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DOI | 10.1175/JCLI-D-12-00093.1 |
Observed Coherent Trends of Surface and Upper-Air Wind Speed over China since 1960 | |
Lin, Changgui; Yang, Kun; Qin, Jun; Fu, Rong | |
通讯作者 | Yang, K (通讯作者) |
发表日期 | 2013 |
ISSN | 0894-8755 |
EISSN | 1520-0442 |
起始页码 | 2891 |
结束页码 | 2903 |
卷号 | 26期号:9 |
英文摘要 | Previous studies indicated that surface wind speed over China declined during past decades, and several explanations exist in the literature. This study presents long-term (1960-2009) changes of both surface and upper-air wind speeds over China and addresses observed evidence to interpret these changes. It is found that surface wind over China underwent a three-phase change over the past 50 yr: (i) it step changed to a strong wind level at the end of the 1960s, (ii) it declined until the beginning of the 2000s, and (iii) it seemed to be steady and even recovering during the very recent years. The variability of surface wind speed is greater at higher elevations and less at lower elevations. In particular, surface wind speed over the elevated Tibetan Plateau has changed more significantly. Changes in upper-air wind speed observed from rawinsonde are similar to surface wind changes. The NCEP-NCAR reanalysis indicates that wind speed changes correspond to changes in geopotential height gradient at 500 hPa. The latter are further correlated with the changes of latitudinal surface temperature gradient, with a correlation coefficient of 0.88 for the past 50 yr over China. This strongly suggests that the spatial gradient of surface global warming or cooling may significantly change surface wind speed at a regional scale through atmospheric thermal adaption. The recovery of wind speed since the beginning of the 2000s over the Tibetan Plateau might be a precursor of the reversal of wind speed trends over China, as wind over high elevations can respond more rapidly to the warming gradient and atmospheric circulation adjustment. |
关键词 | ATMOSPHERIC HEAT-SOURCETIBETAN PLATEAUGEOPOTENTIAL HEIGHTWEAKENING TRENDOSCILLATIONTEMPERATURESUMMERCIRCULATIONMONSOON |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000318159500012 |
来源期刊 | JOURNAL OF CLIMATE |
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/258212 |
推荐引用方式 GB/T 7714 | Lin, Changgui,Yang, Kun,Qin, Jun,et al. Observed Coherent Trends of Surface and Upper-Air Wind Speed over China since 1960[J]. 中国科学院青藏高原研究所,2013,26(9). |
APA | Lin, Changgui,Yang, Kun,Qin, Jun,&Fu, Rong.(2013).Observed Coherent Trends of Surface and Upper-Air Wind Speed over China since 1960.JOURNAL OF CLIMATE,26(9). |
MLA | Lin, Changgui,et al."Observed Coherent Trends of Surface and Upper-Air Wind Speed over China since 1960".JOURNAL OF CLIMATE 26.9(2013). |
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