joule / kilogram'), 6)
assert_almost_equal(cin, -89.8073512 * units('joule / kilogram'), 6)
def test_cape_cin_no_lfc():
"""Test that CAPE is zero with no LFC."""
p = np.array([959., 779.2, 751.3, 724.3, 700., 269.]) * units.mbar
temperature = np.array([22.2, 24.6, 22., 20.4, 18., -10.]) * units.celsius
dewpoint = np.array([19., -11.2, -10.8, -10.4, -10., -53.2]) * units.celsius
parcel_prof = parcel_profile(p, temperature[0], dewpoint[0]).to('degC')
cape, cin = cape_cin(p, temperature, dewpoint, parcel_prof)
assert_almost_equal(cape, 0.0 * units('joule / kilogram'), 6)
assert_almost_equal(cin, 0.0 * units('joule / kilogram'), 6)
def test_cape_cin_no_el():
"""Test that CAPE works with no EL."""
p = np.array([959., 779.2, 751.3, 724.3]) * units.mbar
temperature = np.array([22.2, 14.6, 12., 9.4]) * units.celsius
dewpoint = np.array([19., -11.2, -10.8, -10.4]) * units.celsius
parcel_prof = parcel_profile(p, temperature[0], dewpoint[0]).to('degC')
cape, cin = cape_cin(p, temperature, dewpoint, parcel_prof)
assert_almost_equal(cape, 0.08750805 * units('joule / kilogram'), 6)
assert_almost_equal(cin, -89.8073512 * units('joule / kilogram'), 6)
def test_cape_cin():
"""Test the basic CAPE and CIN calculation."""
p = np.array([959., 779.2, 751.3, 724.3, 700., 269.]) * units.mbar
temperature = np.array([22.2, 14.6, 12., 9.4, 7., -38.]) * units.celsius
dewpoint = np.array([19., -11.2, -10.8, -10.4, -10., -53.2]) * units.celsius
parcel_prof = parcel_profile(p, temperature[0], dewpoint[0])
cape, cin = cape_cin(p, temperature, dewpoint, parcel_prof)
assert_almost_equal(cape, 58.0368212 * units('joule / kilogram'), 6)
assert_almost_equal(cin, -89.8073512 * units('joule / kilogram'), 6)
def test_cape_cin_custom_profile():
"""Test the CAPE and CIN calculation with a custom profile passed to LFC and EL."""
p = np.array([959., 779.2, 751.3, 724.3, 700., 269.]) * units.mbar
temperature = np.array([22.2, 14.6, 12., 9.4, 7., -38.]) * units.celsius
dewpoint = np.array([19., -11.2, -10.8, -10.4, -10., -53.2]) * units.celsius
parcel_prof = parcel_profile(p, temperature[0], dewpoint[0]) + 5 * units.delta_degC
cape, cin = cape_cin(p, temperature, dewpoint, parcel_prof)
assert_almost_equal(cape, 1443.505086499895 * units('joule / kilogram'), 6)
assert_almost_equal(cin, 0.0 * units('joule / kilogram'), 6)
def test_cape_cin_no_lfc():
"""Tests that CAPE is zero with no LFC."""
p = np.array([959., 779.2, 751.3, 724.3, 700., 269.]) * units.mbar
temperature = np.array([22.2, 24.6, 22., 20.4, 18., -10.]) * units.celsius
dewpoint = np.array([19., -11.2, -10.8, -10.4, -10., -53.2]) * units.celsius
parcel_prof = parcel_profile(p, temperature[0], dewpoint[0]).to('degC')
cape, cin = cape_cin(p, temperature, dewpoint, parcel_prof)
assert_almost_equal(cape, 0.0 * units('joule / kilogram'), 6)
assert_almost_equal(cin, 0.0 * units('joule / kilogram'), 6)
def calcMLCAPE(levels, temperature, dewpoint, depth=100.0 * units.hPa):
_, T_parc, Td_par = mixed_parcel(
levels,
temperature,
dewpoint,
depth=depth,
interpolate=False,
)
profile = parcel_profile(levels, T_parc, Td_parc)
cape, cin = cape_cin(levels, temperature, dewpoint, profile)
return cape
def get_cape(inargs, return_parcel_profile=False):
pres_prof, temp_prof, dp_prof = inargs
try:
prof = mpcalc.parcel_profile(pres_prof, temp_prof[0], dp_prof[0])
cape, cin = mpcalc.cape_cin(pres_prof, temp_prof, dp_prof, prof)
except Exception:
cape, cin, prof = np.NaN, np.NaN, np.NaN
print('Problem during CAPE-calculation. Likely NaN-related.')
if return_parcel_profile:
return cape, cin, prof
else:
return cape, cin
for i in range(1, 5):
soundlat = 27.15
soundlon = 360 - (startlat + (londelt * i))
sound_temps = data["temperature"].interp(lat=soundlat, lon=soundlon) - 273.15
sound_rh = data["rh"].interp(lat=soundlat, lon=soundlon)
sound_dp = mpcalc.dewpoint_from_relative_humidity(
sound_temps.data * units.degC, sound_rh.data * units.percent
)
skew = SkewT(fig=fig, rect=(0.75 - (0.15 * i), 0.2, 0.15, 0.1))
parcel_prof = mpcalc.parcel_profile(
sound_pres, sound_temps[0].data * units.degC, sound_dp[0]
)
cape = mpcalc.cape_cin(
sound_pres, sound_temps.data * units.degC, sound_dp, parcel_prof
)
capeout = int(cape[0].m)
cinout = int(cape[1].m)
skew.plot(sound_pres, sound_dp, "g", linewidth=3)
skew.plot(sound_pres, sound_temps, "r", linewidth=3)
if capeout > capemin:
# Shade areas of CAPE and CIN
skew.shade_cin(sound_pres, sound_temps.data * units.degC, parcel_prof)
skew.shade_cape(sound_pres, sound_temps.data * units.degC, parcel_prof)
skew.plot(sound_pres, parcel_prof, color="fuchsia", linewidth=1)
skew.ax.axvline(0, color="purple", linestyle="--", linewidth=3)
skew.ax.set_ylim((1000, ptop))
def getData(self, time, model_vars, mdl2stnd, previous_data=None):
'''
Name:
awips_model_base
Purpose:
A function to get data from NAM40 model to create HDWX products
Inputs:
request : A DataAccessLayer request object
time : List of datatime(s) for data to grab
model_vars : Dictionary with variables/levels to get
mdl2stnd : Dictionary to convert from model variable names
to standardized names
Outputs:
Returns a dictionary containing all data
Keywords:
previous_data : Dictionary with data from previous time step
'''
log = logging.getLogger(__name__)
# Set up function for logger
initTime, fcstTime = get_init_fcst_times(time[0])
data = {
'model': self._request.getLocationNames()[0],
'initTime': initTime,
'fcstTime': fcstTime
}
# Initialize empty dictionary
log.info('Attempting to download {} data'.format(data['model']))
for var in model_vars: # Iterate over variables in the vars list
log.debug('Getting: {}'.format(var))
self._request.setParameters(*model_vars[var]['parameters'])
# Set parameters for the download request
self._request.setLevels(*model_vars[var]['levels'])
# Set levels for the download request
response = DAL.getGridData(self._request, time) # Request the data
for res in response: # Iterate over all data request responses
varName = res.getParameter()
# Get name of the variable in the response
varLvl = res.getLevel()
# Get level of the variable in the response
varName = mdl2stnd[varName]
# Convert variable name to local standarized name
if varName not in data:
data[varName] = {}
# If variable name NOT in data dictionary, initialize new dictionary under key
data[varName][varLvl] = res.getRawData()
# Add data under level name
try: # Try to
unit = units(res.getUnit())
# Get units and convert to MetPy units
except: # On exception
unit = '?'
# Set units to ?
else: # If get units success
data[varName][varLvl] *= unit
# Get data and create MetPy quantity by multiplying by units
log.debug(
'Got data for:\n Var: {}\n Lvl: {}\n Unit: {}'.format(
varName, varLvl, unit))
data['lon'], data['lat'] = res.getLatLonCoords()
# Get latitude and longitude values
data['lon'] *= units('degree')
# Add units of degree to longitude
data['lat'] *= units('degree')
# Add units of degree to latitude
# Absolute vorticity
dx, dy = lat_lon_grid_deltas(data['lon'], data['lat'])
# Get grid spacing in x and y
uTag = mdl2stnd[model_vars['wind']['parameters'][0]]
# Get initial tag name for u-wind
vTag = mdl2stnd[model_vars['wind']['parameters'][1]]
# Get initial tag name for v-wind
if (uTag in data) and (
vTag in data): # If both tags are in the data structure
data['abs_vort'] = {}
# Add absolute vorticity key
for lvl in model_vars['wind'][
'levels']: # Iterate over all leves in the wind data
if (lvl in data[uTag]) and (
lvl in data[vTag]
): # If given level in both u- and v-wind dictionaries
log.debug('Computing absolute vorticity at {}'.format(lvl))
data['abs_vort'][ lvl ] = \
absolute_vorticity( data[uTag][lvl], data[vTag][lvl],
dx, dy, data['lat'] )
# Compute absolute vorticity
# 1000 MB equivalent potential temperature
if ('temperature' in data) and (
'dewpoint'
in data): # If temperature AND depoint data were downloaded
data['theta_e'] = {}
T, Td = 'temperature', 'dewpoint'
if ('1000.0MB' in data[T]) and (
'1000.0MB' in data[Td]
): # If temperature AND depoint data were downloaded
log.debug(
'Computing equivalent potential temperature at 1000 hPa')
data['theta_e']['1000.0MB'] = equivalent_potential_temperature(
1000.0 * units('hPa'), data[T]['1000.0MB'],
data[Td]['1000.0MB'])
return data
# MLCAPE
log.debug('Computing mixed layer CAPE')
T_lvl = list(data[T].keys())
Td_lvl = list(data[Td].keys())
levels = list(set(T_lvl).intersection(Td_lvl))
levels = [float(lvl.replace('MB', '')) for lvl in levels]
levels = sorted(levels, reverse=True)
nLvl = len(levels)
if nLvl > 0:
log.debug(
'Found {} matching levels in temperature and dewpoint data'
.format(nLvl))
nLat, nLon = data['lon'].shape
data['MLCAPE'] = np.zeros((
nLat,
nLon,
), dtype=np.float32) * units('J/kg')
TT = np.zeros((
nLvl,
nLat,
nLon,
), dtype=np.float32) * units('degC')
TTd = np.zeros((
nLvl,
nLat,
nLon,
), dtype=np.float32) * units('degC')
log.debug('Sorting temperature and dewpoint data by level')
for i in range(nLvl):
key = '{:.1f}MB'.format(levels[i])
TT[i, :, :] = data[T][key].to('degC')
TTd[i, :, :] = data[Td][key].to('degC')
levels = np.array(levels) * units.hPa
depth = 100.0 * units.hPa
log.debug('Iterating over grid boxes to compute MLCAPE')
for j in range(nLat):
for i in range(nLon):
try:
_, T_parc, Td_parc = mixed_parcel(
levels,
TT[:, j, i],
TTd[:, j, i],
depth=depth,
interpolate=False,
)
profile = parcel_profile(levels, T_parc, Td_parc)
cape, cin = cape_cin(levels, TT[:, j, i],
TTd[:, j, i], profile)
except:
log.warning(
'Failed to compute MLCAPE for lon/lat: {}; {}'.
