They discussed the effect of variables being non-iid on the extreme value analysis, and after taking that into account, propose that changes in extreme precipitation are likely to be larger than the corresponding changes in annual mean
precipitation under a global warming.
Not exact matches
«Increased Record - Breaking
Precipitation Events
under Global Warming.»
These methods have been significantly improved by fully coupling the hydrologic cycle among land, lake, and atmosphere.94, 95 Without accounting for that cycle of interactions, a study96 concluded that increases in
precipitation would be negated by increases in winter evaporation from less ice cover and by increases in summer evaporation and evapotranspiration from
warmer air temperatures,
under a scenario of continued increases in
global emissions (SRES A2 scenario).
Gutowski, W. J., E. S. Takle, K. A. Kozak, J. C. Patton, R. W. Arritt, and J. H. Christensen, 2007: A possible constraint on regional
precipitation intensity changes
under global warming.
The role of ecosystem - atmosphere interactions in simulated Amazonian
precipitation decrease and forest dieback
under global climate
warming.