For instance, two that were based purely on
global energy balance estimates, with climate sensitivity assumed to be 3 K; three did not themselves actually estimate global aerosol forcing; and one turns out to have used a model with a serious code error, correction of which substantially reduces its estimate of aerosol cooling.
Not exact matches
«The
global mean latent heat flux is required to exceed 80 W m — 2 to close the surface energy balance in Figure 2.11, and comes close to the 85 W m — 2 considered as upper limit by Trenberth and Fasullo (2012b) in view of current uncertainties in precipitation retrieval in the Global Precipitation Climatology Project (GPCP, Adler et al., 2012)(the latent heat flux corresponds to the energy equivalent of evaporation, which globally equals precipitation; thus its magnitude may be constrained by global precipitation estim
global mean latent heat flux is required to exceed 80 W m — 2 to close the surface
energy balance in Figure 2.11, and comes close to the 85 W m — 2 considered as upper limit by Trenberth and Fasullo (2012b) in view of current uncertainties in precipitation retrieval in the
Global Precipitation Climatology Project (GPCP, Adler et al., 2012)(the latent heat flux corresponds to the energy equivalent of evaporation, which globally equals precipitation; thus its magnitude may be constrained by global precipitation estim
Global Precipitation Climatology Project (GPCP, Adler et al., 2012)(the latent heat flux corresponds to the
energy equivalent of evaporation, which globally equals precipitation; thus its magnitude may be constrained by
global precipitation estim
global precipitation
estimates).
The Stephens et al paper is a very incremental change from previous
estimates of the
global energy balances — chiefly an improvement in latent heat fluxes because of undercounts in the satellite precipitation products and an increase in downward longwave radiation.
JimD, BTW, I was curious how much impact the isolation of the Antarctic had on
global temperatures based on the normal radiant
balance, so i did some quick
estimates using the Meridional
energy flux based on the satellite based SST OI v2 data.
So if you do want to help on the issue you raised, then provide an
estimate of the importance of photosynthesis on the
global energy balance.
Since 70 % of the Earth is ocean, Trenberth's
global energy balance diagram gives us a starting
estimate for NLR for the ocean.