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On the Role of the African Topography in the South Asian Monsoon

Wei, Ho-Hsuan and Bordoni, Simona (2016) On the Role of the African Topography in the South Asian Monsoon. Journal of the Atmospheric Sciences, 73 (8). pp. 3197-3212. ISSN 0022-4928. http://resolver.caltech.edu/CaltechAUTHORS:20151203-110419620

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Abstract

The Somali jet, a strong low-level cross-equatorial flow concentrated in a narrow longitudinal band near the coast of Somalia, is a key feature of the South Asian monsoon (SAM) circulation. Previous work has emphasized the role of the East African highlands in strengthening and concentrating the jet. However, the fundamental dynamics of the jet remains debated, as does its relation to the SAM precipitation. In this study, numerical experiments with modified topography over Africa are conducted with the GFDL atmospheric model, version 2.1 (AM2.1), general circulation model (GCM) to examine the influence of topography on the Somali jet and the SAM precipitation. It is found that when the African topography is removed, the SAM precipitation moderately increases in spite of a weakening of the cross-equatorial Somali jet. The counterintuitive precipitation increase is related to lower-level cyclonic wind anomalies, and associated meridional moisture convergence, which develop over the Arabian Sea in the absence of the African topography. Potential vorticity (PV) budget analyses along particle trajectories show that this cyclonic anomaly primarily arises because, in the absence of the blocking effect by the African topography and with weaker cross-equatorial flow, air particles originate from higher latitudes with larger background planetary vorticity and thus larger PV.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1175/JAS-D-15-0182.1DOIArticle
http://journals.ametsoc.org/doi/10.1175/JAS-D-15-0182.1PublisherArticle
ORCID:
AuthorORCID
Bordoni, Simona0000-0003-4771-3350
Additional Information:© 2016 American Meteorological Society. Manuscript received 3 July 2015, in final form 11 May 2016. Published online: 25 July 2016. This work was partially supported by the Caltech Terrestrial Hazard and Reporting (THOR) Center. We thank Brian Hoskins, an anonymous reviewer, and Ming Cai for their helpful review and insightful suggestions. We also thank Zhiming Kuang, Ian Eisenman, andOlivier Pauluis for the helpful discussions. The numerical simulations and analyses were conducted on the Caltech’s Division of Geological and Planetary Sciences CITerra high-performance computing cluster.
Funders:
Funding AgencyGrant Number
Caltech Terrestrial Hazard Observation and Reporting (THOR) CenterUNSPECIFIED
Subject Keywords:Circulation/ Dynamics; Potential vorticity; Stationary waves; Topographic effects; Atm/Ocean Structure/ Phenomena; Monsoons; Physical Meteorology and Climatology; Moisture/moisture budget; Models and modeling; Climate models
Record Number:CaltechAUTHORS:20151203-110419620
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20151203-110419620
Official Citation:Ho-Hsuan Wei and Simona Bordoni, 2016: On the Role of the African Topography in the South Asian Monsoon. J. Atmos. Sci., 73, 3197–3212, doi: 10.1175/JAS-D-15-0182.1.
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:62576
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:04 Dec 2015 17:25
Last Modified:22 Aug 2016 20:01

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