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库姆塔格沙漠东缘荒漠绿洲过渡带风况及输沙势     被引量:17

Wind regime and resultant sand-transporting potential in the desert-oasis ecotone in the eastern marginal zone of the Kumtag Desert

文献类型:期刊文献

中文题名:库姆塔格沙漠东缘荒漠绿洲过渡带风况及输沙势

英文题名:Wind regime and resultant sand-transporting potential in the desert-oasis ecotone in the eastern marginal zone of the Kumtag Desert

作者:王永胜[1,2] 杨文斌[1,2] 李永华[1,2] 李清雪[1,2] 冯伟[1,2]

第一作者:王永胜

机构:[1]中国林业科学研究院荒漠化研究所;[2]国家林业局库姆塔格荒漠生态系统定位研究站

年份:2015

卷号:0

期号:1

起止页码:140-144

中文期刊名:干旱区资源与环境

外文期刊名:Journal of Arid Land Resources and Environment

收录:北大核心:【北大核心2014】;CSSCI:【CSSCI2014_2016】;CSCD:【CSCD_E2015_2016】;

基金:"十二五"科技支撑项目(2012BAD16B0104);国家林业公益性行业科研专项项目(201304325)资助

语种:中文

中文关键词:风况;起沙风;输沙势;荒漠绿洲过渡带;库姆塔格沙漠

外文关键词:wind regime; threshold wind of transporting sand; sand transport potential; desert-oasis ecotone; Kumtag Desert

分类号:P468

摘要:以国家林业局库姆塔格荒漠生态系统定位研究站2012-2013年的气象资料为依据,分析了库姆塔格沙漠东缘荒漠-绿洲过渡带的风况特征和输沙势变化情况。结果表明:1)研究区主要受WNW-NW和ENE-NE两组风向起沙风控制,其中主风向为WNW-NW,占全年起沙风的35.15%,次风向为ENE-NE,占全年起沙风的24.80%;2)该区起沙风主要发生在春季和夏季,占全年起沙风的72.59%,春季起沙风主风向为ENE,其他季节起沙风的主风向为WNW方向。3)在风沙活动期内,年合成输沙势(RDP)为54.73VU,合成输沙势方向(DDR)为S189°,研究区属于低风能环境。研究区输沙势的大小具有明显的季节性,其中春季和夏季具有较高的总输沙势(DP)和合成输沙势(DDR)。
The desert- oasis ecotone in the eastern marginal zone of the Kumtag Desert is one of the areas with the severest desertification in China. In this study a statistical analysis on wind regime and resultant sand- transporting potential from 2012 to 2013 in the eastern marginal zone of the Kumtag Desert was carried out. The results showed that:( 1) This region was affected predominantly by WNW- NW 和 ENE- NE wind directions,there was a higher accumulated frequency with 35. 15% in the WNW- NW direction,and the frequency of sand-moving wind in the ENE- NE was 24. 8%;( 2) Sand- moving wind in the study area occurred mainly in the spring and summer,its occurring frequency was 72. 59%,the prevailing wind in spring was ENE,and WNW in other seasons;( 3) During the phase of wind- sand activity,resultant sand- transporting potential( RDP) was54. 73 VU,resultant sand- transporting directon( RDD) was 189°S. There was a higher sand- transporting potential( RDP) and drift potential( DP) in the spring and summer.

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