Significance of variations in the wind energy environment over the past 50 years with respect to dune activity and desertification in and and semiarid northern China

被引:55
作者
Wang, Xunming [1 ,2 ]
Eerdun, Hasi [3 ]
Zhou, Zijiang [4 ]
Liu, Xiaoping [3 ]
机构
[1] Chinese Acad Sci, Cold Arid Reg Environm & Engn Res Inst, Key Lab Desert & Desertificat, Lanzhou 730000, Peoples R China
[2] Lanzhou Univ, MOE Key Lab W China Environm Syst, CAEP, Lanzhou 730000, Peoples R China
[3] Beijing Normal Univ, China Ctr Desert Res, Beijing 100875, Peoples R China
[4] China Natl Meteorol Informat Ctr, Beijing 100081, Peoples R China
基金
中国国家自然科学基金;
关键词
wind energy environment; aeolian activity; desertification; northern china;
D O I
10.1016/j.geomorph.2006.09.003
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Climate data from 339 meteorological stations collected from the 1950s to the early 2000s was employed to discuss aeolian activity in and and semiarid northern China. The results show that at decadal time scales, erosivity varied greatly in this region. Most of and and semiarid northern China was characterised by environments with moderate to low wind energy. After the 1980s, the erosivity was only 20 to 50% of that beforehand, and this difference had a significant impact on the environmental changes observed during the two periods. The dune mobility index was consistent with the observed dune activity. After the 1980s dune activity decreased and in some deserts with vegetated dune systems during the 1970s most of the dune plinths were active until the 1980s, after which only the crests were active. Some mobile dunes that had developed at the margins of mobile deserts were replaced by semi-anchored or anchored dunes. Because most desert areas with vegetated dune systems in and and semiarid northern China are used for farming or grazing, the results of our monitoring show that the desertification trends were consistent with the trends in erosivity and dune activity in this region. Desertification was controlled much more by climatic changes than has previously been acknowledged, and especially by fluctuations in wind energy. (c) 2006 Elsevier B.V All rights reserved.
引用
收藏
页码:252 / 266
页数:15
相关论文
共 89 条
[1]  
[Anonymous], 1993, World Atlas of Desertification
[2]  
Ash J.E., 1983, Z GEOMORPHOLOGIE S, V45, P7
[3]   PRESENT-DAY DUNE PROCESSES AND DUNE MORPHOLOGY ON THE LEBA BARRIER, POLISH COAST OF THE BALTIC [J].
BOROWKA, RK .
GEOGRAFISKA ANNALER SERIES A-PHYSICAL GEOGRAPHY, 1980, 62 (1-2) :75-82
[4]  
Bullard JE, 1997, EARTH SURF PROC LAND, V22, P165, DOI 10.1002/(SICI)1096-9837(199702)22:2&lt
[5]  
165::AID-ESP687&gt
[6]  
3.0.CO
[7]  
2-9
[8]   A note on the use of the ''Fryberger Method'' for evaluating potential sand transport by wind [J].
Bullard, JE .
JOURNAL OF SEDIMENTARY RESEARCH, 1997, 67 (03) :499-501
[9]  
Bullard JE, 1996, EARTH SURF PROC LAND, V21, P263, DOI 10.1002/(SICI)1096-9837(199603)21:3&lt
[10]  
263::AID-ESP627&gt