Mechanisms of change in ENSO-induced tropical Pacific rainfall variability in a warming climate

TitleMechanisms of change in ENSO-induced tropical Pacific rainfall variability in a warming climate
Publication TypeJournal Article
Year of Publication2015
AuthorsHuang P, Xie SP
JournalNature Geoscience
Volume8
Pagination922-U48
Date Published2015/12
Type of ArticleArticle
ISBN Number1752-0894
Accession NumberWOS:000367200200013
Keywordsconvection; el-nino teleconnections; events; frequency; indo-pacific; la-nina; north-america; patterns; precipitation; response; sea-surface temperature
Abstract

El Nino/Southern Oscillation (ENSO) is a mode of natural variability that has considerable impacts on global climate and ecosystems(1-4), through rainfall variability in the tropical Pacific and atmospheric teleconnections(5). In response to global warming, ENSO-driven rainfall variability is projected to intensify over the central-eastern Pacific but weaken over the western Pacific, whereas ENSO-related sea surface temperature variability is projected to decrease(6-14). Here, we explore the mechanisms that lead to changes in ENSO-driven rainfall variability in the tropical Pacific in response to global warming, with the help of a moisture budget decomposition for simulations from eighteen state-of-the-art climate models(15). We identify two opposing mechanisms that approximately offset each other: the increase in mean-state moisture content associated with surface warming strengthens ENSO-related rainfall anomalies(7), whereas the projected reduction in ENSO-related variability of sea surface temperatures suppresses rainfall. Two additional effects-spatially non-uniform changes in background sea surface temperatures and structural changes in sea surface temperature related to ENSO-both enhance central-eastern Pacific rainfall variability while dampening variability in the western Pacific, in nearly equal amounts. Our decomposition method may be generalized to investigate how rainfall variability would change owing to nonlinear interactions between background sea surface temperatures and their variability.

DOI10.1038/ngeo2571
Short TitleNat. Geosci.
Student Publication: 
No