Search from over 60,000 research works

Advanced Search

On the influence of the Bay of Bengal’s sea surface temperature gradients on rainfall of the South Asian monsoon

[thumbnail of Open Access]
Preview
clim-JCLI-D-22-0288.1.pdf - Published Version (3MB) | Preview
Available under license: Creative Commons Attribution
Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Sheehan, P. M. F., Matthews, A. J., Webber, B. G. M., Sanchez-Franks, A., Klingaman, N. P. orcid id iconORCID: https://orcid.org/0000-0002-2927-9303 and Vinayachandran, P. N. (2023) On the influence of the Bay of Bengal’s sea surface temperature gradients on rainfall of the South Asian monsoon. Journal of Climate, 36 (18). pp. 6499-6513. ISSN 1520-0442 doi: 10.1175/jcli-d-22-0288.1

Abstract/Summary

The southwest monsoon delivers over 70% of India’s annual rainfall and is crucial to the success of agriculture across much of South Asia. Monsoon precipitation is known to be sensitive to sea surface temperature (SST) in the Bay of Bengal (BoB). Here, we use a configuration of the Unified Model of the UK Met Office coupled to an ocean mixed layer model to investigate the role of upper-ocean features in the BoB on southwest monsoon precipitation. We focus on the pronounced zonal and meridional SST gradients characteristic of the BoB; the zonal gradient in particular has an as-yet unknown effect on monsoon rainfall. We find that the zonal SST gradient is responsible for a 50% decrease in rainfall over the southern BoB (approximately 5 mm day−1), and a 50% increase in rainfall over Bangladesh and northern India (approximately 1 mm day−1). This increase is remotely forced by a strengthening of the monsoon Hadley circulation. The meridional SST gradient acts to decrease precipitation over the BoB itself, similarly to the zonal SST gradient, but does not have comparable effects over land. The impacts of barrier layers and high-salinity sub-surface water are also investigated, but neither has significant effects on monsoon precipitation in this model; the influence of barrier layers on precipitation is felt in the months after the southwest monsoon. Models should accurately represent oceanic processes that directly influence BoB SST, such as the BoB cold pool, in order to faithfully represent monsoon rainfall.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/112373
Item Type Article
Refereed Yes
Divisions Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Uncontrolled Keywords Atmospheric Science
Publisher American Meteorological Society
Download/View statistics View download statistics for this item

Downloads

Downloads per month over past year

University Staff: Request a correction | Centaur Editors: Update this record

Search Google Scholar