| 1960―2015年长江流域风速的时空变化特征 |
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| 引用本文： | 李悦佳,贺新光,卢希安,谭子芳.1960―2015年长江流域风速的时空变化特征[J].热带地理,2018,38(5):660-667. |
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| 作者姓名： | 李悦佳 贺新光 卢希安 谭子芳 |
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| 作者单位： | （湖南师范大学 a．资源与环境科学学院；b．地理空间大数据挖掘与应用湖南省重点实验室，长沙 410081） |
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| 基金项目： | 国家自然科学基金（41472238）；湖南省十二五重点学科地理学（20110001） |
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| 摘 要： | 基于1960―2015年长江流域128个站点的月风速观测数据，结合地形特点将长江流域分成5个子区域，并运用一元线性回归、相关分析和修正的Mann-Kendall（MMK）检验对长江流域风速变化趋势的时空特征进行研究，结果表明：1）1960―2015年长江流域年平均风速以-0.006 5 m/s·a的速率显著下降，5个子区域中，区域中下游丘陵与平原区（R1）下降最显著，上游青藏高原区（R5）次之，上游盆地区（R3）变化最小。2）季节上，全区风速春季下降最快，夏季最慢。而子区域除R1冬季降幅最大外，其余区域季节风速变化速率也为春季降幅最大，夏季最小。逐月变化上，流域整体风速3月下降最快，8月最慢，各子区域风速最大降幅也集中在3月。3）空间分布上，长江流域年平均风速降幅呈现东部大、中部小、西部较大的特点，全区50%的站点下降趋势显著，且这些站点集中分布于R1地区。此外，4个季节风速与年风速的变化趋势呈现相似的空间分布特征。4）长江流域风速下降与北极涛动（AO）指数上升、区域气候变暖和城市化加速等有关。
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| 关 键 词： | 气候变化 风速 长江流域 北极涛动 |
Spatio-temporal Variability of Wind Speed in the Yangtze River Basin during 1960-2015 |
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| LI Yuejia,HE Xinguang,LU Xi’an and TAN Zifang.Spatio-temporal Variability of Wind Speed in the Yangtze River Basin during 1960-2015[J].Tropical Geography,2018,38(5):660-667. |
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| Authors: | LI Yuejia HE Xinguang LU Xi’an and TAN Zifang |
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| Institution: | （a．College of Resources and Environmental Science；b．Key Laboratory of Geospatial Big Data Mining and Application， Hunan Normal University，Changsha 410081，China） |
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| Abstract: | Based on the monthly wind speed data of 128 meteorological stations during 1960-2015 in the Yangtze River Basin, and five divided sub-regions according to the terrain, the temporal and spatial characteristics of wind speed variation in the Basin are analyzed by using the linear regression estimation, correlation analysis and modified Mann-Kendall (MMK) trend test. The results are as follows: 1) There is a significant weakening trend over the Yangtze River Basin with the average decreasing rate of -0.006 5 m/s·a in annual mean wind speed. The highest annual mean wind speed over the Basin is 2.17 m/s which occurred in 1969, and the least is 1.63 m/s which occurred in 2002. For the five sub-regions, the most significant downward trend occurs in sub-region R1 (hilly and plain areas in the middle and lower reaches), followed by R5 (Qinghai-Tibet Plateau areas in the upper reaches), and the last one is R3 (the basin areas in the upper reaches). 2) Seasonally, in the whole basin, the most significant weakening is found in spring and the least in summer. The trends in the sub-regions are also found that the most weakening is in spring and the least is in summer except for R1 where the most weakening occurs in winter. Furthermore, the non-significantly slightly increasing trends in summer are found in the sub-regions R2 and R3. Monthly, in the Yangtze River Basin, the most significant weakening of wind speed occurs in March, while the most non-significant one is in August. The most significant weakening monthly is also in March in all sub-regions. 3) Spatially, the annual wind speed and its decreasing trend exhibit similar spatial patterns with being the largest in the eastern basin, larger in the western and the smallest in the central, which means that those stations with higher average annual wind speed in Yangtze River Basin also have larger declining rate of wind speed. There are 50% of stations showing the most significant decline that are located in the east of the basin, especially in R1. In addition, there is a similar spatial distribution in trends with respect to seasonal and annual wind speeds. 4) The decrease of mean annual, spring and winter wind speed over the Yangtze River Basin and its sub-regions R1 and R2 is related to the increase of Arctic Oscillation (AO). Over the whole basin and its sub-regions R1 and R2, the correlation coefficients between annual mean wind speed and AO are -0.25, -0.30 and -0.27, respectively, the correlation coefficients between spring wind speed and AO are -0.28, -0.27 and -0.30, respectively, and the correlation coefficients between winter wind speed and AO are -0.29, -0.30 and -0.25, respectively. Besides, the decrease of pressure gradient force in coastal areas may play a role in the decline of winter wind speed in R1. The non-significantly slightly increasing trend in summer in sub-region R3 is possibly caused by an almost unchanged long-term temperature in this area. Moreover, the regional climate warming and urbanization acceleration have also impacts on the decrease of wind speed in the basin |
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| Keywords: | climate change wind speed the Yangtze River Basin Arctic Oscillation |
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