globalchange  > 过去全球变化的重建
DOI: 10.1007/s00382-011-1169-z
Scopus记录号: 2-s2.0-84861811444
论文题名:
Autumn atmospheric response to the 2007 low Arctic sea ice extent in coupled ocean-atmosphere hindcasts
作者: Orsolini Y.J.; Senan R.; Benestad R.E.; Melsom A.
刊名: Climate Dynamics
ISSN: 9307575
出版年: 2012
卷: 38, 期:2017-11-12
起始页码: 2437
结束页码: 2448
语种: 英语
英文关键词: Atmospheric modeling ; Cryosphere ; Predictability ; Sea ice ; Seasonal forecasting
英文摘要: The autumn and early winter atmospheric response to the record-low Arctic sea ice extent at the end of summer 2007 is examined in ensemble hindcasts with prescribed sea ice extent, made with the European Centre for Medium-Range Weather Forecasts state-of-the-art coupled ocean-atmosphere seasonal forecast model. Robust, warm anomalies over the Pacific and Siberian sectors of the Arctic, as high as 10°C at the surface, are found in October and November. A regime change occurs by December, characterized by weaker temperatures anomalies extending through the troposphere. Geopotential anomalies extend from the surface up to the stratosphere, associated to deeper Aleutian and Icelandic Lows. While the upper-level jet is weakened and shifted southward over the continents, it is intensified over both oceanic sectors, especially over the Pacific Ocean. On the American and Eurasian continents, intensified surface Highs are associated with anomalous advection of cold (warm) polar air on their eastern (western) sides, bringing cooler temperatures along the Pacific coast of Asia and Northeastern North America. Transient eddy activity is reduced over Eurasia, intensified over the entrance and exit regions of the Pacific and Atlantic storm tracks, in broad qualitative agreement with the upper-level wind anomalies. Potential predictability calculations indicate a strong influence of sea ice upon surface temperatures over the Arctic in autumn, but also along the Pacific coast of Asia in December. When the observed sea ice extent from 2007 is prescribed throughout the autumn, a higher correlation of surface temperatures with meteorological re-analyses is found at high latitudes from October until mid-November. This further emphasises the relevance of sea ice for seasonal forecasting in the Arctic region, in the autumn. © 2011 The Author(s).
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/55268
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作者单位: Norwegian Institute for Air Research (NILU), PO BOX 100, 2027 Kjeller, Norway; Norwegian Meteorological Institute (met. no), Oslo, Norway

Recommended Citation:
Orsolini Y.J.,Senan R.,Benestad R.E.,et al. Autumn atmospheric response to the 2007 low Arctic sea ice extent in coupled ocean-atmosphere hindcasts[J]. Climate Dynamics,2012-01-01,38(2017-11-12)
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