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DOI | 10.1007/s00382-015-2952-z |
A stable snow-atmosphere coupled mode | |
Zhao, Liang; Zhu, Yuxiang; Liu, Haiwen; Liu, Zhongfang; Liu, Yanju; Li, Xiuping; Chen, Zhou | |
通讯作者 | Zhu, YX (通讯作者) |
发表日期 | 2016 |
ISSN | 0930-7575 |
EISSN | 1432-0894 |
起始页码 | 2085 |
结束页码 | 2104 |
卷号 | 47期号:7-8 |
英文摘要 | Snow is both an important lower boundary forcing of the atmosphere and a response to atmospheric forcing in the extratropics. It is still unclear whether a stable snow-atmosphere coupled mode exists in the extratropics, like the ENSO in the tropics. Using Sliding Correlation analysis over Any Window, the present study quantitatively evaluates the stability of coupling relationships between the major modes of winter snow over the Northern Hemisphere and the winter atmospheric Arctic Oscillation (AO), the Antarctic Oscillation (AAO) and the Siberian High over the period 1872-2010, and discusses their possible relationships for different seasons. Results show that the first mode of the winter snow cover fraction and the winter AO together constitute a stable snow-atmosphere coupled mode, the SNAO. The coupled mode is stronger during recent decades than before. The snow anomaly over Europe is one key factor of the SNAO mode due to the high stability there, and the polar vortex anomaly in the atmosphere is its other key factor. The continuity of signals in the SNAO between autumn and winter is weaker than that between winter and spring. The second winter snow mode is generally stably correlated with the winter AAO and was more stable before the 1970s. The AAO signal with boreal snow has a strong continuity in seasonal transition. Generally, through these coupled modes, snow and atmosphere can interact in the same season or between different seasons: autumn snow can influence the winter atmosphere; the winter atmosphere can influence spring snow. |
关键词 | HEMISPHERE ANNULAR MODEARCTIC OSCILLATIONEXTRATROPICAL CIRCULATIONREANALYSIS PROJECTCOVER VARIABILITYSIBERIAN SNOWPART ICLIMATE20TH-CENTURYTRENDS |
英文关键词 | SNOW; Arctic oscillation; Antarctic oscillation; Siberia high; EOF analysis; Sliding correlation; Snow-atmosphere coupling |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000384549500005 |
来源期刊 | CLIMATE DYNAMICS
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258841 |
推荐引用方式 GB/T 7714 | Zhao, Liang,Zhu, Yuxiang,Liu, Haiwen,et al. A stable snow-atmosphere coupled mode[J]. 中国科学院青藏高原研究所,2016,47(7-8). |
APA | Zhao, Liang.,Zhu, Yuxiang.,Liu, Haiwen.,Liu, Zhongfang.,Liu, Yanju.,...&Chen, Zhou.(2016).A stable snow-atmosphere coupled mode.CLIMATE DYNAMICS,47(7-8). |
MLA | Zhao, Liang,et al."A stable snow-atmosphere coupled mode".CLIMATE DYNAMICS 47.7-8(2016). |
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