DOI: | 10.1007/s00382-015-2690-2
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Scopus记录号: | 2-s2.0-84933074116
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论文题名: | Rainfall variability and predictability issues for North AMERICA |
作者: | Hunt B.G.
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刊名: | Climate Dynamics
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ISSN: | 9307575
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出版年: | 2016
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卷: | 46, 期:2017-07-08 | 起始页码: | 2067
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结束页码: | 2085
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语种: | 英语
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英文关键词: | Dust bowl simulation
; Multi-millennial simulation
; North American rainfall
; Predictability of North American rainfall
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英文摘要: | A multi-millennial simulation with a coupled global climatic model has been used to investigate extreme rainfall events, mainly droughts, over North America. A rainfall index, based on the US Dust Bowl region, was used to generate a time series from which the extreme events could be identified. A very wide range of drought and pluvial multiyear sequences was obtained, all attributable to internal climatic variability. This time series reproduced the basic characteristics of the corresponding observed time series. Composites of years with negative rainfall anomalies over North America from the simulation replicated the observed rainfall composite for the Dust Bowl era, both in spatial character and intensity. Examination of individual years of a simulated composite revealed not only a wide range of rainfall anomaly patterns, dominated by drought conditions, but also ENSO distributions that included El Niño events as well as the expected La Niña events. Composites for pluvial conditions over North America were associated with composited El Niño events, as expected. Correlation of the simulated Dust Bowl rainfall with global surface temperatures identified a principal connection with the ENSO region. No systematic relationship was obtained in the simulation between the Atlantic multidecadal oscillation and Dust Bowl region rainfall, with the simulated oscillation having a much more variable periodicity than that found in the limited observations. However, a marked connection was found for SST anomalies adjacent to the northeast coast of North America, but this appears to be forced by ENSO events. A scatter diagram of NINO3.4 SST anomalies with the Dust Bowl region rainfall anomalies, for observations and the simulation, revealed inconsistencies between the occurrence of an ENSO event and the “expected” rainfall anomaly. This, and other analysis, resulted in the conclusion that annual or longer term rainfall predictions over North America, with any systematic confidence, are unlikely because of stochastic influences inherent in the climatic system associated with internal climatic variability. © 2016, The Microbiological Society of Korea. |
Citation statistics: |
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资源类型: | 期刊论文
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标识符: | http://119.78.100.158/handle/2HF3EXSE/53666
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Appears in Collections: | 过去全球变化的重建
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作者单位: | CSIRO Oceans and Atmosphere Flagship, Private Bag 1, Aspendale, VIC, Australia
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Recommended Citation: |
Hunt B.G.. Rainfall variability and predictability issues for North AMERICA[J]. Climate Dynamics,2016-01-01,46(2017-07-08)
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