Here is the SMAC atmospheric correction routine in Python language. More about SMAC.

Voici la routine de correction atmosphérique SMAC en python En savoir plus sur SMAC

 

#! /usr/bin/env python# -*- coding: iso-8859-1 -*-#=============================================================================================# library for atmospheric correction using SMAC method (Rahman and Dedieu, 1994)# Contains :#      smac_inv : inverse smac model for atmospheric correction#                          TOA==>Surface#      smac dir : direct smac model#                          Surface==>TOA#      coefs : reads smac coefficients#      PdeZ : #      PdeZ : Atmospheric pressure (in hpa) as a function of altitude (in meters)# Written by O.Hagolle CNES, from the original SMAC C routine#=============================================================================================from math import *import numpy as np#=============================================================================================def PdeZ(Z) :    """    PdeZ : Atmospheric pressure (in hpa) as a function of altitude (in meters)    """    p = 1013.25 * pow( 1 - 0.0065 * Z / 288.15 , 5.31 )    return(p)#=============================================================================================class coeff:  def __init__(self,smac_filename):    with file(smac_filename) as f:      lines=f.readlines()    #H20    temp=lines[0].strip().split()    self.ah2o=float(temp[0])    self.nh2o=float(temp[1])    #O3    temp=lines[1].strip().split()    self.ao3=float(temp[0])    self.no3=float(temp[1])    #O2    temp=lines[2].strip().split()    self.ao2=float(temp[0])    self.no2=float(temp[1])    self.po2=float(temp[2])    #CO2    temp=lines[3].strip().split()    self.aco2=float(temp[0])    self.nco2=float(temp[1])    self.pco2=float(temp[2])    #NH4    temp=lines[4].strip().split()    self.ach4=float(temp[0])    self.nch4=float(temp[1])    self.pch4=float(temp[2])    #NO2    temp=lines[5].strip().split()    self.ano2=float(temp[0])    self.nno2=float(temp[1])    self.pno2=float(temp[2])    #NO2    temp=lines[6].strip().split()    self.aco=float(temp[0])    self.nco=float(temp[1])    self.pco=float(temp[2])    #rayleigh and aerosol scattering    temp=lines[7].strip().split()    self.a0s=float(temp[0])    self.a1s=float(temp[1])    self.a2s=float(temp[2])    self.a3s=float(temp[3])    temp=lines[8].strip().split()    self.a0T=float(temp[0])    self.a1T=float(temp[1])    self.a2T=float(temp[2])    self.a3T=float(temp[3])    temp=lines[9].strip().split()    self.taur=float(temp[0])    self.sr=float(temp[0])    temp=lines[10].strip().split()    self.a0taup  = float(temp[0])    self.a1taup  = float(temp[1])    temp=lines[11].strip().split()    self.wo      = float(temp[0])    self.gc      = float(temp[1])    temp=lines[12].strip().split()    self.a0P     = float(temp[0])    self.a1P     = float(temp[1])    self.a2P     = float(temp[2])    temp=lines[13].strip().split()    self.a3P     = float(temp[0])    self.a4P     = float(temp[1])    temp=lines[14].strip().split()    self.Rest1   = float(temp[0])    self.Rest2   = float(temp[1])    temp=lines[15].strip().split()    self.Rest3   = float(temp[0])    self.Rest4   = float(temp[1])    temp=lines[16].strip().split()    self.Resr1   = float(temp[0])    self.Resr2   = float(temp[1])    self.Resr3   = float(temp[2])    temp=lines[17].strip().split()    self.Resa1   = float(temp[0])    self.Resa2   = float(temp[1])    temp=lines[18].strip().split()    self.Resa3   = float(temp[0])    self.Resa4   = float(temp[1])#======================================================================def smac_inv( r_toa, tetas, phis, tetav, phiv,pressure,taup550, uo3, uh2o, coef) :    """    r_surf=smac_inv( r_toa, tetas, phis, tetav, phiv,pressure,taup550, uo3, uh2o, coef)    Corrections