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DOI | 10.1007/s00382-020-05350-y |
Seasonal asymmetry of equatorial East African rainfall projections: understanding differences between the response of the long rains and the short rains to increased greenhouse gases | |
Cook K.H.; Fitzpatrick R.G.J.; Liu W.; Vizy E.K. | |
发表日期 | 2020 |
ISSN | 0930-7575 |
起始页码 | 1759 |
结束页码 | 1777 |
卷号 | 55 |
英文摘要 | Ensemble simulations with a regional climate model on a large domain and 30-km resolution are used to understand why projected precipitation changes under greenhouse gas-forcing are asymmetric across seasons in equatorial East Africa, with rainfall increasing during the short rains (October through December) but not during the long rains (March through May). The model captures an accurate simulation of observed East African precipitation improving over coupled GCM simulations. Future simulations are generated by increasing atmospheric CO2 according to the RCP8.5 scenario and adding anomalies to observed SSTs as well as initial and lateral boundary conditions derived from coupled GCM simulations. In November, simulated rainfall rates increase by approximately one-third over much of equatorial East Africa by the mid-twenty-first century, and double by the end of the century. The long rains are not significantly increased. The difference in the seasonal response is attributed to differences in the background state. The East African short rains are greatest in November, more than 1 month after the autumnal equinox, when the climatological basic state is in a solstitial pattern. The well-defined heat low over southern Africa and the South Indian Ocean subtropical high to its east are intensified, leading to enhanced moisture convergence over equatorial East Africa. In contrast, the long rains are near their maximum on the vernal equinox, with a continental thermal low centered near the equator that is insensitive to twenty-first century greenhouse gas-induced changes in the subtropical atmospheric hydrodynamics. © 2020, Springer-Verlag GmbH Germany, part of Springer Nature. |
英文关键词 | Angola low; East Africa; East Africa precipitation projections; East Africa precipitation trends; East African climate change projections; East African long rains; East African precipitation; East African short rains; Mascarene high; South Indian high; Turkana channel |
语种 | 英语 |
scopus关键词 | asymmetry; atmospheric moisture; carbon dioxide; climate modeling; computer simulation; greenhouse gas; hydrodynamics; precipitation assessment; rainfall; regional climate; seasonal variation; temperature anomaly; East Africa |
来源期刊 | Climate Dynamics |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/145341 |
作者单位 | Department of Geological Sciences, University of Texas at Austin, Austin, TX, United States; University of California at Davis, Davis, CA, United States |
推荐引用方式 GB/T 7714 | Cook K.H.,Fitzpatrick R.G.J.,Liu W.,et al. Seasonal asymmetry of equatorial East African rainfall projections: understanding differences between the response of the long rains and the short rains to increased greenhouse gases[J],2020,55. |
APA | Cook K.H.,Fitzpatrick R.G.J.,Liu W.,&Vizy E.K..(2020).Seasonal asymmetry of equatorial East African rainfall projections: understanding differences between the response of the long rains and the short rains to increased greenhouse gases.Climate Dynamics,55. |
MLA | Cook K.H.,et al."Seasonal asymmetry of equatorial East African rainfall projections: understanding differences between the response of the long rains and the short rains to increased greenhouse gases".Climate Dynamics 55(2020). |
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