format(data['lon'][j, i], data['lat'][j, i]))
else:
data['MLCAPE'][j, i] = cape
return data
def entropy_plots(pressure,
temperature,
mixing_ratio,
altitude,
h0_std=2000,
ensemble_size=20,
ent_rate=np.arange(0, 2, 0.05),
entrain=False):
"""
plotting the summarized entropy diagram with annotations and thermodynamic parameters
"""
p = pressure * units('mbar')
T = temperature * units('degC')
q = mixing_ratio * units('kilogram/kilogram')
qs = mpcalc.mixing_ratio(mpcalc.saturation_vapor_pressure(T), p)
Td = mpcalc.dewpoint(mpcalc.vapor_pressure(p, q)) # dewpoint
Tp = mpcalc.parcel_profile(p, T[0], Td[0]).to('degC') # parcel profile
# Altitude based on the hydrostatic eq.
if len(altitude) == len(pressure): # (1) altitudes for whole levels
altitude = altitude * units('meter')
elif len(altitude
) == 1: # (2) known altitude where the soundings was launched
z_surf = altitude.copy() * units('meter')
# given altitude
altitude = np.zeros((np.size(T))) * units('meter')
for i in range(np.size(T)):
altitude[i] = mpcalc.thickness_hydrostatic(
p[:i + 1], T[:i + 1]) + z_surf # Hypsometric Eq. for height
else:
print(
'***NOTE***: the altitude at the surface is assumed 0 meter, and altitudes are derived based on the hypsometric equation'
)
altitude = np.zeros(
(np.size(T))) * units('meter') # surface is 0 meter
for i in range(np.size(T)):
altitude[i] = mpcalc.thickness_hydrostatic(
p[:i + 1], T[:i + 1]) # Hypsometric Eq. for height
# specific entropy [joule/(kg*K)]
# sd : specific entropy of dry air
# sm1 : specific entropy of airborne mositure in state 1 (water vapor)
# sm2 : specific entropy of airborne mositure in state 2 (saturated water vapor)
sd = entropy(T.magnitude, q.magnitude * 1e-6, p.magnitude)
sm1 = entropy(T.magnitude, q.magnitude, p.magnitude)
sm2 = entropy(T.magnitude, qs.magnitude, p.magnitude)
###############################
# Water vapor calculations
p_PWtop = min(p)
#p_PWtop = max(200*units.mbar, min(p) + 1*units.mbar) # integrating until 200mb
cwv = mpcalc.precipitable_water(Td, p,
top=p_PWtop) # column water vapor [mm]
cwvs = mpcalc.precipitable_water(
T, p, top=p_PWtop) # saturated column water vapor [mm]
crh = (cwv / cwvs) * 100. # column relative humidity [%]
#================================================
# plotting MSE vertical profiles
fig = plt.figure(figsize=[12, 8])
ax = fig.add_axes([0.1, 0.1, 0.6, 0.8])
ax.plot(sd, p, '-k', linewidth=2)
ax.plot(sm1, p, '-b', linewidth=2)
ax.plot(sm2, p, '-r', linewidth=2)
# mse based on different percentages of relative humidity
qr = np.zeros((9, np.size(qs))) * units('kilogram/kilogram')
sm1_r = qr # container
for i in range(9):
qr[i, :] = qs * 0.1 * (i + 1)
sm1_r[i, :] = entropy(T.magnitude, qr[i, :].magnitude, p.magnitude)
for i in range(9):
ax.plot(sm1_r[i, :], p[:], '-', color='grey', linewidth=0.7)
ax.text(sm1_r[i, 3].magnitude - 2, p[3].magnitude, str((i + 1) * 10))
# drawing LCL and LFC levels
[lcl_pressure, lcl_temperature] = mpcalc.lcl(p[0], T[0], Td[0])
lcl_idx = np.argmin(np.abs(p.magnitude - lcl_pressure.magnitude))
[lfc_pressure, lfc_temperature] = mpcalc.lfc(p, T, Td)
lfc_idx = np.argmin(np.abs(p.magnitude - lfc_pressure.magnitude))
# conserved mse of air parcel arising from 1000 hpa
sm1_p = np.squeeze(np.ones((1, np.size(T))) * sm1[0])
# illustration of CAPE
el_pressure, el_temperature = mpcalc.el(p, T, Td) # equilibrium level
el_idx = np.argmin(np.abs(p.magnitude - el_pressure.magnitude))
ELps = [el_pressure.magnitude
] # Initialize an array of EL pressures for detrainment profile
[CAPE, CIN] = mpcalc.cape_cin(p[:el_idx], T[:el_idx], Td[:el_idx],
Tp[:el_idx])
plt.plot(sm1_p, p, color='green', linewidth=2)
#ax.fill_betweenx(p[lcl_idx:el_idx+1],sm1_p[lcl_idx:el_idx+1],sm2[lcl_idx:el_idx+1],interpolate=True
# ,color='green',alpha='0.3')
ax.fill_betweenx(p, sd, sm1, color='deepskyblue', alpha='0.5')
ax.set_xlabel('Specific entropies: sd, sm, sm_sat [J K$^{-1}$ kg$^{-1}$]',
fontsize=14)
ax.set_ylabel('Pressure [hPa]', fontsize=14)
ax.set_xticks([0, 50, 100, 150, 200, 250, 300, 350])
ax.set_xlim([0, 440])
ax.set_ylim(1030, 120)
if entrain is True:
# Depict Entraining parcels
# Parcel mass solves dM/dz = eps*M, solution is M = exp(eps*Z)
# M=1 at ground without loss of generality
# Distribution of surface parcel h offsets
h0offsets = np.sort(np.random.normal(
0, h0_std, ensemble_size)) * units('joule/kilogram')
# Distribution of entrainment rates
entrainment_rates = ent_rate / (units('km'))
for h0offset in h0offsets:
h4ent = sm1.copy()
h4ent[0] += h0offset
for eps in entrainment_rates:
M = np.exp(eps * (altitude - altitude[0])).to('dimensionless')
# dM is the mass contribution at each level, with 1 at the origin level.
M[0] = 0
dM = np.gradient(M)
# parcel mass is a sum of all the dM's at each level
# conserved linearly-mixed variables like h are weighted averages
if eps.magnitude == 0.0:
hent = np.ones(len(h4ent)) * h4ent[0] # no mixing
else:
hent = np.cumsum(dM * h4ent) / np.cumsum(dM)
# Boolean for positive buoyancy, and its topmost altitude (index) where curve is clippes
posboy = (hent > sm2)
posboy[0] = True # so there is always a detrainment level
# defining the first EL by posboy as the detrainment layer, swiching from positive buoyancy to
# negative buoyancy (0 to 1) and skipping the surface
ELindex_ent = 0
for idx in range(len(posboy) - 1):
if posboy[idx + 1] == 0 and posboy[idx] == 1 and idx > 0:
ELindex_ent = idx
break
# Plot the curve
plt.plot(hent[0:ELindex_ent + 2],
p[0:ELindex_ent + 2],
linewidth=0.6,
color='g')
#plt.plot( hent[0:], p[0:], linewidth=0.6, color='g')
# Keep a list for a histogram plot (detrainment profile)
if p[ELindex_ent].magnitude < lfc_pressure.magnitude: # buoyant parcels only
ELps.append(p[ELindex_ent].magnitude)
# Plot a crude histogram of parcel detrainment levels
NBINS = 20
pbins = np.linspace(1000, 150,
num=NBINS) # pbins for detrainment levels
hist = np.zeros((len(pbins) - 1))
for x in ELps:
for i in range(len(pbins) - 1):
if (x < pbins[i]) & (x >= pbins[i + 1]):
hist[i] += 1
break
det_per = hist / sum(hist) * 100
# percentages of detrainment ensumbles at levels
ax2 = fig.add_axes([0.705, 0.1, 0.1, 0.8], facecolor=None)
ax2.barh(pbins[1:],
det_per,
color='lightgrey',
edgecolor='k',
height=15 * (20 / NBINS))
ax2.set_xlim([0, 100])
ax2.set_xticks([0, 20, 40, 60, 80, 100])
ax2.set_ylim([1030, 120])
ax2.set_xlabel('Detrainment [%]')
ax2.grid()
ax2.set_zorder(2)
ax.plot([400, 400], [1100, 0])
ax.annotate('Detrainment', xy=(362, 320), color='dimgrey')
ax.annotate('ensemble: ' + str(ensemble_size * len(entrainment_rates)),
xy=(364, 340),
color='dimgrey')
ax.annotate('Detrainment', xy=(362, 380), color='dimgrey')
ax.annotate(' scale: 0 - 2 km', xy=(365, 400), color='dimgrey')
