def Wavebreaking_modulation(kr, K, theta, azimuth, u_10, fetch, wind_dir, tsc,
                            polarization):
    """
    :param kp:
    :param kr:
    :param theta:
    :param azi:
    :param u_10:
    :param fetch:
    :return:
    """
    if polarization == 'VH':
        print('no modulation cross-pol')
        return

    nphi = theta.shape[0]

    ind = np.where(np.degrees(azimuth) == wind_dir)[0]

    # divergence of the sea surface current
    divergence = np.gradient(tsc[:, :, 0], 1e3, axis=1) + np.gradient(
        tsc[:, :, 1], 1e3, axis=0)

    # NRCS of plumes
    wb0 = np.exp(-np.tan(theta)**2 / const.Swb) / (
        np.cos(theta)**4 * const.Swb
    ) + const.yitawb / const.Swb  # Kudryavstev 2003a equation (60)
    knb = min(const.br * kr, const.kwb)

    # tilting transfer function
    dtheta = theta[1] - theta[0]
    Mwb = np.gradient(wb0, dtheta) / wb0

    # distribution function
    # in radians azimuth of breaking surface area: -pi/2,pi/2
    # phi1 = np.linspace(-np.pi/2, np.pi/2, nphi)
    phi1 = np.linspace(-np.pi, np.pi, nphi)
    nk = 1024

    q = np.zeros([tsc.shape[0], tsc.shape[1]])
    WB = np.zeros([tsc.shape[0], tsc.shape[1]])

    for ii in np.arange(tsc.shape[0]):
        for jj in np.arange(tsc.shape[1]):
            KK = np.linspace(10 * spec_peak(u_10[ii, jj], fetch), knb, nk)
            T = Trans_func(KK, K[ii, jj], u_10[ii, jj], fetch, azimuth,
                           divergence[ii, jj])
            Bkdir = kudryavtsev05(KK.reshape(nk, 1), u_10[ii, jj], fetch,
                                  phi1) * (1 + abs(T.reshape(nk, 1)))
            n, alpha = param(KK, u_10[ii, jj], fetch)
            lamda = (Bkdir / alpha.reshape(nk, 1))**(n.reshape(nk, 1) + 1) / (
                2 * KK.reshape(nk, 1)
            )  # distribution of breaking front lengths
            lamda_k = np.trapz(lamda, phi1, axis=1)
            lamda = np.trapz(lamda, KK, axis=0)
            lamda_k = np.trapz(lamda_k, KK)
            q[ii, jj] = const.cq * lamda_k
            Awb = np.trapz(np.cos(phi1 - azimuth[ind]) * lamda, phi1) / lamda_k
            WB[ii, jj] = wb0[jj] * (1 + Mwb[jj] * const.theta_wb * Awb)
    return WB, q
Exemplo n.º 2
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def eq_wb(kr, theta_eq, eq_azi, u_10, fetch, spec_name, polarization):
    """
    :param kp:
    :param kr:
    :param theta:
    :param azi:
    :param u_10:
    :param fetch:
    :return:
    """

    nphi = theta_eq.shape[0]
    # Spectral model
    # Omni directional spectrum model name
    specf = spec.models[spec_name]

    # NRCS of plumes
    wb0 = np.exp(-np.tan(theta_eq)**2 / const.Swb) / (
        np.cos(theta_eq)**4 * const.Swb
    ) + const.yitawb / const.Swb  # Kudryavstev 2003a equation (60)
    knb = min(const.br * kr, const.kwb)

    # tilting transfer function
    dtheta = theta_eq[1] - theta_eq[0]
    Mwb = np.gradient(wb0, dtheta) / wb0

    # distribution function
    # in radians azimuth of breaking surface area: -pi/2,pi/2
    # phi1 = np.linspace(-np.pi / 2, np.pi / 2, nphi)
    phi1 = np.linspace(-np.pi, np.pi, nphi)
    nk = 1024
    K = np.linspace(10 * spec_peak(u_10, fetch), knb, nk)
    # K = np.linspace(spec_peak(u_10, fetch), knb, nk)

    if spec_name == 'elfouhaily':
        # Directional spectrum model name
        spreadf = spread.models[spec_name]
        Bkdir = specf(K.reshape(nk, 1), u_10, fetch) * spreadf(
            K.reshape(nk, 1), phi1, u_10, fetch) * K.reshape(nk, 1)**3
    else:
        Bkdir = specf(K.reshape(nk, 1), u_10, fetch, phi1)

    n, alpha = param(K, u_10, fetch)
    lamda = (Bkdir / alpha.reshape(nk, 1))**(n.reshape(nk, 1) + 1) / (
        2 * K.reshape(nk, 1))  # distribution of breaking front lengths
    lamda_k = np.trapz(lamda, phi1, axis=1)
    lamda = np.trapz(lamda, K, axis=0)
    lamda_k = np.trapz(lamda_k, K)
    q = const.cq * lamda_k
    if polarization == 'VH':
        WB = CP_breaking(theta_eq)[:, 0]
    else:
        Awb = np.trapz(np.cos(phi1 - eq_azi.reshape(nphi, 1)) * lamda,
                       phi1,
                       axis=1) / lamda_k
        WB = wb0 * (1 + Mwb * const.theta_wb * Awb)
    return WB, q
Exemplo n.º 3
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def eq_wb_mo(kr, K, theta_eq, eq_azi, u_10, fetch, div):
    """
    :param kp:
    :param kr:
    :param theta:
    :param azi:
    :param u_10:
    :param fetch:
    :return:
    """

