Numerical simulation of the sensitivity of summer monsoon circulation and rainfall over india to land surface processes

Raman, S. ; Mohanty, U. C. ; Reddy, N. C. ; Alapaty, K. ; Madala, R. V. (1998) Numerical simulation of the sensitivity of summer monsoon circulation and rainfall over india to land surface processes Pure and Applied Geophysics, 152 (4). pp. 781-809. ISSN 0033-4553

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Official URL: http://www.springerlink.com/content/74flfjcqa8hrtb...

Related URL: http://dx.doi.org/10.1007/s000240050178

Abstract

The influence of soil moisture and vegetation variation on simulation of monsoon circulation and rainfall is investigated. For this purpose a simple land surface parameterization scheme is incorporated in a three-dimensional regional high resolution nested grid atmospheric model. Based on the land surface parameterization scheme, latent heat and sensible heat fluxes are explicitly estimated over the entire domain of the model. Two sensitivity studies are conducted; one with bare dry soil conditions (no latent heat flux from land surface) and the other with realistic representation of the land surface parameters such as soil moisture, vegetation cover and landuse patterns in the numerical simulation. The sensitivity of main monsoon features such as Somali jet, monsoon trough and tropical easterly jet to land surface processes are discussed. Results suggest the necessity of including a detailed land surface parameterization in the realistic short-range weather numerical predictions. An enhanced short-range prediction of hydrological cycle including precipitation was produced by the model, with land surface processes parameterized. This parameterization appears to simulate all the main circulation features associated with the summer monsoon in a realistic manner.

Item Type:Article
Source:Copyright of this article belongs to Birkhauser-Verlag.
Keywords:Numerical Simulation; Summer Monsoon; Circulation; Land Surface; Parameterization
ID Code:26597
Deposited On:08 Dec 2010 13:31
Last Modified:17 May 2016 09:53

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