Calculation of solar irradiance i.e.
shortwave radiation flux and the atmosphere's heat radiation i.e. longwave radiation flux is important.
Not exact matches
where is the vertically integrated energy
flux in the atmosphere, is the net radiative energy input to an atmospheric column (the difference between absorbed
shortwave radiation and emitted longwave
radiation), and is the oceanic energy uptake at the surface.
The other
fluxes (
shortwave and longwave
radiation at both surface and top of atmosphere) show more «normal» cycles (though somewhat higher values).
where SW denotes net downward
shortwave radiation, LW net upward longwave
radiation, LH latent heat
flux, and SH sensible heat
flux I can find these products at http://www.esrl.noaa.gov/psd/data/gridded/data.ncep.reanalysis.surfaceflux.html Regarding the latent and sensible
fluxes I don't have a problem (since there are only two in the NCEP list), but regarding the others I have several.
[1] Total absorbed
radiation (TAR), the sum of SNR [
shortwave net
radiation] and LDR [longwave downward
radiation], represents the total radiative energy available to maintain the Earth's surface temperature and to sustain the turbulent (sensible and latent) heat
fluxes in the atmosphere.
In other words, a bigger share of the 240 W / m 2 of the vertical energy transport will be transported by convective / advective means with a stronger GHE, and a smaller share by radiative means because the sum of convective vertical energy transport plus the diminished radiative
flux must add up to about 240 W / m 2 in order to balance the incoming
shortwave radiation.
We use the 9 climate variables of surface air temperature (SAT), sea level pressure (SLP), precipitation (rain), the top of atmosphere (TOA)
shortwave (SW) and longwave (LW) full - sky
radiation, clear - sky
radiation (CLR, radiative
flux where clouds do not exists), and cloud radiative forcing (CRF, radiative effect by clouds diagnosed from the difference between full - sky and clear - sky
radiation, Cess et al. 1990).