The model simulated and CERES EBAF observed TOA reflected SW and OLR fluxes on average differ by 1.8 and 0.9Wm 2 , respectively. The averaged SW, LW, and net CRFs from CERES EBAF are 50.1, 27.6, and 22.5Wm 2 , respectively, indicating a net cooling effect of clouds on the TOA ...
The model simulated and CERES EBAF observed TOA reflected SW and OLR fluxes on average differ by 1.8 and −0.9 Wm−2, respectively. The averaged SW, LW, and net CRFs from CERES EBAF are −50.1, 27.6, and −22.5 Wm−2, respectively, indicating a net cooling effect of ...
Overall we find that the SYN and EBAF results provide better comparisons to surface observed fluxes than the other re-analyses products. This is attributed to the fact that the multiple geostationary data sets are calibrated to the CERES Terra and Aqua instruments across the years providing TOA ...
The model simulated and CERES EBAF observed TOA reflected shortwave (SW) and outgoing longwave (LW) radiation fluxes, on average, differ by 1.6 and -0.9 Wm-2, respectively, and is contrary to physical theory. The global averaged SW, LW, and net CRFs form CERES EBAF are -47.2, 26.2, ...