| Literature DB >> 23878328 |
Richard Washington1, Rachel James, Helen Pearce, Wilfried M Pokam, Wilfran Moufouma-Okia.
Abstract
The Congo Basin is one of three key convective regions on the planet which, during the transition seasons, dominates global tropical rainfall. There is little agreement as to the distribution and quantity of rainfall across the basin with datasets differing by an order of magnitude in some seasons. The location of maximum rainfall is in the far eastern sector of the basin in some datasets but the far western edge of the basin in others during March to May. There is no consistent pattern to this rainfall distribution in satellite or model datasets. Resolving these differences is difficult without ground-based data. Moisture flux nevertheless emerges as a useful variable with which to study these differences. Climate models with weak (strong) or even divergent moisture flux over the basin are dry (wet). The paper suggests an approach, via a targeted field campaign, for generating useful climate information with which to confront rainfall products and climate models.Entities:
Keywords: CMIP5; Congo rainfall; climatology; moisture flux
Mesh:
Year: 2013 PMID: 23878328 PMCID: PMC3720019 DOI: 10.1098/rstb.2012.0296
Source DB: PubMed Journal: Philos Trans R Soc Lond B Biol Sci ISSN: 0962-8436 Impact factor: 6.237