globalchange  > 气候减缓与适应
DOI: 10.1175/JCLI-D-17-0783.1
Scopus记录号: 2-s2.0-85048484649
论文题名:
How well do we know ENSO's climate impacts over North America, and how do we evaluate models accordingly?
作者: Deser C.; Simpson I.R.; Phillips A.S.; McKinnon K.A.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2018
卷: 31, 期:13
起始页码: 4991
结束页码: 5014
语种: 英语
英文关键词: Atmosphere-ocean interaction ; Climate variability ; ENSO ; Interannual variability
Scopus关键词: Atmospheric temperature ; Atmospheric thermodynamics ; Climate change ; Oceanography ; Surface waters ; Atmosphere-ocean interactions ; Atmospheric dynamics ; Climate variability ; ENSO ; Imperfect estimations ; Interannual variability ; Sea surface temperature anomalies ; Surface air temperatures ; Climate models ; air-sea interaction ; annual variation ; atmospheric dynamics ; climate change ; climate modeling ; El Nino-Southern Oscillation ; ensemble forecasting ; La Nina ; sampling ; sea surface temperature ; spatial variation ; North America ; Pacific Ocean ; Pacific Ocean (East)
英文摘要: The role of sampling variability in ENSO composites of winter surface air temperature and precipitation over North America during the period 1920-2013 is assessed for observations and ensembles of coupled model simulations in which sea surface temperature anomalies in the tropical eastern Pacific are nudged to those of the real world. The individual members of each model ensemble show a surprising amount of diversity in their ENSO composites, despite being constructed from the same observed set of 18 El Niño and 14 La Niña events. For a given model, this ensemble spread can only be due to sampling variability, that is, aliasing of internal variability that is unrelated to ENSO, which in turn is shown to arise from internal atmospheric dynamics rather than coupled ocean-atmosphere processes. Analogous ensemble spread is evident in 2000 synthetic ENSO composites based on observations using random sampling techniques. These synthetic composites provide information on the range of spatial patterns and amplitudes associated with imperfect estimation of the forced ENSO signal in the observational record. In some locations, the amplitude of the estimated ENSO signal can vary by more than a factor of two. This observational uncertainty necessitates an approach to model assessment that considers not only the model's forced response to ENSO, given by its ensemble-mean ENSO composite, but also its representation of internal variability unrelated to ENSO. Such an approach is used to reveal fidelities and shortcomings in the Community Earth System Model, version 1. © 2018 American Meteorological Society.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/111487
Appears in Collections:气候减缓与适应

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作者单位: National Center for Atmospheric Research, Boulder, CO, United States

Recommended Citation:
Deser C.,Simpson I.R.,Phillips A.S.,et al. How well do we know ENSO's climate impacts over North America, and how do we evaluate models accordingly?[J]. Journal of Climate,2018-01-01,31(13)
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