ID:
publications-2650
Type:
Peer reviewed articles
Year:
2017
Authors:
A. Orr, C. Listowski, M. Couttet, E. Collier, W. Immerzeel, P. Deb, D. Bannister
Title:
Sensitivity of simulated summer monsoonal precipitation in Langtang Valley, Himalaya, to cloud microphysics schemes in WRF
Venue/Journal:
Journal of Geophysical Research: Atmospheres
DOI:
10.1002/2016JD025801
Research type:
Data Management & Analytics
Water System:
Water Distribution Networks
Technical Focus:
Abstract:
AbstractA better understanding of regionalāscale precipitation patterns in the Himalayan region is required to increase our knowledge of the impacts of climate change on downstream water availability. This study examines the impact of four cloud microphysical schemes (Thompson, Morrison, Weather Research and Forecasting (WRF) singleāmoment 5āclass, and WRF doubleāmoment 6āclass) on summer monsoon precipitation in the Langtang Valley in the central Nepalese Himalayas, as simulated by the WRF model at 1Ā km grid spacing for a 10Ā day period in July 2012. The model results are evaluated through a comparison with surface precipitation and radiation measurements made at two observation sites. Additional understanding is gained from a detailed examination of the microphysical characteristics simulated by each scheme, which are compared with measurements using a spaceborne radar/lidar cloud product. Also examined are the roles of largeā and smallāscale forcings. In general, the schemes are able to capture the timing of surface precipitation better than the actual amounts in the Langtang Valley, which are predominately underestimated, with the Morrison scheme showing the best agreement with the measured values. The schemes all show a large positive bias in incoming radiation. Analysis of the radar/lidar cloud product and hydrometeors from each of the schemes suggests that ācoldārainā processes are a key precipitation formation mechanism, which is also well represented by the Morrison scheme. As well as microphysical structure, both largeāscale and localized forcings are also important for determining surface precipitation.
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676819
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