# Overplots on the mess: undilute parcel and CAPE, etc.
ax.plot((1, 1) * sm1[0], (1, 0) * (p[0]), color='g', linewidth=2)
# Replot the sounding on top of all that mess
ax.plot(sm2, p, color='r', linewidth=1.5)
ax.plot(sm1, p, color='b', linewidth=1.5)
# label LCL and LCF
ax.plot((sm2[lcl_idx] + (-2000, 2000) * units('joule/kilogram')),
lcl_pressure + (0, 0) * units('mbar'),
color='orange',
linewidth=3)
ax.plot((sm2[lfc_idx] + (-2000, 2000) * units('joule/kilogram')),
lfc_pressure + (0, 0) * units('mbar'),
color='magenta',
linewidth=3)
# Plot a crude histogram of parcel detrainment levels
# Text parts
ax.text(30, pressure[3], 'RH (%)', fontsize=11, color='k')
ax.text(20,
200,
'CAPE = ' + str(np.around(CAPE.magnitude, decimals=2)) + ' [J/kg]',
fontsize=12,
color='green')
ax.text(20,
250,
'CIN = ' + str(np.around(CIN.magnitude, decimals=2)) + ' [J/kg]',
fontsize=12,
color='green')
ax.text(20,
300,
'LCL = ' + str(np.around(lcl_pressure.magnitude, decimals=2)) +
' [hpa]',
fontsize=12,
color='darkorange')
ax.text(20,
350,
'LFC = ' + str(np.around(lfc_pressure.magnitude, decimals=2)) +
' [hpa]',
fontsize=12,
color='magenta')
ax.text(20,
400,
'CWV = ' + str(np.around(cwv.magnitude, decimals=2)) + ' [mm]',
fontsize=12,
color='deepskyblue')
ax.text(20,
450,
'CRH = ' + str(np.around(crh.magnitude, decimals=2)) + ' [%]',
fontsize=12,
color='blue')
ax.legend(['DEnt', 'MEnt', 'SMEnt'], fontsize=12, loc=1)
ax.set_zorder(3)
return (ax)
def plot_soundings(fig,ax,temp,rh,centerlat,centerlon,domainsize,cape):
'''
This function will plot a bunch of little soundings onto a matplotlib fig,ax.
temp is an xarray dataarray with temperature data on pressure levels at least
between 1000 and 300mb (you can change the ylimits for other datasets)
rh is an xarray dataarray with temperature data on pressure levels at least
between 1000 and 300mb (you can change )
centerlat and centerlon are the coordinates around which you want your map
to be centered. both are floats or integers and are in degrees of latitude
and degrees of longitude west (i.e. 70W would be input as positive 70 here)
domainsize is a string either 'local' for ~WFO-size domains or 'regional' for
NE/SE/Mid-Atlantic-size domains (12 deg lat by 15 deg lon). More will be added soon.
cape is a boolean to indicate whether you want to overlay parcel paths and
shade CAPE/CIN on soundings with >100 J/kg of CAPE (this value can be changed)
note that this function doesn't "return" anything but if you just call it and
provide the right arguments, it works.
for example:
import soundingmaps as smap
...
smap.plot_soundings(fig,ax1,data['temperature'],data['rh'],30.5,87.5,'local',cape=True)
'''
r=5
if domainsize=='local':
init_lat_delt = 1.625
init_lon_delt = 0.45
lat_delts = [.2,.7,1.2,1.75,2.25,2.8]
londelt = 0.76
startlon = centerlon-2+0.45
elif domainsize=='regional':
init_lat_delt = 6
init_lon_delt = 1.6
lat_delts = [0.6,2.5,4.5,6.4,8.4,10.25]
londelt = 2.9
startlon = centerlon-7.5+1.6
startlat = centerlat-init_lat_delt
startlon = centerlon-2+0.45
sound_lats=[]
sound_lons=[]
for i in range(0,6):
lats = startlat+lat_delts[i]
sound_lats.append(lats)
for i in range(0,r):
lons = -startlon-(londelt*i)
sound_lons.append(lons)
plot_elevs=[0.2,0.3,0.4,0.5,0.6,0.7]
dashed_red_line = lines.Line2D([], [], linestyle='solid', color='r', label='Temperature')
dashed_purple_line = lines.Line2D([],[],linestyle='dashed',color='purple',label='0C Isotherm')
dashed_green_line = lines.Line2D([], [], linestyle='solid', color='g', label='Dew Point')
grey_line = lines.Line2D([], [], color='darkgray', label='MSLP (hPa)')
blue_line = lines.Line2D([], [], color='b',label='2m 0C Isotherm')
pink_line = lines.Line2D([], [], color='fuchsia',label='Surface-Based Parcel Path')
red = mpatches.Patch(color='tab:red',label='CAPE')
blue = mpatches.Patch(color='tab:blue',label='CIN')
if cape==True:
for k in range(len(plot_elevs)):
soundlat = sound_lats[k]
plot_elev = plot_elevs[k]
if k==0:
s=1
else:
s=0
for i in range(s,r):
sound_pres = temp.lev
soundlon = -(startlon+(londelt*i))
sound_temps = temp.interp(lat=soundlat,lon=soundlon)-273.15
sound_rh = rh.interp(lat=soundlat,lon=soundlon)
sound_dp = mpcalc.dewpoint_from_relative_humidity(sound_temps.data*units.degC,sound_rh.data*units.percent)
skew = SkewT(fig=fig,rect=(0.75-(0.15*i),plot_elev,.15,.1))
parcel_prof = mpcalc.parcel_profile(sound_pres,sound_temps[0].data*units.degC,sound_dp[0])
cape = mpcalc.cape_cin(sound_pres,sound_temps.data*units.degC,sound_dp,parcel_prof)
capeout = int(cape[0].m)
cinout = int(cape[1].m)
skew.plot(sound_pres,sound_dp,'g',linewidth=3)
skew.plot(sound_pres,sound_temps,'r',linewidth=3)
if capeout >100:
# Shade areas of CAPE and CIN
print(sound_temps)
print(parcel_prof)
skew.shade_cin(sound_pres, sound_temps.data*units.degC, parcel_prof)
skew.shade_cape(sound_pres, sound_temps.data*units.degC, parcel_prof)
skew.plot(sound_pres,parcel_prof,color='fuchsia',linewidth=1)
skew.ax.axvline(0, color='purple', linestyle='--', linewidth=3)
skew.ax.set_ylim((1000,300))
skew.ax.axis('off')
leg = ax.legend(handles=[dashed_red_line,dashed_green_line,dashed_purple_line,pink_line,red,blue],title='Sounding Legend',loc=4,framealpha=1)
else:
for k in range(len(plot_elevs)):
soundlat = sound_lats[k]
plot_elev = plot_elevs[k]
if k==0:
s=1
else:
s=0
for i in range(s,r):
soundlon = -(startlon+(londelt*i))
sound_pres = temp.lev
sound_temps = temp.interp(lat=soundlat,lon=soundlon)-273.15
sound_rh = rh.interp(lat=soundlat,lon=soundlon)
sound_dp = mpcalc.dewpoint_from_relative_humidity(sound_temps.data*units.degC,sound_rh.data*units.percent)
skew = SkewT(fig=fig,rect=(0.75-(0.15*i),plot_elev,.15,.1))
skew.plot(sound_pres,sound_dp,'g',linewidth=3)
skew.plot(sound_pres,sound_temps,'r',linewidth=3)
skew.ax.axvline(0, color='purple', linestyle='--', linewidth=3)
skew.ax.set_ylim((1000,300))
skew.ax.axis('off')
leg = ax.legend(handles=[dashed_red_line,dashed_green_line,dashed_purple_line],title='Sounding Legend',loc=4,framealpha=1)
def process_skewt(self):
# Calculation
index_p100 = get_pressure_level_index(self.p_i, 100)
lcl_p, lcl_t = mpcalc.lcl(self.p_i[0], self.t_i[0], self.td_i[0])
lfc_p, lfc_t = mpcalc.lfc(self.p_i, self.t_i, self.td_i)
el_p, el_t = mpcalc.el(self.p_i, self.t_i, self.td_i)
prof = mpcalc.parcel_profile(self.p_i, self.t_i[0], self.td_i[0]).to('degC')
cape, cin = mpcalc.cape_cin(self.p_i, self.t_i, self.td_i, prof)
mucape, mucin = mpcalc.most_unstable_cape_cin(self.p_i, self.t_i, self.td_i)
pwat = mpcalc.precipitable_water(self.td_i, self.p_i)
i8 = get_pressure_level_index(self.p_i, 850)
i7 = get_pressure_level_index(self.p_i, 700)
i5 = get_pressure_level_index(self.p_i, 500)
theta850 = mpcalc.equivalent_potential_temperature(850 * units('hPa'), self.t_i[i8], self.td_i[i5])
theta500 = mpcalc.equivalent_potential_temperature(500 * units('hPa'), self.t_i[i5], self.td_i[i5])
thetadiff = theta850 - theta500
k = self.t_i[i8] - self.t_i[i5] + self.td_i[i8] - (self.t_i[i7] - self.td_i[i7])
a = ((self.t_i[i8] - self.t_i[i5]) - (self.t_i[i8] - self.td_i[i5]) -
(self.t_i[i7] - self.td_i[i7]) - (self.t_i[i5] - self.td_i[i5]))
sw = c_sweat(np.array(self.t_i[i8].magnitude), np.array(self.td_i[i8].magnitude),
np.array(self.t_i[i5].magnitude), np.array(self.u_i[i8].magnitude),
np.array(self.v_i[i8].magnitude), np.array(self.u_i[i5].magnitude),
np.array(self.v_i[i5].magnitude))
si = showalter_index(self.t_i[i8], self.td_i[i8], self.t_i[i5])
li = lifted_index(self.t_i[0], self.td_i[0], self.p_i[0], self.t_i[i5])
srh_pos, srh_neg, srh_tot = mpcalc.storm_relative_helicity(self.u_i, self.v_i, self.alt, 1000 * units('m'))
sbcape, sbcin = mpcalc.surface_based_cape_cin(self.p_i, self.t_i, self.td_i)
shr6km = mpcalc.bulk_shear(self.p_i, self.u_i, self.v_i, heights=self.alt, depth=6000 * units('m'))
wshr6km = mpcalc.wind_speed(*shr6km)
sigtor = mpcalc.significant_tornado(sbcape, delta_height(self.p_i[0], lcl_p), srh_tot, wshr6km)[0]
# Plotting
self.ax.set_ylim(1050, 100)
self.ax.set_xlim(-40, 50)
self.plot(self.p_i, self.t_i, 'r', linewidth=1)
self.plot(self.p_i[:self.dp_idx], self.td_i[:self.dp_idx], 'g', linewidth=1)
self.plot_barbs(self.p_i[:index_p100], self.u_i[:index_p100] * 1.94, self.v_i[:index_p100] * 1.94)
self.plot(lcl_p, lcl_t, 'ko', markerfacecolor='black')
self.plot(self.p_i, prof, 'k', linewidth=2)
if cin.magnitude < 0:
chi = -1 * cin.magnitude
self.shade_cin(self.p_i, self.t_i, prof)
elif cin.magnitude > 0:
chi = cin.magnitude
self.shade_cin(self.p_i, self.t_i, prof)
else:
chi = 0.