    # NRCS of plumes
    wb0 = np.exp(-np.tan(theta_eq)**2 / const.Swb) / (
        np.cos(theta_eq)**4 * const.Swb
    ) + const.yitawb / const.Swb  # Kudryavstev 2003a equation (60)
    knb = min(const.br * kr, const.kwb)

    # tilting transfer function
    dtheta = theta_eq[1] - theta_eq[0]
    Mwb = np.gradient(wb0, dtheta) / wb0

    # distribution function
    phi1 = np.linspace(-np.pi, np.pi, 37)
    nk = 1024

    q = np.zeros([div.shape[0], div.shape[1]])
    WB = np.zeros([div.shape[0], div.shape[1]])

    for ii in np.arange(div.shape[0]):
        for jj in np.arange(div.shape[1]):
            KK = np.linspace(10 * spec_peak(u_10[ii, jj], fetch), knb, nk)
            T = Trans_func(KK, K[ii, jj], u_10[ii, jj], fetch, phi1, div[ii,
                                                                         jj])
            Bkdir = kudryavtsev05(KK.reshape(nk, 1), u_10[ii, jj], fetch,
                                  phi1) * (1 + abs(T.reshape(nk, 1)))
            n, alpha = param(KK, u_10[ii, jj], fetch)
            lamda = (Bkdir / alpha.reshape(nk, 1))**(n.reshape(nk, 1) + 1) / (
                2 * KK.reshape(nk, 1)
            )  # distribution of breaking front lengths
            lamda_k = np.trapz(lamda, phi1, axis=1)
            lamda = np.trapz(lamda, KK, axis=0)
            lamda_k = np.trapz(lamda_k, KK)
            q[ii, jj] = const.cq * lamda_k
            Awb = np.trapz(np.cos(phi1 - eq_azi[jj]) * lamda, phi1) / lamda_k
            WB[ii, jj] = wb0[jj] * (1 + Mwb[jj] * const.theta_wb * Awb)
    return WB, q
Exemplo n.º 4
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def mono(u_10, pol):
    """ :param kr: Radar wave number
        :param theta: Normal incidence angle vector
        :param azimuth: radar look angle relative to wind direction vector
        :param pol: Polarization ('vv', 'hh')
        :param u_10: Wind speed (U_10)
        :param fetch: Wind fetch
        :param spec_name: spectrum function
    """
    kr = 2 * np.pi / 5.6e-2
    spec_name = 'kudryavtsev05'
    fetch = 500e+3
    k_min = spec_peak(u_10, fetch)
    nk = 1024
    k = np.linspace(10 * k_min, const.ky, nk)
    nphi = 28
    theta = np.radians(np.linspace(20, 47, nphi))  # 28
    nazi = 37
    azimuth = np.radians(np.linspace(-180, 180, nazi))  # 37
    wb, q = Wave_breaking(kr, theta, azimuth, u_10, fetch, spec_name, pol)
    br = Bragg_scattering(k, kr, theta, azimuth, u_10, fetch, spec_name, pol)
    nrcs = br * (1 - q) + wb * q
    return nrcs


# u_10 = np.linspace(3, 15, 13)
# pol=['VV','HH', 'VH']
# nphi = 28
# theta = np.radians(np.linspace(20, 47, nphi))  # 28
# nazi = 37
# azimuth = np.radians(np.linspace(-180, 180, nazi))  # 37
# nrcsmn = np.zeros([nazi, nphi, u_10.shape[0], len(pol)])
# for mm in np.arange(len(pol)):
#     for nn in np.arange(u_10.shape[0]):
#         nrcsmn[:, :, nn, mm] = mono(u_10[nn], pol[mm])
#
# MN = xr.DataArray(nrcsmn, coords=[azimuth, theta, u_10, pol], dims=['azi','theta','u_10','pol'])
# path = 'd:/TU Delft/Msc Thesis/LUT/mono.nc'
# MN.to_netcdf(path)
# obj = xr.open_dataarray(path)
Exemplo n.º 5
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def bi(kr, theta_i, theta_s, theta_eq, bist_ang_az, fetch, spec_name, u_10,
       azi, inc_polar, re_polar, sat):
    """ :param kr: Radar wave number
        :param theta: Normal incidence angle vector
        :param azimuth: radar look angle relative to wind direction vector
        :param u_10: Wind speed (U_10)
    """
    k_min = spec_peak(u_10, fetch)
    nk = 1024
    k = np.linspace(10 * k_min, const.ky, nk)

