globalchange  > 气候变化事实与影响
DOI: 10.1175/JCLI-D-11-00273.1
Scopus记录号: 2-s2.0-84859153199
论文题名:
Observed Antarctic interannual climate variability and tropical linkages
作者: Schneider D.P.; Okumura Y.; Deser C.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2012
卷: 25, 期:12
起始页码: 4048
结束页码: 4066
语种: 英语
Scopus关键词: Antarctic climate ; Antarctic Peninsula ; Antarctic stations ; Antarctica ; Atmospheric conditions ; Austral spring ; Austral summers ; Circulation patterns ; Climate linkages ; Coastal station ; Decadal timescale ; Deep convection ; Eddy momentum flux ; ENSO events ; Ice core ; Ice core records ; Interannual climate variability ; Meridional circulation ; Rossby wave ; ROSSBY wave propagation ; Sea level pressure ; Sea surface temperature (SST) ; Seasonality ; Southern Annular Mode ; Spatial patterns ; Subtropical jet ; Teleconnections ; Temperature anomaly ; Temperature data ; Tropical climates ; Climate change ; Ice ; Ocean currents ; Sea level ; Tropics ; annual variation ; climate change ; climate variation ; decadal variation ; El Nino-Southern Oscillation ; ice core ; meridional circulation ; precipitation (climatology) ; regression analysis ; Rossby wave ; sea level pressure ; sea surface temperature ; seasonality ; spatial analysis ; teleconnection ; temperature anomaly ; Antarctic Peninsula ; Antarctica ; East Antarctica ; Pacific Ocean ; Pacific Ocean (Tropical) ; West Antarctica
英文摘要: This study reviews the mechanisms associated with Antarctic-tropical climate linkages and presents new analyses of the seasonality and spatial patterns of tropical climate signals in the Antarctic for the late 1950s to the present. Tropical climate signals are primarily communicated to the Antarctic via the Pacific-South America (PSA) pattern and the southern annular mode (SAM). The impacts of these circulation patterns and their tropical linkages are evident in regressions of seasonally stratified Antarctic station temperature data and annually resolved ice core records on global fields of sea surface temperature, sea level pressure, and precipitation. Temperature and ice core anomalies in the Antarctic Peninsula region and adjoining areas of West Antarctica are significantly impacted by the PSA, interpreted as a Rossby wave train driven by anomalous tropical deep convection during ENSO events. This pattern is most evident in the austral spring, consistent with recent studies, suggesting that atmospheric conditions for Rossby wave propagation are most favorable during this season. During austral summer at the peak of theENSO cycle, temperature anomalies at East Antarctic coastal stations exhibit significant correlations with tropical Pacific anomalies. This linkage reflects the influence of anomalous tropical heating on the position and strength of the subtropical jets and is consistent with changes in eddy momentum fluxes that alter the mean meridional circulation associated with the SAM. Of the ice cores that exhibit tropical linkages, most tend to be associated with the PSA teleconnection. The implications of the study's findings for understanding Antarctic climate variability and climate change from seasonal to decadal time scales are also discussed. © 2012 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/52359
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作者单位: Climate and Global Dynamics Division, Earth System Laboratory, National Center for Atmospheric Research, Boulder, CO, United States

Recommended Citation:
Schneider D.P.,Okumura Y.,Deser C.. Observed Antarctic interannual climate variability and tropical linkages[J]. Journal of Climate,2012-01-01,25(12)
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