self.shade_cape(self.p_i, self.t_i, prof)
self.plot_dry_adiabats(linewidth=0.5)
self.plot_moist_adiabats(linewidth=0.5)
self.plot_mixing_lines(linewidth=0.5)
plt.title('Skew-T Plot \nStation: {} Time: {}'.format(self.st, self.time.strftime('%Y.%m.%d %H:%M')), fontsize=14, loc='left')
# Add hodograph
ax = self._fig.add_axes([0.95, 0.71, 0.17, 0.17])
h = Hodograph(ax, component_range=50)
h.add_grid(increment=20)
h.plot_colormapped(self.u_i[:index_p100], self.v_i[:index_p100], self.alt[:index_p100], linewidth=1.2)
# Annotate parameters
# Annotate names
namelist = ['CAPE', 'CIN', 'MUCAPE', 'PWAT', 'K', 'A', 'SWEAT', 'LCL', 'LFC', 'EL', 'SI', 'LI', 'T850-500',
'θse850-500', 'SRH', 'STP']
xcor = -50
ycor = -90
spacing = -9
for nm in namelist:
ax.text(xcor, ycor, '{}: '.format(nm), fontsize=10)
ycor += spacing
# Annotate values
varlist = [cape, chi, mucape, pwat, k, a, sw, lcl_p, lfc_p, el_p, si, li, self.t_i[i8] - self.t_i[i5], thetadiff,
srh_tot, sigtor]
xcor = 10
ycor = -90
for v in varlist:
if hasattr(v, 'magnitude'):
v = v.magnitude
ax.text(xcor, ycor, str(np.round_(v, 2)), fontsize=10)
ycor += spacing
# Annotate units
unitlist = ['J/kg', 'J/kg', 'J/kg', 'mm', '°C', '°C', '', 'hPa', 'hPa', 'hPa', '°C', '°C', '°C', '°C']
xcor = 45
ycor = -90
for u in unitlist:
ax.text(xcor, ycor, ' {}'.format(u), fontsize=10)
ycor += spacing
def plot_upper_air(station='11035', date=False):
'''
-----------------------------
Default use of plot_upper_air:
This will plot a SkewT sounding for station '11035' (Wien Hohe Warte)
plot_upper_air(station='11035', date=False)
'''
# sns.set(rc={'axes.facecolor':'#343837', 'figure.facecolor':'#343837',
# 'grid.linestyle':'','axes.labelcolor':'#04d8b2','text.color':'#04d8b2',
# 'xtick.color':'#04d8b2','ytick.color':'#04d8b2'})
# Get time in UTC
station = str(station)
if date is False:
now = datetime.utcnow()
# If morning then 0z sounding, otherwise 12z
if now.hour < 12:
hour = 0
else:
hour = 12
date = datetime(now.year, now.month, now.day, hour)
datestr = date.strftime('%Hz %Y-%m-%d')
print('{}'.format(date))
else:
year = int(input('Please specify the year: '))
month = int(input('Please specify the month: '))
day = int(input('Please specify the day: '))
hour = int(input('Please specify the hour: '))
if hour < 12:
hour = 0
else:
hour = 12
date = datetime(year, month, day, hour)
datestr = date.strftime('%Hz %Y-%m-%d')
print('You entered {}'.format(date))
# This requests the data 11035 is
df = WyomingUpperAir.request_data(date, station)
# Create single variables wih the right units
p = df['pressure'].values * units.hPa
T = df['temperature'].values * units.degC
Td = df['dewpoint'].values * units.degC
wind_speed = df['speed'].values * units.knots
wind_dir = df['direction'].values * units.degrees
wind_speed_6k = df['speed'][df.height <= 6000].values * units.knots
wind_dir_6k = df['direction'][df.height <= 6000].values * units.degrees
u, v = mpcalc.get_wind_components(wind_speed, wind_dir)
u6, v6 = mpcalc.get_wind_components(wind_speed_6k, wind_dir_6k)
# Calculate the LCL
lcl_pressure, lcl_temperature = mpcalc.lcl(p[0], T[0], Td[0])
print(lcl_pressure, lcl_temperature)
# Calculate the parcel profile.
parcel_prof = mpcalc.parcel_profile(p, T[0], Td[0]).to('degC')
cape, cin = mpcalc.cape_cin(p, T, Td, parcel_prof)
#############################
# Create a new figure. The dimensions here give a good aspect ratio
fig = plt.figure(figsize=(9, 9))
gs = gridspec.GridSpec(3, 3)
skew = SkewT(fig, rotation=45, subplot=gs[:, :2])
# Plot the data using normal plotting functions, in this case using
# log scaling in Y, as dictated by the typical meteorological plot
skew.plot(p, T, 'r')
skew.plot(p, Td, 'g')
skew.plot_barbs(p, u, v)
skew.ax.set_ylim(1000, 100)
skew.ax.set_xlim(-45, 40)
# Plot LCL as black dot
skew.plot(lcl_pressure, lcl_temperature, 'ko', markerfacecolor='black')
# Plot the parcel profile as a black line
skew.plot(p, parcel_prof, 'k', linewidth=2)
# Shade areas of CAPE and CIN
skew.shade_cin(p, T, parcel_prof)
skew.shade_cape(p, T, parcel_prof)
# Plot a zero degree isotherm
skew.ax.axvline(0, color='c', linestyle='--', linewidth=2)
skew.ax.set_title('Station: ' + str(station) + '\n' + datestr) # set title
skew.ax.set_xlabel('Temperature (C)')
skew.ax.set_ylabel('Pressure (hPa)')
# Add the relevant special lines
skew.plot_dry_adiabats(linewidth=0.7)
skew.plot_moist_adiabats(linewidth=0.7)
skew.plot_mixing_lines(linewidth=0.7)
# Create a hodograph
# Create an inset axes object that is 40% width and height of the
# figure and put it in the upper right hand corner.
# ax_hod = inset_axes(skew.ax, '40%', '40%', loc=1)
ax = fig.add_subplot(gs[0, -1])
h = Hodograph(ax, component_range=60.)
h.add_grid(increment=20)
# Plot a line colored by windspeed
h.plot_colormapped(u6, v6, wind_speed_6k)
# add another subplot for the text of the indices
# ax_t = fig.add_subplot(gs[1:,2])
skew2 = SkewT(fig, rotation=0, subplot=gs[1:, 2])
skew2.plot(p, T, 'r')
skew2.plot(p, Td, 'g')
# skew2.plot_barbs(p, u, v)
skew2.ax.set_ylim(1000, 700)
skew2.ax.set_xlim(-30, 10)
# Show the plot
plt.show()
return cape
def msed_plots(pressure,
temperature,
mixing_ratio,
h0_std=2000,
ensemble_size=20,
ent_rate=np.arange(0, 2, 0.05),
entrain=False):
"""
plotting the summarized static energy diagram with annotations and thermodynamic parameters
"""
p = pressure * units('mbar')
T = temperature * units('degC')
q = mixing_ratio * units('kilogram/kilogram')
qs = mpcalc.mixing_ratio(mpcalc.saturation_vapor_pressure(T), p)
