Soil moisture initialization effects in the Indian monsoon system

  • Towards the goal to understand the role of land-surface processes over the Indian sub-continent, a series of soil-moisture sensitivity simulations have been performed using a non-hydrostatic regional climate model COSMO-CLM. The experiments were driven by the lateral boundary conditions provided by the ERA-Interim (ECMWF) reanalysis. The simulation results show that the pre-monsoonal soil moisture has a significant influence on the monsoonal precipitation. Both, positive and negative soil-moisture precipitation (S-P) feedback processes are of importance. The negative S-P feedback process is especially influential in the western and the northern parts of India.

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Metadaten
Author:Shakeel Asharaf, Andreas Dobler, Bodo AhrensORCiDGND
URN:urn:nbn:de:hebis:30:3-271426
DOI:https://doi.org/10.5194/asr-6-161-2011
ISSN:1992-0636
ISSN:1992-0628
Parent Title (English):Advances in science and research : ASR
Publisher:Copernicus-Ges.
Place of publication:Katlenburg-Lindau
Document Type:Article
Language:English
Date of Publication (online):2012/12/19
Date of first Publication:2011/06/14
Publishing Institution:Universitätsbibliothek Johann Christian Senckenberg
Release Date:2012/12/19
Volume:6
Page Number:5
First Page:161
Last Page:165
Note:
© Author(s) 2011. This work is distributed under the Creative Commons Attribution 3.0 License.
Note:
10th EMS Annual Meeting and 8th European Conference on Applied Climatology (ECAC) 2010
HeBIS-PPN:315857528
Institutes:Geowissenschaften / Geographie / Geowissenschaften
Dewey Decimal Classification:5 Naturwissenschaften und Mathematik / 55 Geowissenschaften, Geologie / 550 Geowissenschaften
Sammlungen:Universitätspublikationen
Licence (German):License LogoCreative Commons - Namensnennung 3.0