Wikindx Resources

Journal Article: ID no. (ISBN etc.):  0903-7575 (Print) 1432-0894 (Online) BibTeX citation key:  Druyan2009b
Druyan, L. M., Feng, J., Cook, K. H., Xue, Y., Fulakeza, M., Hagos, S. M., Konaré, A., Moufouma-Okia, W., Rowell, D. P., Vizy, E. K. & Ibrah, S. S. (2009) The WAMME regional model intercomparison study. IN Climate Dynamics, .
Added by: roussot 2010-02-12 12:31:36    Last Edited by: Fanny Lefebvre 2011-01-17 15:33:08
 B  
Categories: Weather to Climatic modelling and forecasting
Keywords: Downscaling, Modelling
Creators: Cook, Druyan, Feng, Fulakeza, Hagos, Ibrah, Konaré, Moufouma-Okia, Rowell, Vizy, Xue
Collection: Climate Dynamics
Bibliographies: Prior150410

Peer reviewed
Number of views:  1084
Popularity index:  57.35%
Maturity index:  published

 
Abstract
Results from five regional climate models (RCMs) participating in the West African Monsoon Modeling and Evaluation (WAMME) initiative are analyzed. The RCMs were driven by boundary conditions from National Center for Environmental Prediction reanalysis II data sets and observed sea-surface temperatures (SST) over four May–October seasons, (2000 and 2003–2005). In addition, the simulations were repeated with two of the RCMs, except that lateral boundary conditions were derived from a continuous global climate model (GCM) simulation forced with observed SST data. RCM and GCM simulations of precipitation, surface air temperature and circulation are compared to each other and to observational evidence. Results demonstrate a range of RCM skill in representing the mean summer climate and the timing of monsoon onset. Four of the five models generate positive precipitation biases and all simulate negative surface air temperature biases over broad areas. RCM spatial patterns of June–September mean precipitation over the Sahel achieve spatial correlations with observational analyses of about 0.90, but within two areas south of 10°N the correlations average only about 0.44. The mean spatial correlation coefficient between RCM and observed surface air temperature over West Africa is 0.88. RCMs show a range of skill in simulating seasonal mean zonal wind and meridional moisture advection and two RCMs overestimate moisture convergence over West Africa. The 0.5° computing grid enables three RCMs to detect local minima related to high topography in seasonal mean meridional moisture advection. Sensitivity to lateral boundary conditions differs between the two RCMs for which this was assessed. The benefits of dynamic downscaling the GCM seasonal climate prediction are analyzed and discussed.
Document
This paper is a contribution to the special issue on West African Climate, consisting of papers from the African Multidisciplinary Monsoon Analysis (AMMA) and West African Monsoon Modeling and Evaluation (WAMME) projects, and coordinated by Y. Xue and P. M. Ruti.
Added by: roussot    Last Edited by: Fanny Lefebvre