Td = mpcalc.dewpoint(mpcalc.vapor_pressure(p, q)) # dewpoint
Tp = mpcalc.parcel_profile(p, T[0], Td[0]).to('degC') # parcel profile
# Altitude based on the hydrostatic eq.
altitude = np.zeros((np.size(T))) * units('meter') # surface is 0 meter
for i in range(np.size(T)):
altitude[i] = mpcalc.thickness_hydrostatic(
p[:i + 1], T[:i + 1]) # Hypsometric Eq. for height
# Static energy calculations
mse = mpcalc.moist_static_energy(altitude, T, q)
mse_s = mpcalc.moist_static_energy(altitude, T, qs)
dse = mpcalc.dry_static_energy(altitude, T)
# Water vapor calculations
p_PWtop = max(200 * units.mbar,
min(p) + 1 * units.mbar) # integrating until 200mb
cwv = mpcalc.precipitable_water(Td, p,
top=p_PWtop) # column water vapor [mm]
cwvs = mpcalc.precipitable_water(
T, p, top=p_PWtop) # saturated column water vapor [mm]
crh = (cwv / cwvs) * 100. # column relative humidity [%]
#================================================
# plotting MSE vertical profiles
fig = plt.figure(figsize=[12, 8])
ax = fig.add_axes([0.1, 0.1, 0.6, 0.8])
ax.plot(dse, p, '-k', linewidth=2)
ax.plot(mse, p, '-b', linewidth=2)
ax.plot(mse_s, p, '-r', linewidth=2)
# mse based on different percentages of relative humidity
qr = np.zeros((9, np.size(qs))) * units('kilogram/kilogram')
mse_r = qr * units('joule/kilogram') # container
for i in range(9):
qr[i, :] = qs * 0.1 * (i + 1)
mse_r[i, :] = mpcalc.moist_static_energy(altitude, T, qr[i, :])
for i in range(9):
ax.plot(mse_r[i, :], p[:], '-', color='grey', linewidth=0.7)
ax.text(mse_r[i, 3].magnitude / 1000 - 1, p[3].magnitude,
str((i + 1) * 10))
# drawing LCL and LFC levels
[lcl_pressure, lcl_temperature] = mpcalc.lcl(p[0], T[0], Td[0])
lcl_idx = np.argmin(np.abs(p.magnitude - lcl_pressure.magnitude))
[lfc_pressure, lfc_temperature] = mpcalc.lfc(p, T, Td)
lfc_idx = np.argmin(np.abs(p.magnitude - lfc_pressure.magnitude))
# conserved mse of air parcel arising from 1000 hpa
mse_p = np.squeeze(np.ones((1, np.size(T))) * mse[0].magnitude)
# illustration of CAPE
el_pressure, el_temperature = mpcalc.el(p, T, Td) # equilibrium level
el_idx = np.argmin(np.abs(p.magnitude - el_pressure.magnitude))
ELps = [el_pressure.magnitude
] # Initialize an array of EL pressures for detrainment profile
[CAPE, CIN] = mpcalc.cape_cin(p[:el_idx], T[:el_idx], Td[:el_idx],
Tp[:el_idx])
plt.plot(mse_p, p, color='green', linewidth=2)
ax.fill_betweenx(p[lcl_idx:el_idx + 1],
mse_p[lcl_idx:el_idx + 1],
mse_s[lcl_idx:el_idx + 1],
interpolate=True,
color='green',
alpha='0.3')
ax.fill_betweenx(p, dse, mse, color='deepskyblue', alpha='0.5')
ax.set_xlabel('Specific static energies: s, h, hs [kJ kg$^{-1}$]',
fontsize=14)
ax.set_ylabel('Pressure [hpa]', fontsize=14)
ax.set_xticks([280, 300, 320, 340, 360, 380])
ax.set_xlim([280, 390])
ax.set_ylim(1030, 120)
if entrain is True:
# Depict Entraining parcels
# Parcel mass solves dM/dz = eps*M, solution is M = exp(eps*Z)
# M=1 at ground without loss of generality
# Distribution of surface parcel h offsets
H0STDEV = h0_std # J/kg
h0offsets = np.sort(np.random.normal(
0, H0STDEV, ensemble_size)) * units('joule/kilogram')
# Distribution of entrainment rates
entrainment_rates = ent_rate / (units('km'))
for h0offset in h0offsets:
h4ent = mse.copy()
h4ent[0] += h0offset
for eps in entrainment_rates:
M = np.exp(eps * (altitude - altitude[0])).to('dimensionless')
# dM is the mass contribution at each level, with 1 at the origin level.
M[0] = 0
dM = np.gradient(M)
# parcel mass is a sum of all the dM's at each level
# conserved linearly-mixed variables like h are weighted averages
hent = np.cumsum(dM * h4ent) / np.cumsum(dM)
# Boolean for positive buoyancy, and its topmost altitude (index) where curve is clippes
posboy = (hent > mse_s)
posboy[0] = True # so there is always a detrainment level
ELindex_ent = np.max(np.where(posboy))
# Plot the curve
plt.plot(hent[0:ELindex_ent + 2],
p[0:ELindex_ent + 2],
linewidth=0.25,
color='g')
# Keep a list for a histogram plot (detrainment profile)
if p[ELindex_ent].magnitude < lfc_pressure.magnitude: # buoyant parcels only
ELps.append(p[ELindex_ent].magnitude)
# Plot a crude histogram of parcel detrainment levels
NBINS = 20
pbins = np.linspace(1000, 150,
num=NBINS) # pbins for detrainment levels
hist = np.zeros((len(pbins) - 1))
for x in ELps:
for i in range(len(pbins) - 1):
if (x < pbins[i]) & (x >= pbins[i + 1]):
hist[i] += 1
break
det_per = hist / sum(hist) * 100
# percentages of detrainment ensumbles at levels
ax2 = fig.add_axes([0.705, 0.1, 0.1, 0.8], facecolor=None)
ax2.barh(pbins[1:],
det_per,
color='lightgrey',
edgecolor='k',
height=15 * (20 / NBINS))
ax2.set_xlim([0, max(det_per)])
ax2.set_ylim([1030, 120])
ax2.set_xlabel('Detrainment [%]')
ax2.grid()
ax2.set_zorder(2)
ax.plot([400, 400], [1100, 0])
ax.annotate('Detrainment', xy=(362, 320), color='dimgrey')
ax.annotate('ensemble: ' + str(ensemble_size * len(entrainment_rates)),
xy=(364, 340),
color='dimgrey')
ax.annotate('Detrainment', xy=(362, 380), color='dimgrey')
ax.annotate(' scale: 0 - 2 km', xy=(365, 400), color='dimgrey')
# Overplots on the mess: undilute parcel and CAPE, etc.
ax.plot((1, 1) * mse[0], (1, 0) * (p[0]), color='g', linewidth=2)
# Replot the sounding on top of all that mess
ax.plot(mse_s, p, color='r', linewidth=1.5)
ax.plot(mse, p, color='b', linewidth=1.5)
# label LCL and LCF
ax.plot((mse_s[lcl_idx] + (-2000, 2000) * units('joule/kilogram')),
lcl_pressure + (0, 0) * units('mbar'),
color='orange',
linewidth=3)
ax.plot((mse_s[lfc_idx] + (-2000, 2000) * units('joule/kilogram')),
lfc_pressure + (0, 0) * units('mbar'),
color='magenta',
linewidth=3)
### Internal waves (100m adiabatic displacements, assumed adiabatic: conserves s, sv, h).
#dZ = 100 *mpunits.units.meter
dp = 1000 * units.pascal
# depict displacements at sounding levels nearest these target levels
targetlevels = [900, 800, 700, 600, 500, 400, 300, 200] * units.hPa
for ilev in targetlevels:
idx = np.argmin(np.abs(p - ilev))
# dp: hydrostatic
rho = (p[idx]) / Rd / (T[idx])
dZ = -dp / rho / g
# dT: Dry lapse rate dT/dz_dry is -g/Cp
dT = (-g / Cp_d * dZ).to('kelvin')
Tdisp = T[idx].to('kelvin') + dT
# dhsat
dqs = mpcalc.mixing_ratio(mpcalc.saturation_vapor_pressure(Tdisp),
p[idx] + dp) - qs[idx]
dhs = g * dZ + Cp_d * dT + Lv * dqs
# Whiskers on the data plots
ax.plot((mse_s[idx] + dhs * (-1, 1)),
p[idx] + dp * (-1, 1),
linewidth=3,
color='r')
ax.plot((dse[idx] * (1, 1)),
p[idx] + dp * (-1, 1),
linewidth=3,
color='k')
ax.plot((mse[idx] * (1, 1)),
p[idx] + dp * (-1, 1),
linewidth=3,
color='b')
# annotation to explain it
if ilev == 400 * ilev.units:
ax.plot(360 * mse_s.units + dhs * (-1, 1) / 1000,
440 * units('mbar') + dp * (-1, 1),
linewidth=3,
color='r')
ax.annotate('+/- 10mb', xy=(362, 440), fontsize=8)
ax.annotate(' adiabatic displacement', xy=(362, 460), fontsize=8)
# Plot a crude histogram of parcel detrainment levels
# Text parts
ax.text(290, pressure[3], 'RH (%)', fontsize=11, color='k')
ax.text(285,
200,
'CAPE = ' + str(np.around(CAPE.magnitude, decimals=2)) + ' [J/kg]',
fontsize=12,
color='green')
ax.text(285,
250,
'CIN = ' + str(np.around(CIN.magnitude, decimals=2)) + ' [J/kg]',
fontsize=12,
color='green')
ax.text(285,
300,
'LCL = ' + str(np.around(lcl_pressure.magnitude, decimals=2)) +
' [hpa]',
fontsize=12,
color='darkorange')
ax.text(285,
350,
'LFC = ' + str(np.around(lfc_pressure.magnitude, decimals=2)) +
' [hpa]',
fontsize=12,
color='magenta')
ax.text(285,
400,
'CWV = ' + str(np.around(cwv.magnitude, decimals=2)) + ' [mm]',
fontsize=12,
color='deepskyblue')
ax.text(285,
450,
'CRH = ' + str(np.around(crh.magnitude, decimals=2)) + ' [%]',
fontsize=12,
color='blue')
ax.legend(['DSE', 'MSE', 'SMSE'], fontsize=12, loc=1)
ax.set_zorder(3)
return (ax)
def EnergyMassPlot(pressure, temperature, dewpoint,
height, uwind, vwind, sphum=None, rh=None,
label='', size=(12,10), return_fig=False):
p=pressure
Z=height
T=temperature
Td=dewpoint
if isinstance(sphum,np.ndarray) and isinstance(rh,np.ndarray):
q=sphum
qs=q/rh
else:
q = mpcalc.mixing_ratio(mpcalc.saturation_vapor_pressure(Td),p)
qs= mpcalc.mixing_ratio(mpcalc.saturation_vapor_pressure(T),p)
s = g*Z + Cp_d*T
sv= g*Z + Cp_d*mpcalc.virtual_temperature(T,q)
h = s + Lv*q
hs= s + Lv*qs
parcel_Tprofile = mpcalc.parcel_profile(p, T[0], Td[0]).to('degC')
CAPE,CIN = mpcalc.cape_cin(p,T,Td,parcel_Tprofile)
ELp,ELT = mpcalc.el(p,T,Td)
ELindex = np.argmin(np.abs(p - ELp))
lcl_pressure, lcl_temperature = mpcalc.lcl(p[0], T[0], Td[0])
p_PWtop = max(200*units.mbar, min(p) +1*units.mbar)
PW = mpcalc.precipitable_water(Td,p, top=p_PWtop)
PWs = mpcalc.precipitable_water(T,p, top=p_PWtop)
CRH = (PW/PWs).magnitude *100.