atmosphériques    """    ah2o    	= coef.ah2o    nh2o    	= coef.nh2o    ao3     	= coef.ao3    no3     	= coef.no3    ao2     	= coef.ao2    no2     	= coef.no2    po2     	= coef.po2    aco2 	= coef.aco2    nco2 	= coef.nco2    pco2 	= coef.pco2    ach4 	= coef.ach4    nch4 	= coef.nch4    pch4 	= coef.pch4    ano2 	= coef.ano2    nno2 	= coef.nno2    pno2 	= coef.pno2    aco  	= coef.aco    nco  	= coef.nco    pco  	= coef.pco    a0s  	= coef.a0s    a1s  	= coef.a1s    a2s  	= coef.a2s    a3s  	= coef.a3s    a0T  	= coef.a0T    a1T  	= coef.a1T    a2T  	= coef.a2T    a3T     	= coef.a3T    taur    	= coef.taur    sr      	= coef.sr    a0taup  	= coef.a0taup    a1taup  	= coef.a1taup    wo      	= coef.wo    gc     	= coef.gc    a0P     	= coef.a0P    a1P     	= coef.a1P    a2P     	= coef.a2P    a3P     	= coef.a3P    a4P     	= coef.a4P    Rest1   	= coef.Rest1    Rest2   	= coef.Rest2    Rest3   	= coef.Rest3    Rest4   	= coef.Rest4    Resr1   	= coef.Resr1    Resr2   	= coef.Resr2    Resr3   	= coef.Resr3    Resa1   	= coef.Resa1    Resa2   	= coef.Resa2    Resa3   	= coef.Resa3    Resa4   	= coef.Resa4    cdr=pi/180    crd=180/pi    #/*------:  calcul de la reflectance de surface  smac               :--------*/    us = cos (tetas * cdr)    uv = cos (tetav * cdr)    Peq= pressure/1013.25     #/*------:  1) air mass */    m =  1/us + 1/uv    #/*------:  2) aerosol optical depth in the spectral band, taup     :--------*/    taup = (a0taup) + (a1taup) * taup550     #/*------:  3) gaseous transmissions (downward and upward paths)    :--------*/    to3 = 1.    th2o= 1.    to2 = 1.    tco2= 1.    tch4= 1.     uo2 =  (Peq ** (po2))    uco2=  (Peq ** (pco2))    uch4=  (Peq ** (pch4))    uno2=  (Peq ** (pno2))    uco =  (Peq ** (pco))    #/*------:  4) if uh2o <= 0 and uo3 <=0 no gaseous absorption is computed  :--------*/    to3   = exp ( (ao3)  * ( (uo3 *m)  ** (no3)  ) )    th2o  = exp ( (ah2o) * ( (uh2o*m)  ** (nh2o) ) )    to2   = exp ( (ao2)  * ( (uo2 *m)  ** (no2)  ) )    tco2  = exp ( (aco2) * ( (uco2*m)  ** (nco2) ) )    tch4  = exp ( (ach4) * ( (uch4*m)  ** (nch4) ) )    tno2  = exp ( (ano2) * ( (uno2*m)  ** (nno2) ) )    tco   = exp ( (aco)  * ( (uco *m)  ** (nco) ) )    tg      = th2o * to3 * to2 * tco2 * tch4 * tco * tno2    #/*------:  5) Total scattering transmission                      :--------*/    ttetas = (a0T) + (a1T)*taup550/us + ((a2T)*Peq + (a3T))/(1.+us)  #/* downward */    ttetav = (a0T) + (a1T)*taup550/uv + ((a2T)*Peq + (a3T))/(1.+uv)  #/* upward   */    #/*------:  6) spherical albedo of the atmosphere                 :--------*/    s = (a0s) * Peq +  (a3s) + (a1s)*taup550 + (a2s) * (taup550 ** 2)     #/*------:  7) scattering angle cosine                            :--------*/    cksi = - ( (us*uv) + (sqrt(1. - us*us) * sqrt (1. - uv*uv)*cos((phis-phiv) * cdr) ) )    if (cksi < -1 ) :	   cksi=-1.0     #/*------:  8) scattering angle in degree 			 :--------*/    ksiD = crd*acos(cksi)     #/*------:  9) rayleigh atmospheric reflectance 			 :--------*/    ray_phase = 0.7190443 * (1. + (cksi*cksi))  + 0.0412742    ray_ref   = ( taur*ray_phase ) / (4*us*uv)    ray_ref   = ray_ref*pressure / 1013.25    taurz=(taur)*Peq    #/*------:  10) Residu Rayleigh 					 :--------*/    Res_ray= Resr1 + Resr2 * taur*ray_phase / (us*uv) + Resr3 * ( (taur*ray_phase/(us*uv)) ** 2)     #/*------:  11) aerosol atmospheric reflectance			 :--------*/    aer_phase = a0P + a1P*ksiD + a2P*ksiD*ksiD +a3P*(ksiD ** 3) + a4P * (ksiD ** 4)    ak2 = (1. - wo)*(3. - wo*3*gc)    ak  = sqrt(ak2)    e   = -3*us*us*wo /  (4*(1. - ak2*us*us) )    f   = -(1. - wo)*3*gc*us*us*wo / (4*(1. - ak2*us*us) )    dp  = e / (3*us) + us*f    d   = e + f    b   = 2*ak / (3. - wo*3*gc)    delta = np.exp( ak*taup )*(1. + b)*(1. + b) - np.exp(-ak*taup)*(1. - b)*(1. - b)    ww  = wo/4.    