If not
the downwelling atmospheric radiation where is all the extra energy necessary to balance coming from?
Not exact matches
Without an atmosphere, inputs that represent the
atmospheric forcing (near surface winds, temperature, humidity, and
downwelling short and longwave
radiation) need to be provided.
It then
downwells a lesser amount of
radiation and this restores the radiative balance throughout the
atmospheric column.
Daily mean NCEP / NCAR reanalysis data are used as
atmospheric forcing, i.e., 10 - m surface winds, 2 - m surface air temperature (SAT), specific humidity, precipitation, evaporation,
downwelling longwave
radiation, sea level pressure, and cloud fraction.
During dimming (1950s — 80s) the decline in surface solar
radiation (SSR) may have outweighed increasing
atmospheric downwelling thermal
radiation (LW) from enhanced greenhouse gases and effectively counteracted global warming, causing only little increase in surface thermal emission (LW).
During dimming (1950s — 80s) the decline in surface solar
radiation (SSR) may have outweighed increasing
atmospheric downwelling thermal
radiation (LW