fig,ax=setup_fig(size=size,label=label)
ax.plot(s /1000, p, color='r', linewidth=1.5) ### /1000 for kJ/kg
ax.plot(sv /1000, p, color='r', linestyle='-.')
ax.plot(h /1000, p, color='b', linewidth=1.5)
ax.plot(hs /1000, p, color='r', linewidth=1.5)
### RH rulings between s and h lines: annotate near 800 hPa level
annot_level = 800 #hPa
idx = np.argmin(np.abs(p - annot_level *units.hPa))
right_annot_loc = 380
for iRH in np.arange(10,100,10):
ax.plot( (s+ Lv*qs*iRH/100.)/1000, p, linewidth=0.5, linestyle=':', color='k')
ax.annotate(str(iRH), xy=( (s[idx]+Lv*qs[idx]*iRH/100.)/1000, annot_level),
horizontalalignment='center',fontsize=6)
ax.annotate('RH (%)', xy=(right_annot_loc, annot_level), fontsize=10)
if not np.isnan(CAPE.magnitude) and CAPE.magnitude >10:
parcelh = h [0] # for a layer mean: np.mean(h[idx1:idx2])
parcelsv = sv[0]
parcelp0 = p[0]
# Undilute parcel
ax.plot( (1,1)*parcelh/1000., (1,0)*parcelp0, linewidth=0.5, color='g')
maxbindex = np.argmax(parcel_Tprofile - T)
ax.annotate('CAPE='+str(int(CAPE.magnitude)),
xy=(parcelh/1000., p[maxbindex]), color='g')
# Plot LCL at saturation point, above the lifted sv of the surface parcel
lcl_pressure, lcl_temperature = mpcalc.lcl(p[0], T[0], Td[0])
ax.annotate('LCL', xy=(sv[0]/1000., lcl_pressure), fontsize=10, color='g', horizontalalignment='right')
# Purple fill for negative buoyancy below LCL:
ax.fill_betweenx(p, sv/1000., parcelsv/1000., where=p>lcl_pressure, facecolor='purple', alpha=0.4)
# Positive moist convective buoyancy in green
# Above LCL:
ax.fill_betweenx(p, hs/1000., parcelh/1000., where= parcelh>hs, facecolor='g', alpha=0.4)
# Depict Entraining parcels
# Parcel mass solves dM/dz = eps*M, solution is M = exp(eps*Z)
# M=1 at ground without loss of generality
entrainment_distance = 10000., 5000., 2000.
ax.annotate('entrain: 10,5,2 km', xy=(parcelh/1000, 140), color='g',
fontsize=8, horizontalalignment='right')
ax.annotate('parcel h', xy=(parcelh/1000, 120), color='g',
fontsize=10, horizontalalignment='right')
for ED in entrainment_distance:
eps = 1.0 / (ED*units.meter)
M = np.exp(eps * (Z-Z[0]).to('m')).to('dimensionless')
# dM is the mass contribution at each level, with 1 at the origin level.
M[0] = 0
dM = np.gradient(M)
# parcel mass is a sum of all the dM's at each level
# conserved linearly-mixed variables like h are weighted averages
hent = np.cumsum(dM*h) / np.cumsum(dM)
ax.plot( hent[0:ELindex+3]/1000., p[0:ELindex+3], linewidth=0.5, color='g')
### Internal waves (100m adiabatic displacements, assumed adiabatic: conserves s, sv, h).
dZ = 100 *units.meter
# depict displacements at sounding levels nearest these target levels
targetlevels = [900,800,700,600,500,400,300,200]*units.hPa
for ilev in targetlevels:
idx = np.argmin(np.abs(p - ilev))
# dT: Dry lapse rate dT/dz_dry is -g/Cp
dT = (-g/Cp_d *dZ).to('kelvin')
Tdisp = T[idx].to('kelvin') + dT
# dp: hydrostatic
rho = (p[idx]/Rd/T[idx])
dp = -rho*g*dZ
# dhsat
#qs = mpcalc.mixing_ratio(mpcalc.saturation_vapor_pressure(T) ,p)
dqs = mpcalc.mixing_ratio(mpcalc.saturation_vapor_pressure(Tdisp) ,p[idx]+dp) -qs[idx]
dhs = g*dZ + Cp_d*dT + Lv*dqs
# Whiskers on the data plots
ax.plot( (hs[idx]+dhs*(-1,1))/1000, p[idx]+dp*(-1,1), linewidth=3, color='r')
ax.plot( (s [idx] *( 1,1))/1000, p[idx]+dp*(-1,1), linewidth=3, color='r')
ax.plot( (h [idx] *( 1,1))/1000, p[idx]+dp*(-1,1), linewidth=3, color='b')
# annotation to explain it
if ilev == 600*ilev.units:
ax.plot(right_annot_loc*hs.units +dhs*(-1,1)/1000, p[idx]+dp*(-1,1), linewidth=3, color='r')
ax.annotate('+/- 100m', xy=(right_annot_loc,600), fontsize=8)
ax.annotate(' internal', xy=(right_annot_loc,630), fontsize=8)
ax.annotate(' waves', xy=(right_annot_loc,660), fontsize=8)
### Blue fill proportional to precipitable water, and blue annotation
ax.fill_betweenx(p, s/1000., h/1000., where=h > s, facecolor='b', alpha=0.4)
# Have to specify the top of the PW integral.
# I want whole atmosphere of course, but 200 hPa captures it all really.
#import metpy.calc as mpcalc
p_PWtop = max(200*units.mbar, min(p) +1*units.mbar)
PW = mpcalc.precipitable_water(Td,p, top=p_PWtop)
PWs = mpcalc.precipitable_water(T,p, top=p_PWtop)
CRH = (PW/PWs).magnitude *100.
# PW annotation arrow tip at 700 mb
idx = np.argmin(np.abs(p - 700*p.units))
centerblue = (s[idx]+h[idx])/2.0 /1000.
ax.annotate('CWV='+str(round(PW.to('mm').magnitude, 1))+'mm',
xy=(centerblue, 700), xytext=(285, 200),
color='blue', fontsize=15,
arrowprops=dict(width = 1, edgecolor='blue', shrink=0.02),
)
ax.annotate('(' + str(round(CRH,1)) +'% of sat)',
xy=(285, 230), color='blue', fontsize=12)
### Surface water values at 1C intervals, for eyeballing surface fluxes
sT = np.trunc(T[0].to('degC'))
sTint = int(sT.magnitude)
for idT in [-2,0,2,4]:
ssTint = sTint + idT # UNITLESS degC integers, for labels
# Kelvin values for computations
ssTC = ssTint * units.degC
ssTK = ssTC.to('kelvin')
ss = g*Z[0] + Cp_d*ssTK
hs = ss + Lv*mpcalc.mixing_ratio(mpcalc.saturation_vapor_pressure(ssTK) ,p[0])
ax.annotate(str(ssTint), xy=(ss/1000., p[0]+0*p.units),
verticalalignment='top', horizontalalignment='center',
color='red', fontsize=7)
ax.annotate(str(ssTint), xy=(hs/1000., p[0]+0*p.units),
verticalalignment='top', horizontalalignment='center',
color='red', fontsize=9)
ax.annotate('\u00b0C water', xy=(right_annot_loc, p[0]), verticalalignment='top',
fontsize=10, color='r')
if return_fig:
return ax,fig
'dewpoint': Td,
'speed': ws,
'direction': wd
})
p = df['pressure'].values * units.hPa
T = df['temperature'].values * units.degC
Td = df['dewpoint'].values * units.degC
wind_speed = df['speed'].values * units.meter / (units.second)
wind_dir = df['direction'].values * units.degrees
u, v = mpcalc.wind_components(wind_speed, wind_dir)
lcl_pressure, lcl_temperature = mpcalc.lcl(p[0], T[0], Td[0])
lfc_pressure, lfc_temperature = mpcalc.lfc(p, T, Td)
parcel_prof = mpcalc.parcel_profile(p, T[0], Td[0]).to('degC')
cape, cin = mpcalc.cape_cin(p, T, Td, parcel_prof)
fig = plt.figure(figsize=(12., 9.))