    # azimuth angle with respect to the wind direction
    if sat == 'A':
        azimuth = azi - bist_ang_az / 2
    else:
        azimuth = azi + bist_ang_az / 2

    pol = 'VV'
    if inc_polar == 'V':
        pol = 'VV'
    else:
        pol = 'HH'

    if re_polar == 'Bragg':
        wb, q = Wb_bi(kr, theta_i, theta_s, theta_eq, bist_ang_az, azimuth,
                      u_10, fetch, spec_name, pol, inc_polar, re_polar, sat)
        br = Br_bi(k, kr, theta_i, theta_s, theta_eq, bist_ang_az, azimuth,
                   u_10, fetch, spec_name, pol, inc_polar, sat)
        return br * (1 - q) + wb * q
    else:
        wb, q = Wb_bi(kr, theta_i, theta_s, theta_eq, bist_ang_az, azimuth,
                      u_10, fetch, spec_name, pol, inc_polar, re_polar, sat)
        wb_vh, q_vh = Wb_bi(kr, theta_i, theta_s, theta_eq, bist_ang_az,
                            azimuth, u_10, fetch, spec_name, 'VH', inc_polar,
                            re_polar, sat)
        br = Br_bi(k, kr, theta_i, theta_s, theta_eq, bist_ang_az, azimuth,
                   u_10, fetch, spec_name, 'VH', inc_polar, sat)
        return br * (1 - q_vh) + wb * q + wb_vh * q_vh
Exemplo n.º 6
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def Wave_breaking_new(K, kr, theta, azimuth, u_10, fetch, spec_name, tsc):
    """
    :param kp:
    :param kr:
    :param theta:
    :param azi:
    :param u_10:
    :param fetch:
    :return:
    """

    nphi = theta.shape[0]
    divergence = np.gradient(tsc[:, :, 0], 1e3, axis=1) + np.gradient(
        tsc[:, :, 1], 1e3, axis=0)

    # Spectral model
    # Omni directional spectrum model name
    specf = spec.models[spec_name]

    # NRCS of plumes
    wb0 = np.exp(-np.tan(theta)**2 / const.Swb) / (
        np.cos(theta)**4 * const.Swb
    ) + const.yitawb / const.Swb  # Kudryavstev 2003a equation (60)
    knb = min(const.br * kr, const.kwb)

    # tilting transfer function
    dtheta = theta[1] - theta[0]
    Mwb = np.gradient(wb0, dtheta) / wb0

    # distribution function
    phi1 = (np.arange(nphi) * np.pi / nphi).reshape(
        1, nphi
    ) - np.pi / 2  # in radians azimuth of breaking surface area: -pi/2,pi/2
    nk = 1024
    nazi = azimuth.shape[0]
    q = np.zeros([u_10.shape[0], u_10.shape[1]])
    WB = np.zeros([u_10.shape[0], u_10.shape[1], nazi, nphi])

    for ii in np.arange(u_10.shape[0]):
        for jj in np.arange(u_10.shape[1]):
            KK = np.linspace(10 * spec_peak(u_10[ii, jj], fetch), knb, nk)
            T = Trans_single(KK.reshape(nk, 1), K[ii, jj], u_10[ii, jj], fetch,
                             azimuth, spec_name, divergence[ii, jj])
            if spec_name == 'elfouhaily':
                spreadf = spread.models[spec_name]
                Bkdir = specf(KK.reshape(nk, 1), u_10[ii, jj],
                              fetch) * (1 + np.abs(T)) * spreadf(
                                  KK.reshape(nk, 1), phi1, u_10[ii, jj],
                                  fetch) * KK.reshape(nk, 1)**3
            else:
                Bkdir = specf(KK.reshape(nk, 1), u_10[ii, jj], fetch,
                              phi1) * (1 + np.abs(T))
            n, alpha = param(KK, u_10[ii, jj])
            lamda = (Bkdir / alpha.reshape(nk, 1))**(n.reshape(nk, 1) + 1) / (
                2 * KK.reshape(nk, 1)
            )  # distribution of breaking front lengths
            lamda_k = np.trapz(lamda, phi1, axis=1)
            lamda = np.trapz(lamda, KK, axis=0)
            lamda_k = np.trapz(lamda_k, KK)
            q[ii, jj] = const.cq * lamda_k
            Awb = np.trapz(np.cos(phi1 - azimuth.reshape(nazi, 1)) * lamda,
                           phi1,
                           axis=1) / lamda_k
            Awb = Awb.reshape(nazi, 1)
            WB[ii, jj, :, :] = wb0.reshape(
                1, nphi) * (1 + Mwb.reshape(1, nphi) * const.theta_wb * Awb)
    return WB, q
Exemplo n.º 7
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def MSS(kbr, u_10, fetch):
    # Kudryavtsev, 2019a
    alpha = u_10 * np.sqrt(spec_peak(u_10, fetch) / const.g)
    kd = kbr / 4
    return 4.5 * 10**(-3) * np.log(alpha**(-2) * kd * u_10**2 / const.g) / 2