PDF Download

[1]CHANG Chun-ping,YUAN Li-feng.A Disscussion on the Status, Origin and Developmental Trends of Blown-Sand in the Valley of Lower Reaches of Lhasa River, Tibet Plateau[J].Research of Soil and Water Conservation,2010,17(01):122-126.

Copy

A Disscussion on the Status, Origin and Developmental Trends of Blown-Sand in the Valley of Lower Reaches of Lhasa River, Tibet Plateau

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 17 Number of periods: 2010 01 Page number: 122-126 Column: Public date: 2010-02-20

Title:: A Disscussion on the Status, Origin and Developmental Trends of Blown-Sand in the Valley of Lower Reaches of Lhasa River, Tibet Plateau

Author(s):: CHANG Chun-ping¹, YUAN Li-feng²; 1. College of Resources and Environment Sciences, Hebei Normal University, Shijiazhuang, 050016, China;
2. Department of Electronics and Information Science, Nanjing University of Posts and Telecommunications, Nanjing, 210003, China

Keywords:: the lower Lhasa river valley; present situation; origin; trends

CLC:: P445.4

DOI:: -

Abstract:: Based on the field survey of the lower Lhasa river valley and the interpretation results of IKONOS and Quick Bird’s video,finding out the source of sand and dust storm in the valley distribute along river valley and its two sides,the distribution’s physiographical places are varety and sporadic,small size.Such feature cause serious hazards of sand to the urban environment and agricultural production.The analysis show that the vulnerable ecological environment in the plateau climate conditions,the characteristics of sand sources,vegetation condition and the intense human activities are the main causes of disaster.Finally,the analysis of human activities and climate change trend indicates that in the the next 15 years,the climate change unsuitable weakened sandstorm’ strength,human activities’ intensity of strengthening effect to the sandstorm will gradually decrease,however,in general,it is still has the strengthening effect.Lhasa river valley will tend to strengthen the disaster,if the human measures not be taken.

References:: [1] 徐海量,陈亚宁.塔里木盆地风沙灾害危险性评价[J].自然灾害学报,2003,12(2):35-39.
[2] 倪雪.拉萨贡嘎机场干季风沙、浮尘天气特征及预报初探[J].四川气象,2001,21(4):46-48.
[3] 周顺武,黄琼中.拉萨市空气污染物浓度的统计分析及其可能的天气原因[J].西藏科技,2002(5):39-42.
[4] 黄琼中.拉萨市环境空气质量与气象特征分析[J].中国环境监测,2001,17(6):50-53.
[5] 缪启龙,向毓意,顾显跃.气候变化对西藏环境经济的可能影响[J].应用气象学报,1998,9(2):225-230.
[6] 董治宝,李振山.风成沙粒度特征对其风蚀可蚀性的影响[J].土壤侵蚀与水土保持学报,1998,4(4):1-5,12.
[7] 代加冼.青藏高原气候学[M].北京:气象出版社,1990.
[8] 吴祥定,林振耀.历史时期青藏高原高原气候变化特征的初步分析[J].气象学报,1981,39(1):90-97.
[9] 吴祥定,林振耀.横断山区近代气候变化的研究[J].地理研究,1987,6(2):48-55.
[10] 林振耀,赵昕奕.青藏高原气温降水变化的空间特征[J].中国科学:D辑,1996,26(4):354-358.

Similar References:

Memo

Last Update: 1900-01-01