Climate Change Data Portal
DOI | 10.1002/joc.3807 |
Observed surface wind speed in the Tibetan Plateau since 1980 and its physical causes | |
You, Qinglong; Fraedrich, Klaus; Min, Jinzhong; Kang, Shichang; Zhu, Xiuhua; Pepin, Nick; Zhang, Ling | |
发表日期 | 2014 |
ISSN | 0899-8418 |
EISSN | 1097-0088 |
卷号 | 34期号:6 |
英文摘要 | Climate warming on the Tibetan Plateau (TP) potentially influences many climate parameters other than temperature including wind speed, cloudiness and precipitation. Temporal trends of surface wind speed at 71 stations above 2000 m above sea level in the TP are examined during 1980-2005. To uncover causes of observed trends in wind speed, relationships with surface temperature, a TP index and sunshine duration are also analysed. The TP index is calculated as the accumulated 500 hPa geopotential height above 5000 m over the region of 30 degrees N-40 degrees N, 75 degrees E-105 degrees E from NCEP/NCAR reanalysis. The annual mean wind speed patterns during 1980-2005 are similar to those in different seasons, with higher wind speeds in the northern and western parts of the TP. Highest mean wind speeds occur in spring and lowest in autumn. During 1980-2005, annual and seasonal mean wind speeds show statistically decreasing trends at most stations. The mean trend magnitude for annual mean wind speed is -0.24 m s(-1) decade(-1), with the maximum decline in spring (-0.29 m s(-1) decade(-1)) and minimum in autumn (-0.19 m s(-1) decade(-1)). Both annually and in different seasons, wind speed is significantly negatively correlated with mean temperature, minimum temperature, maximum temperature, and the TP index, but significantly positively correlated with sunshine duration. Wind speed trends fail to show a simple elevation dependency but speeds are positively correlated with meridional surface temperature/pressure gradients. Warming in the TP may weaken the latitudinal gradients of both regional temperature and surface pressure, thus altering the regional atmospheric circulation and accounting in part for the observed decline of wind speed. |
关键词 | Tibetan Plateauwind speedTibetan Plateau indexMann-Kendall analysis |
学科领域 | Meteorology & Atmospheric Sciences |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
来源期刊 | INTERNATIONAL JOURNAL OF CLIMATOLOGY |
来源机构 | 中国科学院西北生态环境资源研究院 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/111719 |
作者单位 | Nanjing Univ Informat Sci & Technol, Minist Educ, Key Lab Meteorol Disaster, Nanjing 210044, Jiangsu, Peoples R China |
推荐引用方式 GB/T 7714 | You, Qinglong,Fraedrich, Klaus,Min, Jinzhong,et al. Observed surface wind speed in the Tibetan Plateau since 1980 and its physical causes[J]. 中国科学院西北生态环境资源研究院,2014,34(6). |
APA | You, Qinglong.,Fraedrich, Klaus.,Min, Jinzhong.,Kang, Shichang.,Zhu, Xiuhua.,...&Zhang, Ling.(2014).Observed surface wind speed in the Tibetan Plateau since 1980 and its physical causes.INTERNATIONAL JOURNAL OF CLIMATOLOGY,34(6). |
MLA | You, Qinglong,et al."Observed surface wind speed in the Tibetan Plateau since 1980 and its physical causes".INTERNATIONAL JOURNAL OF CLIMATOLOGY 34.6(2014). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。