Global increase in tropical cyclone rain rate

Abstract Theoretical models of the potential intensity of tropical cyclones (TCs) suggest that TC rainfall rates should increase in a warmer environment but limited observational evidence has been studied to test these hypotheses on a global scale. The present study explores the general trends of TC...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Guzman, Oscar, Jiang, Haiyan
Other Authors: Fulbright-Colciencias grant as part of the cultural exchange program between the United States of America and the Republic of Colombia., National Science Foundation, National Aeronautics and Space Administration, United States Department of Commerce | National Oceanic and Atmospheric Administration
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2021
Subjects:
Online Access:http://dx.doi.org/10.1038/s41467-021-25685-2
https://www.nature.com/articles/s41467-021-25685-2.pdf
https://www.nature.com/articles/s41467-021-25685-2
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Summary:Abstract Theoretical models of the potential intensity of tropical cyclones (TCs) suggest that TC rainfall rates should increase in a warmer environment but limited observational evidence has been studied to test these hypotheses on a global scale. The present study explores the general trends of TC rainfall rates based on a 19-year (1998–2016) time series of continuous observational data collected by the Tropical Rainfall Measuring Mission and the Global Precipitation Measurement mission. Overall, observations exhibit an increasing trend in the average TC rainfall rate of about 1.3% per year, a fact that is contributed mainly by the combined effect of the reduction in the inner-core rainfall rate with the increase in rainfall rate on the rainband region. We found that the increasing trend is more pronounced in the Northwestern Pacific and North Atlantic than in other global basins, and it is relatively uniform for all TC intensities. Further analysis shows that these trends are associated with increases in sea surface temperature and total precipitable water in the TC environment.