|
|
|
|
LEADER |
01799 am a22002173u 4500 |
001 |
114588 |
042 |
|
|
|a dc
|
100 |
1 |
0 |
|a Nicholson, S. E.
|e author
|
100 |
1 |
0 |
|a Massachusetts Institute of Technology. Department of Civil and Environmental Engineering
|e contributor
|
100 |
1 |
0 |
|a Whittleston, David
|e contributor
|
100 |
1 |
0 |
|a Entekhabi, Dara
|e contributor
|
700 |
1 |
0 |
|a Schlosser, A.
|e author
|
700 |
1 |
0 |
|a Whittleston, David
|e author
|
700 |
1 |
0 |
|a Entekhabi, Dara
|e author
|
245 |
0 |
0 |
|a Climate Models Lack Jet-Rainfall Coupling over West Africa
|
260 |
|
|
|b American Meteorological Society,
|c 2018-04-06T14:34:03Z.
|
856 |
|
|
|z Get fulltext
|u http://hdl.handle.net/1721.1/114588
|
520 |
|
|
|a Changes in large-scale dynamics over West Africa-the strength and position of zonal jets-are a key interim step by which local and remote forcing is communicated into changes in rainfall. This study identifies a key mode of jet variability and demonstrates how it is strongly coupled with rainfall. The approach provides a quantitative framework to assess jet-rainfall coupling and a useful tool to investigate the concerning spread in CMIP5 rainfall projections over the West African Sahel. It is shown that many CMIP5 simulations fail to capture this coupling, indicating a fundamental limitation in their ability to predict future rainfall conditions. The results demonstrate that West African rainfall in the coming CMIP6 ensemble should be interpreted with caution; key atmospheric processes that deliver rainfall must be validated before conducting detailed analysis on rainfall. Keywords: Africa; Dynamics; Jets; Monsoons; Hydrometeorology; Model evaluation/performance
|
520 |
|
|
|a United States. National Aeronautics and Space Administration (Grant NNX09AK26G)
|
655 |
7 |
|
|a Article
|
773 |
|
|
|t Journal of Climate
|