Modes of coastal precipitation over southwest India and their relationship to intraseasonal variability

[thumbnail of Open Access]
Preview
Text (Open Access) - Published Version
· Available under License Creative Commons Attribution.
· Please see our End User Agreement before downloading.
| Preview
Available under license: Creative Commons Attribution
[thumbnail of main-v2 (3).pdf]
Text - Accepted Version
· Restricted to Repository staff only
Restricted to Repository staff only

Please see our End User Agreement.

It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing.

Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Hunt, K. M. R. orcid id iconORCID: https://orcid.org/0000-0003-1480-3755, Turner, A. G. orcid id iconORCID: https://orcid.org/0000-0002-0642-6876, Stein, T. H. M. orcid id iconORCID: https://orcid.org/0000-0002-9215-5397, Fletcher, J. K. and Schiemann, R. H. orcid id iconORCID: https://orcid.org/0000-0003-3095-9856 (2021) Modes of coastal precipitation over southwest India and their relationship to intraseasonal variability. Quarterly Journal of the Royal Meteorological Society, 147 (734). pp. 181-201. ISSN 1477-870X doi: 10.1002/qj.3913

Abstract/Summary

The west coast of India, dominated by the Western Ghats mountain range, is among the rainiest places in the tropics. The interaction between the land-sea contrast of the coast, the monsoonal westerlies, and the oblique mountains is subject to complex intraseasonal variability, which has not previously been explored in depth. This study investigates that variability from the perspective of the land-sea contrast, using empirical orthogonal function analysis to discern regimes of onshore and offshore rainfall over southwest India and the eastern Indian Ocean. Locally, it is found that the rainfall is most sensitive to mid-tropospheric humidity: when this is anomalously high, deep convection is encouraged; when this is anomalously low, it is suppressed. A moisture tracking algorithm is employed to determine the primary sources of the anomalously wet and dry mid-tropospheric air. There are important secondary contributions from low-level vorticity and cross-shore moisture flux. The dominant control on intraseasonal variability in coastal precipitation is found to be the BSISO: over 75% of the strongest offshore events occur during phases 3 and 4; and about 40% of the strongest onshore events occur during phases 5 and 6. The location of monsoon low-pressure systems is also shown to be important in determining the magnitude and location of coastal rainfall.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/92889
Identification Number/DOI 10.1002/qj.3913
Refereed Yes
Divisions Science > School of Mathematical, Physical and Computational Sciences > NCAS
Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Publisher Royal 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