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艾比湖流域风沙强度特征及其空间差异
引用本文:马倩,武胜利,吴烨,赵枫.艾比湖流域风沙强度特征及其空间差异[J].水土保持通报,2014(4):21-27.
作者姓名:马倩  武胜利  吴烨  赵枫
作者单位:新疆师范大学地理科学与旅游学院, 新疆乌鲁木齐 830054;新疆干旱区湖泊环境与资源实验室, 新疆乌鲁木齐 830054;新疆师范大学地理科学与旅游学院, 新疆乌鲁木齐 830054;新疆干旱区湖泊环境与资源实验室, 新疆乌鲁木齐 830054;新疆气象信息中心, 新疆乌鲁木齐 830002;新疆师范大学地理科学与旅游学院, 新疆乌鲁木齐 830054;新疆干旱区湖泊环境与资源实验室, 新疆乌鲁木齐 830054
基金项目:国家自然科学基金项目"艾比湖流域抛物线沙丘形成演化研究"(41161004); 新疆干旱区湖泊环境与资源重点实验室开放基金项目(XJDX0909-2010-06; XJDX0909-2012-14; XJDX09092012-13); 新疆师范大学博士启动基金项目(XJNUBS1401)
摘    要:以艾比湖流域内6个国家气象站2005—2011年的气象资料为依据,分析了艾比湖流域的起沙风况特征、输沙势(DP)变化及风沙强度的空间差异。结果表明:(1)研究区风向以NW和NNW向为主,其频率分别占54.98%和18.31%。(2)该区起沙风主要发生在4,5和6月,其频率分别占全年的12.48%,14.70%和13.08%。输沙势的季节变化幅度较大,主要集中在春夏两季。(3)研究区合成输沙势(RDP)及合成输沙方向(RDD)分别为988.86VU和126.5°(ESE—SE),属于高风能环境。风向变率指数(RDP/DP)为0.94,属于单风风况特征。(4)研究区风沙强度表现为高值点是以孤点出现,为阿拉山口,而低值区则是一个面积较为广阔的区域。

关 键 词:起沙风  输沙势  空间差异  艾比湖流域
收稿时间:2013/6/22 0:00:00
修稿时间:2013/9/13 0:00:00

Characteristics of Sand-blown Intensity and Spatial Differences in Ebinur Lake Basin
MA Qian,WU Sheng-li,WU Ye and ZHAO Feng.Characteristics of Sand-blown Intensity and Spatial Differences in Ebinur Lake Basin[J].Bulletin of Soil and Water Conservation,2014(4):21-27.
Authors:MA Qian  WU Sheng-li  WU Ye and ZHAO Feng
Institution:College of Geography Sciences and Tourism, Xinjiang Normal University, Urumqi, Xinjiang 830054, China;Xinjiang Laboratory of Lake Environment and Resources in Arid Zone, Urumqi, Xinjiang 830054, China;College of Geography Sciences and Tourism, Xinjiang Normal University, Urumqi, Xinjiang 830054, China;Xinjiang Laboratory of Lake Environment and Resources in Arid Zone, Urumqi, Xinjiang 830054, China;Xinjiang Meteorological Information Center, Urumqi, Xinjiang 830002, China;College of Geography Sciences and Tourism, Xinjiang Normal University, Urumqi, Xinjiang 830054, China;Xinjiang Laboratory of Lake Environment and Resources in Arid Zone, Urumqi, Xinjiang 830054, China
Abstract:Sand driving wind characteristics, drift potential(DP) changes and spatial difference of sand strength in Ebinur Lake Basin was analyzed based on the data of six national weather stations during the period from 2005 to 2011. The results are as follows:(1) The wind direction in the study area are NW and NNW, and the occurring frequency were 54.98% and 18.31%, respectively.(2) The threshold wind occurs mainly in April, May and June, the occurring frequency were 12.48%, 14.70% and 13.08%, respectively. There are big differences of sand drift potential in defferent seasons, and the drift potential was concentrated in the spring and summer.(3) The variability index is 0.94, It belongs to a single air damper characteristic, resultant drift potential(RDP) and resultant drift direction(RDD) are 988.86 VU and 126.5°(ESE-SE).(4) The wind strength of study area appears a high value point as Alashankou, while the low value point is a wide area.
Keywords:sand-driving wind  sand drift potential  spatial differences  Ebinur Lake Basin
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