Affiliation:
1. Department of Environmental Health Sciences, Columbia University, New York, New York
Abstract
Abstract
An analysis and characterization of seasonal changes in the atmospheric teleconnection between ENSO and western European precipitation, as well as atmospheric conditions over the North Atlantic and Europe, are presented. Significant ENSO-associated changes in precipitation are evident during the boreal spring and fall seasons, marginal during boreal summer, and absent during boreal winter. The spring and fall precipitation anomalies are accompanied by statistically significant ENSO-related changes in large-scale fields over the North Atlantic and Europe. These seasonal teleconnections appear to be mediated by changes in upper tropospheric conditions along the coast of Europe that project down to the lower troposphere and produce onshore or offshore moisture flux anomalies, depending on the season. Some ENSO-related changes in storm activity are also evident during fall and winter. Analyses during boreal winter reveal little effect of coincident ENSO conditions on either European precipitation or upper tropospheric conditions over Europe.
Publisher
American Meteorological Society
Reference61 articles.
1. The version 2 Global Precipitation Climatology Project (GPCP) monthly precipitation analysis (1979–present);Adler;J. Hydrometeor.,2003
2. Classification, seasonality, and persistence of low-frequency atmospheric circulation patterns;Barnston;Mon. Wea. Rev.,1987
3. Horizontal structure of 500-mb height fluctuations with long, intermediate, and short time scales;Blackmon;J. Atmos. Sci.,1984
4. Time variation of 500-mb height fluctuations with long, intermediate, and short time scales as deduced from lag-correlation statistics;Blackmon;J. Atmos. Sci.,1984
5. Analysis of general circulation model sea-surface temperature anomaly simulations using a linear model. Part I: Forced solutions;Branstator;J. Atmos. Sci.,1985
Cited by
42 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献