Affiliation:
1. Earth and Environmental Sciences Columbia University New York NY USA
2. Lamont‐Doherty Earth Observatory Columbia University Palisades NY USA
3. Applied Physics and Applied Mathematics Columbia University New York NY USA
4. School of the Environment Washington State University Vancouver WA USA
Abstract
AbstractThe South Asian summer monsoon strongly modulates regional temperature and humidity. While extreme dry heat peaks in the pre‐monsoon season, recent literature suggests that extreme humid heat can continue to build throughout the monsoon season. Here we explore the influence of monsoon onset and subseasonal precipitation variability on the occurrence of extreme wet bulb temperatures (Tw) across South Asia. We find that extreme Tw events often occur on rainy days during the monsoon season. However, the influence of precipitation on Tw varies with the background climatology of surface specific humidity. In climatologically drier areas, positive Tw anomalies tend to occur when precipitation increases due to either early onset or wet spells during the monsoon. In contrast, in climatologically humid areas, positive Tw anomalies occur during periods of suppressed precipitation, including both delayed onset and dry spells during the monsoon.
Funder
National Oceanic and Atmospheric Administration
National Science Foundation
Publisher
American Geophysical Union (AGU)
Cited by
1 articles.
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