ss  = us / (1. - ak2*us*us)    q1  = 2. + 3*us + (1. - wo)*3*gc*us*(1. + 2*us)    q2  = 2. - 3*us - (1. - wo)*3*gc*us*(1. - 2*us)    q3  = q2*np.exp( -taup/us )    c1  =  ((ww*ss) / delta) * ( q1*np.exp(ak*taup)*(1. + b) + q3*(1. - b) )    c2  = -((ww*ss) / delta) * (q1*np.exp(-ak*taup)*(1. - b) + q3*(1. + b) )    cp1 =  c1*ak / ( 3. - wo*3*gc )    cp2 = -c2*ak / ( 3. - wo*3*gc )    z   = d - wo*3*gc*uv*dp + wo*aer_phase/4.    x   = c1 - wo*3*gc*uv*cp1    y   = c2 - wo*3*gc*uv*cp2    aa1 = uv / (1. + ak*uv)    aa2 = uv / (1. - ak*uv)    aa3 = us*uv / (us + uv)     aer_ref = x*aa1* (1. - np.exp( -taup/aa1 ) )    aer_ref = aer_ref + y*aa2*( 1. - np.exp( -taup / aa2 )  )    aer_ref = aer_ref + z*aa3*( 1. - np.exp( -taup / aa3 )  )    aer_ref = aer_ref / ( us*uv )    #/*------:  12) Residu Aerosol  					:--------*/    Res_aer= ( Resa1 + Resa2 * ( taup * m *cksi ) + Resa3 * ( (taup*m*cksi ) ** 2) )+ Resa4 * ( (taup*m*cksi) ** 3)    #/*------:  13)  Terme de couplage molecule / aerosol		:--------*/    tautot=taup+taurz    Res_6s= ( Rest1 + Rest2 * ( tautot * m *cksi )   + Rest3 * ( (tautot*m*cksi) ** 2) ) + Rest4 * ( (tautot*m*cksi) ** 3)    #/*------:  14) total atmospheric reflectance  			:--------*/    atm_ref = ray_ref - Res_ray + aer_ref - Res_aer + Res_6s    #/*------:  15) Surface reflectance  				:--------*/    r_surf = r_toa - (atm_ref * tg)    r_surf = r_surf / ( (tg * ttetas * ttetav) + (r_surf * s) )     return r_surf#=======================================================================================================def smac_dir ( r_surf, tetas, phis, tetav, phiv,pressure,taup550, uo3, uh2o, coef):    """    r_toa=smac_dir ( r_surf, tetas, phis, tetav, phiv,pressure,taup550, uo3, uh2o, coef)    Application des effets atmosphériques    """    ah2o    	= coef.ah2o    nh2o    	= coef.nh2o    ao3     	= coef.ao3    no3     	= coef.no3    ao2     	= coef.ao2    no2     	= coef.no2    po2     	= coef.po2    aco2 	= coef.aco2    nco2 	= coef.nco2    pco2 	= coef.pco2    ach4 	= coef.ach4    nch4 	= coef.nch4    pch4 	= coef.pch4    ano2 	= coef.ano2    nno2 	= coef.nno2    pno2 	= coef.pno2    aco  	= coef.aco    nco  	= coef.nco    pco  	= coef.pco    a0s  	= coef.a0s    a1s  	= coef.a1s    a2s  	= coef.a2s    a3s  	= coef.a3s    a0T  	= coef.a0T    a1T  	= coef.a1T    a2T  	= coef.a2T    a3T     	= coef.a3T    taur    	= coef.taur    sr      	= coef.sr    a0taup  	= coef.a0taup    a1taup  	= coef.a1taup    wo      	= coef.wo    gc     	= coef.gc    a0P     	= coef.a0P    a1P     	= coef.a1P    a2P     	= coef.a2P    a3P     	= coef.a3P    a4P     	= coef.a4P    Rest1   	= coef.Rest1    Rest2   	= coef.Rest2    Rest3   	= coef.Rest3    Rest4   	= coef.Rest4    Resr1   	= coef.Resr1    Resr2   	= coef.Resr2    Resr3   	= coef.Resr3    Resa1   	= coef.Resa1    Resa2   	= coef.Resa2    Resa3   	= coef.Resa3    Resa4   	= coef.Resa4    cdr=pi/180    crd=180/pi    #/*------:  calcul de la reflectance de surface  smac               :--------*/    us = cos (tetas * cdr)    uv = cos (tetav * cdr)    Peq= pressure/1013.25     #/*------:  1) air mass */    m =  1/us + 1/uv    #/*------:  2) aerosol optical depth in the spectral band, taup     :--------*/    taup = (a0taup) + (a1taup) * taup550     #/*------:  3) gaseous transmissions (downward and upward paths)    :--------*/    to3 = 1.    th2o= 1.    to2 = 1.    tco2= 1.    tch4= 1.     uo2 =  (Peq ** (po2))    uco2=  (Peq ** (pco2))    uch4=  (Peq ** (pch4))    uno2=  (Peq ** (pno2))    uco =  (Peq ** (pco))    #/*------:  4) if uh2o <= 0 and uo3<= 0 no gaseous absorption is computed  :--------*/    to3   = exp ( (ao3)  * ( (uo3 *m)  ** (no3)  ) )    th2o  = exp ( (ah2o) * ( (uh2o*m)  ** (nh2o) ) )    to2   = exp ( (ao2)  * ( (uo2 *m)  ** (no2)  ) )    tco2  = exp ( (aco2) * ( (uco2*m)  ** (nco2) ) )    tch4  = exp ( (ach4) * ( (uch4*m)  ** (nch4) ) )    tno2  = exp ( (ano2) * ( (uno2*m)  ** (nno2) ) )    tco   = exp ( (aco)  * ( (uco *m)  ** (nco) ) )    tg      = th2o * to3 * to2 * tco2 * tch4 * tco * tno2    #/*------:  5) Total scattering transmission                      :--------*/    ttetas = (a0T) + (a1T)*taup550/us + ((a2T)*Peq + (a3T))/(1.