fig.subplots_adjust(top=0.9,
bottom=0.1,
left=0.05,
right=0.96,
wspace=0.08,
hspace=0.25)
gs = gridspec.GridSpec(21, 5)
skew = SkewT(fig, subplot=gs[:, :4], rotation=45)
# Plot the data using normal plotting functions, in this case using
# log scaling in Y, as dictated by the typical meteorological plot
skip = 100
skew.plot(p, T, 'r', linewidth=3)
def cape_cin(self, index_from):
return mpcalc.cape_cin(self.p[index_from:], self.T[index_from:],
self.Td[index_from:],
self.parcel_trace(index_from))
def fmi2skewt(station, time, img_name):
apikey = 'e72a2917-1e71-4d6f-8f29-ff4abfb8f290'
url = 'http://data.fmi.fi/fmi-apikey/' + str(
apikey
) + '/wfs?request=getFeature&storedquery_id=fmi::observations::weather::sounding::multipointcoverage&fmisid=' + str(
station) + '&starttime=' + str(time) + '&endtime=' + str(time) + '&'
req = requests.get(url)
xmlstring = req.content
tree = ET.ElementTree(ET.fromstring(xmlstring))
root = tree.getroot()
#reading location and time data to "positions" from XML
positions = ""
for elem in root.getiterator(
tag='{http://www.opengis.net/gmlcov/1.0}positions'):
positions = elem.text
#'positions' is string type variable
#--> split positions into a list by " "
#then remove empty chars and "\n"
# from pos_split --> data into positions_data
try:
pos_split = positions.split(' ')
except NameError:
return "Sounding data not found: stationid " + station + " time " + time
pos_split = positions.split(' ')
positions_data = []
for i in range(0, len(pos_split)):
if not (pos_split[i] == "" or pos_split[i] == "\n"):
positions_data.append(pos_split[i])
#index for height: 2,6,10 etc in positions_data
height = []
myList = range(2, len(positions_data))
for i in myList[::4]:
height.append(positions_data[i])
p = []
for i in range(0, len(height)):
p.append(height2pressure(float(height[i])))
#reading wind speed, wind direction, air temperature and dew point data to 'values'
values = ""
for elem in root.getiterator(
tag='{http://www.opengis.net/gml/3.2}doubleOrNilReasonTupleList'):
values = elem.text
#split 'values' into a list by " "
#then remove empty chars and "\n"
val_split = values.split(' ')
values_data = []
for i in range(0, len(val_split)):
if not (val_split[i] == "" or val_split[i] == "\n"):
values_data.append(val_split[i])
#data in values_data: w_speed, w_dir, t_air, t_dew
wind_speed = []
wind_dir = []
T = []
Td = []
myList = range(0, len(values_data))
for i in myList[::4]:
wind_speed.append(float(values_data[i]))
wind_dir.append(float(values_data[i + 1]))
T.append(float(values_data[i + 2]))
Td.append(float(values_data[i + 3]))
if stationid == "101104":
loc_time = "Jokioinen Ilmala " + time
elif stationid == "101932":
loc_time = "Sodankyla Tahtela " + time
else:
return None
#calculate wind components u,v:
u = []
v = []
for i in range(0, len(wind_speed)):
u1, v1 = getWindComponent(wind_speed[i], wind_dir[i])
u.append(u1)
v.append(v1)
#find index for pressure < 100hPa (for number of wind bars)
if min(p) > 100:
wthin = len(p) / 20
u_plot = u
v_plot = v
p_plot = p
else:
for i in range(0, len(p)):
if p[i] - 100 <= 0:
wthin = i / 20
u_plot = u[0:i]
v_plot = v[0:i]
p_plot = p[0:i]
break
#units
wind_speed = wind_speed * units("m/s")
wind_dir = wind_dir * units.deg
T = T * units.degC
Td = Td * units.degC
p = p * units("hPa")
#calculate pwat, lcl, cape, cin and plot cape
pwat = mpcalc.precipitable_water(Td, p, bottom=None, top=None)
lcl_pressure, lcl_temperature = mpcalc.lcl(p[0], T[0], Td[0])
prof = mpcalc.parcel_profile(p, T[0], Td[0]).to('degC')
try:
cape, cin = mpcalc.cape_cin(p, T, Td, prof)
except IndexError:
cape = 0 * units("J/kg")
cin = 0 * units("J/kg")
#__________________plotting__________________
fig = plt.figure(figsize=(9, 9))
skew = SkewT(fig, rotation=45)
font_par = {
'family': 'monospace',
'color': 'darkred',
'weight': 'normal',
'size': 10,
}
font_title = {
'family': 'monospace',
'color': 'black',
'weight': 'normal',
'size': 20,
}
font_axis = {
'family': 'monospace',
'color': 'black',
'weight': 'normal',
'size': 10,
}
# Plot the data using normal plotting functions, in this case using
# log scaling in Y, as dictated by the typical meteorological plot
skew.plot(p, T, 'k')
skew.plot(p, Td, 'b')
skew.ax.set_ylim(1000, 100)
skew.ax.set_xlim(-50, 30)
skew.plot_barbs(p_plot[0::wthin], u_plot[0::wthin], v_plot[0::wthin])
skew.plot_dry_adiabats(alpha=0.4)
skew.plot_moist_adiabats(alpha=0.4)
skew.plot_mixing_lines(alpha=0.4)
#skew.shade_cape(p, T, prof,color="orangered")
plt.title(loc_time, fontdict=font_title)
plt.xlabel("T (C)", fontdict=font_axis)
plt.ylabel("P (hPa)", fontdict=font_axis)
#round and remove units from cape,cin,plcl,tlcl,pwat
if cape.magnitude > 0:
capestr = str(np.round(cape.magnitude))
else:
capestr = "NaN"
if cin.magnitude > 0:
cinstr = str(np.round(cin.magnitude))
else:
cinstr = "NaN"
lclpstr = str(np.round(lcl_pressure.magnitude))
lclTstr = str(np.round(lcl_temperature.magnitude))
pwatstr = str(np.round(pwat.magnitude))
# str_par = "CAPE[J/kg]=" + capestr + " CIN[J/kg]=" + cinstr + " Plcl[hPa]=" + lclpstr + " Tlcl[C]=" + lclTstr + " pwat[mm]=" + pwatstr
# font = {'family': 'monospace',
# 'color': 'darkred',
# 'weight': 'normal',
# 'size': 10,
# }
# plt.text(-20,1250,str_par,fontdict=font_par)
save_file = img_name
plt.savefig(save_file)
def plot_soundings(fig,
ax,
temp,
rh,
sfc_pressure,
centerlat,
centerlon,
domainsize,
model,
cape=False,
wetbulb=False):
"""
This function will plot a bunch of little soundings onto a matplotlib fig,ax.
temp is an xarray dataarray with temperature data on pressure levels at least
between 1000 and 300mb (you can change the ylimits for other datasets)
rh is an xarray dataarray with temperature data on pressure levels at least
between 1000 and 300mb (you can change )
sfc_pressure is an xarray dataarray with surface pressure data (NOT MSLP!)
centerlat and centerlon are the coordinates around which you want your map
to be centered. both are floats or integers and are in degrees of latitude
and degrees of longitude west (i.e. 70W would be input as positive 70 here)
domainsize is a string either 'local' for ~WFO-size domains or 'regional' for
NE/SE/Mid-Atlantic-size domains (12 deg lat by 15 deg lon). More will be added soon.
model is a string that specifies which model is providing data for the plots.
This determines a few things, most importantly longitude selections. Models
currently supported are 'GFS','NAM',and 'RAP'
cape is a boolean to indicate whether you want to overlay parcel paths and
shade CAPE/CIN on soundings with >100 J/kg of CAPE (this value can be changed)
wetbulb is a boolean to indicate whether you want to draw wet bulb profiles
note that this function doesn't "return" anything but if you just call it and
provide the right arguments, it works.
for example:
import soundingmaps as smap
...
