The Influence of the 1998 El Niño upon Cloud-Radiative Forcing over the Pacific Warm Pool
Open Access
- 1 May 2001
- journal article
- Published by American Meteorological Society in Journal of Climate
- Vol. 14 (9) , 2129-2137
- https://doi.org/10.1175/1520-0442(2001)014<2129:tioten>2.0.co;2
Abstract
Clouds cool the climate system by reflecting shortwave radiation and warm it by increasing the atmospheric greenhouse. Previous studies have shown that in tropical regions of deep convection there is a near cancellation between cloud-induced shortwave cooling and longwave warming. The present study investigates the possible influence of the 1998 El Niño upon this near cancellation for the tropical western Pacific’s warm pool; this was accomplished by employing satellite radiometric measurements (Earth Radiation Budget Experiment, and Clouds and the Earth’s Radiant Energy System). With the exclusion of the 1998 El Niño, this study also finds near cancellation between the shortwave and longwave cloud forcings and demonstrates that it refers to the average of different cloud types rather than being indicative of a single cloud type. The shortwave cooling slightly dominates the longwave warming, and there is considerable interannual variability in this modest dominance that appears attributable to in... Abstract Clouds cool the climate system by reflecting shortwave radiation and warm it by increasing the atmospheric greenhouse. Previous studies have shown that in tropical regions of deep convection there is a near cancellation between cloud-induced shortwave cooling and longwave warming. The present study investigates the possible influence of the 1998 El Niño upon this near cancellation for the tropical western Pacific’s warm pool; this was accomplished by employing satellite radiometric measurements (Earth Radiation Budget Experiment, and Clouds and the Earth’s Radiant Energy System). With the exclusion of the 1998 El Niño, this study also finds near cancellation between the shortwave and longwave cloud forcings and demonstrates that it refers to the average of different cloud types rather than being indicative of a single cloud type. The shortwave cooling slightly dominates the longwave warming, and there is considerable interannual variability in this modest dominance that appears attributable to in...This publication has 0 references indexed in Scilit: