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private |
colamt | column amounts of absorbing gases the index are for h2o, co2, o3, n2o, ch4, and o2, respectively \((mol/cm^2)\) |
colmol | total column amount (dry air+water vapor) |
fac00,fac01,fac10,fac11 | for each layer, these are factors that are needed to compute the interpolation factors that multiply the appropriate reference k-values. a value of 0/1 for i,j indicates that the corresponding factor multiplies reference k-value for the lower/higher of the two appropriate temperatures, and altitudes, respectively. |
jp | the index of the lower (in altitude) of the two appropriate ref pressure levels needed for interpolation. |
jt,jt1 | the indices of the lower of the two approp ref temperatures needed for interpolation (for pressure levels jp and jp+1, respectively) |
laytrop | tropopause layer index |
forfac | scale factor needed to foreign-continuum. |
forfrac | factor needed for temperature interpolation |
indfor | index of the lower of the two appropriate reference temperatures needed for foreign-continuum interpolation |
selffac | scale factor needed to h2o self-continuum. |
selffrac | factor needed for temperature interpolation of reference h2o self-continuum data |
indself | index of the lower of the two appropriate reference temperatures needed for the self-continuum interpolation |
nlay | number of vertical layers |
sfluxzen | spectral distribution of incoming solar flux |
taug | spectral optical depth for gases |
taur | opt depth for rayleigh scattering |
Definition at line 4095 of file radsw_main.F90.
References taumol16(), taumol17(), taumol18(), taumol19(), taumol20(), taumol21(), taumol22(), taumol23(), taumol24(), taumol25(), taumol26(), taumol27(), taumol28(), and taumol29().
Referenced by rrtmg_sw_run().