smap.plot_soundings(fig,ax1,data['temperature'],data['rh'],30.5,87.5,'local',cape=True)
"""
r = 5
if domainsize == "local":
init_lat_delt = 1.625
init_lon_delt = 0.45
lat_delts = [0.2, 0.7, 1.2, 1.75, 2.25, 2.8]
londelt = 0.76
startlon = centerlon - 2 + 0.45
elif domainsize == "regional":
init_lat_delt = 6
init_lon_delt = 1.6
lat_delts = [0.6, 2.5, 4.5, 6.4, 8.4, 10.25]
londelt = 2.9
startlon = centerlon - 7.5 + 1.6
# Lon adjustment for GFS because it's [0,360] not [-180,180]
if model == 'GFS':
startlon = 360 - startlon
# set lat/lon grid from which to pull data to plot soundings
startlat = centerlat - init_lat_delt
sound_lats = []
sound_lons = []
for i in range(0, 6):
lats = startlat + lat_delts[i]
sound_lats.append(lats)
for i in range(0, r):
if model == 'GFS':
lons = startlon - (londelt * i)
else:
lons = -startlon - (londelt * i)
sound_lons.append(lons)
# this sets how high each row of soundings is on the plot
plot_elevs = [0.2, 0.3, 0.4, 0.5, 0.6, 0.7]
# whole bunch of legend stuff
dashed_red_line = lines.Line2D([], [],
linestyle='solid',
color='r',
label='Temperature')
dashed_purple_line = lines.Line2D([], [],
linestyle='dashed',
color='purple',
label='0C Isotherm')
dashed_green_line = lines.Line2D([], [],
linestyle='solid',
color='g',
label='Dew Point')
grey_line = lines.Line2D([], [], color='darkgray', label='MSLP (hPa)')
blue_line = lines.Line2D([], [], color='b', label='Wet Bulb')
pink_line = lines.Line2D([], [],
color='fuchsia',
label='Surface-Based Parcel Path')
teal_line = lines.Line2D([], [],
linestyle='dashed',
color='teal',
label='HGZ')
green_dot = lines.Line2D([], [],
marker='o',
color='forestgreen',
label='LCL')
black_dot = lines.Line2D([], [],
marker='o',
color='k',
label='Sounding Origin')
red = mpatches.Patch(color='tab:red', label='CAPE')
blue = mpatches.Patch(color='tab:blue', label='CIN')
# do the plotting based on user inputs
if cape and wetbulb is True:
print('CAPE + Wetbulb')
for i, plot_elev in enumerate(plot_elevs):
soundlat = sound_lats[i]
if k < 2:
s = 1
else:
s = 0
for i in range(s, r):
levs_abv_ground = []
soundlon = sound_lons[i]
sound_temps = temp.interp(lat=soundlat, lon=soundlon) - 273.15
sound_rh = rh.interp(lat=soundlat, lon=soundlon)
sound_pres = temp.lev
spres = sfc_pressure.interp(lat=soundlat, lon=soundlon)
sound_dp = mpcalc.dewpoint_from_relative_humidity(
sound_temps.data * units.degC,
sound_rh.data * units.percent)
sound_wb = mpcalc.wet_bulb_temperature(
sound_pres, sound_temps.data * units.degC, sound_dp)
#Only want data above the ground
abv_sfc_temp = spt.mask_below_terrain(spres, sound_temps,
sound_pres)[0]
abv_sfc_dewp = spt.mask_below_terrain(spres, sound_dp,
sound_pres)[0]
abv_sfc_wetb = spt.mask_below_terrain(spres, sound_wb,
sound_pres)[0]
pres_abv_ground = spt.mask_below_terrain(
spres, sound_temps, sound_pres)[1]
#sound_wb = sound_wb*units.degC
skew = SkewT(fig=fig,
rect=(0.75 - (0.15 * i), plot_elev, .15, .1))
parcel_prof = mpcalc.parcel_profile(
pres_abv_ground, abv_sfc_temp[0].data * units.degC,
abv_sfc_dewp[0])
cape = mpcalc.cape_cin(pres_abv_ground,
abv_sfc_temp.data * units.degC,
abv_sfc_dewp, parcel_prof)
capeout = int(cape[0].m)
cinout = int(cape[1].m)
#skew.ax.axvspan(-30, -10, color='cyan', alpha=0.4)
skew.plot(pres_abv_ground, abv_sfc_wetb, 'b', linewidth=2)
skew.plot(pres_abv_ground, abv_sfc_dewp, 'g', linewidth=3)
skew.plot(pres_abv_ground, abv_sfc_temp, 'r', linewidth=3)
if capeout > 100:
# Shade areas of CAPE and CIN
print(pres_abv_ground)
print(abv_sfc_temp.data * units.degC)
print(parcel_prof)
skew.shade_cin(pres_abv_ground,
abv_sfc_temp.data * units.degC, parcel_prof)
skew.shade_cape(pres_abv_ground,
abv_sfc_temp.data * units.degC,
parcel_prof)
skew.plot(pres_abv_ground,
parcel_prof,
color='fuchsia',
linewidth=1)
lcl_pressure, lcl_temperature = mpcalc.lcl(
pres_abv_ground[0], abv_sfc_temp.data[0] * units.degC,
abv_sfc_dewp[0])
skew.plot(lcl_pressure,
lcl_temperature,
'ko',
markerfacecolor='forestgreen')
skew.ax.axvline(-30,
color='teal',
linestyle='--',
linewidth=1)
skew.ax.axvline(-10,
color='teal',
linestyle='--',
linewidth=1)
skew.plot(975, 0, 'ko', markerfacecolor='k')
skew.ax.axvline(0, color='purple', linestyle='--', linewidth=3)
skew.ax.set_ylim((1000, 300))
skew.ax.axis('off')
leg = ax.legend(handles=[
dashed_red_line, dashed_green_line, blue_line, dashed_purple_line,
teal_line, green_dot, pink_line, red, blue, black_dot
],
title='Sounding Legend',
loc=4,
framealpha=1)
elif cape == True and wetbulb == False:
print('CAPE no wetbulb')
for k in range(len(plot_elevs)):
soundlat = sound_lats[k]
plot_elev = plot_elevs[k]
if k == 0:
s = 1
else:
s = 0
for i in range(s, r):
levs_abv_ground = []
soundlon = sound_lons[i]
sound_temps = temp.interp(lat=soundlat, lon=soundlon) - 273.15
sound_rh = rh.interp(lat=soundlat, lon=soundlon)
sound_pres = temp.lev
spres = sfc_pressure.interp(lat=soundlat, lon=soundlon)
sound_dp = mpcalc.dewpoint_from_relative_humidity(
sound_temps.data * units.degC,
sound_rh.data * units.percent)
abv_sfc_temp = spt.mask_below_terrain(spres, sound_temps,
sound_pres)[0]
abv_sfc_dewp = spt.mask_below_terrain(spres, sound_dp,
sound_pres)[0]
pres_abv_ground = spt.mask_below_terrain(
spres, sound_temps, sound_pres)[1]
skew = SkewT(fig=fig,
rect=(0.75 - (0.15 * i), plot_elev, .15, .1))
parcel_prof = mpcalc.parcel_profile(
pres_abv_ground, abv_sfc_temp[0].data * units.degC,
abv_sfc_dewp[0])
cape = mpcalc.cape_cin(pres_abv_ground,
abv_sfc_temp.data * units.degC,
abv_sfc_dewp, parcel_prof)
capeout = int(cape[0].m)
cinout = int(cape[1].m)
skew.plot(pres_abv_ground, abv_sfc_dewp, 'g', linewidth=3)
skew.plot(pres_abv_ground, abv_sfc_temp, 'r', linewidth=3)
if capeout > 100:
# Shade areas of CAPE and CIN
skew.shade_cin(pres_abv_ground,
abv_sfc_temp.data * units.degC, parcel_prof)
skew.shade_cape(pres_abv_ground,
abv_sfc_temp.data * units.degC,
parcel_prof)
skew.plot(pres_abv_ground,
parcel_prof,
color='fuchsia',
linewidth=1)
print(abv_sfc_temp)
lcl_pressure, lcl_temperature = mpcalc.lcl(
pres_abv_ground[0], abv_sfc_temp.data[0] * units.degC,
abv_sfc_dewp[0])
skew.plot(lcl_pressure,
lcl_temperature,
'ko',
markerfacecolor='forestgreen')
skew.ax.axvline(-30,
color='teal',
linestyle='--',
linewidth=1)
skew.ax.axvline(-10,
color='teal',
linestyle='--',
linewidth=1)
skew.plot(975, 0, 'ko', markerfacecolor='k')
skew.ax.axvline(0, color='purple', linestyle='--', linewidth=3)
skew.ax.set_ylim((1000, 300))
skew.ax.axis('off')
leg = ax.legend(handles=[
dashed_red_line, dashed_green_line, dashed_purple_line, teal_line,
green_dot, pink_line, red, blue, black_dot
],
title='Sounding Legend',
loc=4,
framealpha=1)
elif wetbulb == True and cape == False:
print('Wetbulb no CAPE')
for k in range(len(plot_elevs)):
soundlat = sound_lats[k]
plot_elev = plot_elevs[k]
if k == 0:
s = 1
else:
s = 0
for i in range(s, r):
levs_abv_ground = []
soundlon = sound_lons[i]
sound_temps = temp.interp(lat=soundlat, lon=soundlon) - 273.15
sound_rh = rh.interp(lat=soundlat, lon=soundlon)
sound_pres = temp.lev
spres = sfc_pressure.interp(lat=soundlat, lon=soundlon)
sound_dp = mpcalc.dewpoint_from_relative_humidity(
sound_temps.data * units.degC,
sound_rh.data * units.percent)
sound_wb = mpcalc.wet_bulb_temperature(
sound_pres, sound_temps.data * units.degC, sound_dp)
abv_sfc_temp = spt.mask_below_terrain(spres, sound_temps,
sound_pres)[0]
abv_sfc_dewp = spt.mask_below_terrain(spres, sound_dp,
sound_pres)[0]
abv_sfc_wetb = spt.mask_below_terrain(spres, sound_wb,
sound_pres)[0]
pres_abv_ground = spt.mask_below_terrain(
spres, sound_temps, sound_pres)[1]
#sound_wb = sound_wb*units.degC
skew = SkewT(fig=fig,
rect=(0.75 - (0.15 * i), plot_elev, .15, .1))
skew.plot(pres_abv_ground, abv_sfc_wetb, 'b', linewidth=2)
skew.plot(pres_abv_ground, abv_sfc_dewp, 'g', linewidth=3)
skew.plot(pres_abv_ground, abv_sfc_temp, 'r', linewidth=3)
skew.ax.axvline(0, color='purple', linestyle='--', linewidth=3)
skew.ax.set_ylim((1000, 300))
skew.ax.axis('off')
else:
print('No Wetbulb or CAPE')
for k in range(len(plot_elevs)):
soundlat = sound_lats[k]
plot_elev = plot_elevs[k]
if k == 0:
s = 1
else:
s = 0
for i in range(s, r):
sound_pres = temp.lev
sound_temps = temp.interp(lat=soundlat, lon=soundlon) - 273.15
sound_rh = rh.interp(lat=soundlat, lon=soundlon)
sound_dp = mpcalc.dewpoint_from_relative_humidity(
sound_temps.data * units.degC,
sound_rh.data * units.percent)
skew = SkewT(fig=fig,
rect=(0.75 - (0.15 * i), plot_elev, .15, .1))
skew.plot(sound_pres, sound_dp, 'g', linewidth=3)
skew.plot(sound_pres, sound_temps, 'r', linewidth=3)
skew.plot(1000, 0, 'ko', markerfacecolor='k')
skew.ax.axvline(0, color='purple', linestyle='--', linewidth=3)
skew.ax.set_ylim((1000, 300))
skew.ax.axis('off')
leg = ax.legend(handles=[
dashed_red_line, dashed_green_line, blue_line, dashed_purple_line,
black_dot
],
title='Sounding Legend',
loc=4,
framealpha=1)