+us)  #/* downward */    ttetav = (a0T) + (a1T)*taup550/uv + ((a2T)*Peq + (a3T))/(1.+uv)  #/* upward   */    #/*------:  6) spherical albedo of the atmosphere                 :--------*/    s = (a0s) * Peq +  (a3s) + (a1s)*taup550 + (a2s) * (taup550 ** 2)     #/*------:  7) scattering angle cosine                            :--------*/    cksi = - ( (us*uv) + (sqrt(1. - us*us) * sqrt (1. - uv*uv)*cos((phis-phiv-360) * cdr) ) )    if (cksi < -1 ) :       cksi=-1.0     #/*------:  8) scattering angle in degree            :--------*/    ksiD = crd*acos(cksi)     #/*------:  9) rayleigh atmospheric reflectance              :--------*/    ray_phase = 0.7190443 * (1. + (cksi*cksi))  + 0.0412742    ray_ref   = ( taur*ray_phase ) / (4*us*uv)    ray_ref   = ray_ref*pressure / 1013.25    taurz=(taur)*Peq    #/*------:  10) Residu Rayleigh                      :--------*/    Res_ray= Resr1 + Resr2 * taur*ray_phase / (us*uv) + Resr3 * ( (taur*ray_phase/(us*uv)) ** 2)     #/*------:  11) aerosol atmospheric reflectance          :--------*/    aer_phase = a0P + a1P*ksiD + a2P*ksiD*ksiD +a3P*(ksiD ** 3) + a4P * (ksiD ** 4)    ak2 = (1. - wo)*(3. - wo*3*gc)    ak  = sqrt(ak2)    e   = -3*us*us*wo /  (4*(1. - ak2*us*us) )    f   = -(1. - wo)*3*gc*us*us*wo / (4*(1. - ak2*us*us) )    dp  = e / (3*us) + us*f    d   = e + f    b   = 2*ak / (3. - wo*3*gc)    delta = np.exp( ak*taup )*(1. + b)*(1. + b) - np.exp(-ak*taup)*(1. - b)*(1. - b)    ww  = wo/4.    ss  = us / (1. - ak2*us*us)    q1  = 2. + 3*us + (1. - wo)*3*gc*us*(1. + 2*us)    q2  = 2. - 3*us - (1. - wo)*3*gc*us*(1. - 2*us)    q3  = q2*np.exp( -taup/us )    c1  =  ((ww*ss) / delta) * ( q1*np.exp(ak*taup)*(1. + b) + q3*(1. - b) )    c2  = -((ww*ss) / delta) * (q1*np.exp(-ak*taup)*(1. - b) + q3*(1. + b) )    cp1 =  c1*ak / ( 3. - wo*3*gc )    cp2 = -c2*ak / ( 3. - wo*3*gc )    z   = d - wo*3*gc*uv*dp + wo*aer_phase/4.    x   = c1 - wo*3*gc*uv*cp1    y   = c2 - wo*3*gc*uv*cp2    aa1 = uv / (1. + ak*uv)    aa2 = uv / (1. - ak*uv)    aa3 = us*uv / (us + uv)     aer_ref = x*aa1* (1. - np.exp( -taup/aa1 ) )    aer_ref = aer_ref + y*aa2*( 1. - np.exp( -taup / aa2 )  )    aer_ref = aer_ref + z*aa3*( 1. - np.exp( -taup / aa3 )  )    aer_ref = aer_ref / ( us*uv )    #/*------:  12) Residu Aerosol                      :--------*/    Res_aer= ( Resa1 + Resa2 * ( taup * m *cksi ) + Resa3 * ( (taup*m*cksi ) ** 2) )+ Resa4 * ( (taup*m*cksi) ** 3)    #/*------:  13)  Terme de couplage molecule / aerosol       :--------*/    tautot=taup+taurz    Res_6s= ( Rest1 + Rest2 * ( tautot * m *cksi )   + Rest3 * ( (tautot*m*cksi) ** 2) ) + Rest4 * ( (tautot*m*cksi) ** 3)    #/*------:  14) total atmospheric reflectance           :--------*/    atm_ref = ray_ref - Res_ray + aer_ref - Res_aer + Res_6s    #/*------:  15) TOA reflectance                 :--------*/    r_toa = r_surf*tg*ttetas*ttetav/(1-r_surf*s) + (atm_ref * tg)     return r_toa#=============================================================================if __name__=="__main__" :    #example    theta_s = 45    theta_v = 5    phi_s =  200    phi_v = -160    r_toa=0.2    ######################################lecture des coefs_smac    nom_smac ='COEFS/coef_FORMOSAT2_B1_CONT.dat'    coefs=coeff(nom_smac)    bd=1    r_surf = smac_inv(r_toa , theta_s, phi_s, theta_v, phi_v,1013,0.1,0.3,0.3, coefs)    r_toa2 = smac_dir(r_surf, theta_s, phi_s, theta_v, phi_v,1013,0.1,0.3,0.3, coefs)           print r_toa, r_surf,r_toa2

