Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1007/s00382-019-04616-4 |
Seasonal climatology and dynamical mechanisms of rainfall in the Caribbean | |
Martinez, Carlos1,2; Goddard, Lisa2; Kushnir, Yochanan1; Ting, Mingfang1 | |
2019-07-01 | |
发表期刊 | CLIMATE DYNAMICS
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ISSN | 0930-7575 |
EISSN | 1432-0894 |
出版年 | 2019 |
卷号 | 53页码:825-846 |
文章类型 | Article |
语种 | 英语 |
国家 | USA |
英文摘要 | The Caribbean is a complex region that heavily relies on its rainfall cycle for its economic and societal needs. This makes the Caribbean especially susceptible to hydro-meteorological disasters (i.e. droughts and floods). Previous studies have investigated the seasonal cycle of rainfall in the Caribbean with monthly or longer resolutions that often mask the seasonal transitions and regional differences of rainfall. This has resulted in inconsistent findings on the seasonal cycle. In addition, the mechanisms that shape the climatological rainfall cycle in the region are not fully understood. To address these problems, this study conducts: (i) a principal component analysis of the annual cycle of precipitation across 38 Caribbean stations using daily observed precipitation data; and, (ii) a moisture budget analysis for the Caribbean, using the ERA-Interim Reanalysis. This study finds that the seasonal cycle of rainfall in the Caribbean hinges on three main facilitators of moisture convergence: the Eastern Pacific ITCZ, the Atlantic ITCZ, and the western flank of the North Atlantic Subtropical High (NASH). The Atlantic Warm Pool and Caribbean Low-Level Jet modify the extent of moisture provided by these main facilitators. The expansion and contraction of the western flank of NASH generate the bimodal pattern of the precipitation annual cycle in the northwestern Caribbean, central Caribbean, and with the Eastern Pacific ITCZ the western Caribbean. This study identifies the Atlantic ITCZ as the major source of precipitation for the central and southern Lesser Antilles, which is responsible for their unimodal rainfall pattern. Convergence by sub-monthly transients contributes little to Caribbean rainfall. |
英文关键词 | Climate variability Precipitation Large-scale dynamics Caribbean |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000471722400049 |
WOS关键词 | INTERTROPICAL CONVERGENCE ZONE ; LOW-LEVEL JET ; ERA-INTERIM REANALYSIS ; MIDSUMMER DROUGHT ; AMERICA ; PRECIPITATION ; SEA ; VARIABILITY ; MOISTURE ; PATTERNS |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/184407 |
专题 | 气候变化 |
作者单位 | 1.Columbia Univ, Lamont Doherty Earth Observ, 61 US-9W, Palisades, NY 10964 USA; 2.Columbia Univ, Int Res Inst Climate & Soc, 61 US-9W, Palisades, NY 10964 USA |
推荐引用方式 GB/T 7714 | Martinez, Carlos,Goddard, Lisa,Kushnir, Yochanan,et al. Seasonal climatology and dynamical mechanisms of rainfall in the Caribbean[J]. CLIMATE DYNAMICS,2019,53:825-846. |
APA | Martinez, Carlos,Goddard, Lisa,Kushnir, Yochanan,&Ting, Mingfang.(2019).Seasonal climatology and dynamical mechanisms of rainfall in the Caribbean.CLIMATE DYNAMICS,53,825-846. |
MLA | Martinez, Carlos,et al."Seasonal climatology and dynamical mechanisms of rainfall in the Caribbean".CLIMATE DYNAMICS 53(2019):825-846. |
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