5 thoughts on “SMAC Python

  1. Bonjour, voilà je voudrais utilisée la routine SMAC pour corriger atmosphériquemment des images landsat 7 mais je n'arrive à intégrer la routine smac sous python . est-ce que quelqu'un pourrait m'aider je débute en programmation?merci d'avance Stéphanie

  2. Hello,thank you very much for the code! I found a difference in the Python code compared with the C-code of SMAC available at the CESBIO website:in Step 10 - "Residual Rayleigh", in the Python code the factor "taur" is used as provided in the coefficient files, while in the C-code this factor is weighted in Step 9 - "Rayleigh atmospheric reflectance" with Peq (taurz = taur * Peq).Could you please clarify if this is a typo in the Python code, or if this change was made consciously compared to the C-code?In the latter case, why?Thank you very much in advance,Gabi

    1. Dear Gabriele, \nthanks for pointing this inconsistency !\nI do not have the answer yet, we have dug in all the multiple versions we have of the code, and some of them use taurz, others taur, we thus need to dig a little more to find out which one is the right one.\nAs it is a regression, the answer should be in the software which computes the coefficients, but we have several versions of it...\n\nI tested the effect of the error, for a blue band and a pressure of 900 hpa. Difference is only 0.35%, but still, we should correct it.\nI'll come back to you soon.\nOlivier

      1. Dear Olivier,did you already had time to clarify the inconsistencies in the C- and Python-codes of SMAC regarding the parameters taur and taurz, respectively?Further, do you have any experiences with combining the atmospheric correction with a topographic correction? Thanks!Gabi

        1. Dear Gabriele,\nsorry for replying so late, last weeks have been hectic. \nWe did not have time to look at your question yet. Please remind us from time to time !\nOlivier

Laisser un commentaire

Votre adresse de messagerie ne sera pas publiée. Les champs obligatoires sont indiqués avec *