PDF Download

[1]QI Donglin,LI Xiaodong,SU Wenjiang,et al.Tendency of Spatiotemporal Evolution of Wind Erosion Climatic Erosivity in Qinghai Province in Recent 50 Years[J].Research of Soil and Water Conservation,2015,22(06):234-239.

Copy

Tendency of Spatiotemporal Evolution of Wind Erosion Climatic Erosivity in Qinghai Province in Recent 50 Years

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 22 Number of periods: 2015 06 Page number: 234-239 Column: Public date: 2015-12-28

Title:: Tendency of Spatiotemporal Evolution of Wind Erosion Climatic Erosivity in Qinghai Province in Recent 50 Years

Author(s):: QI Donglin¹, LI Xiaodong^1,2, SU Wenjiang¹, ZHOU Wanfu¹, XIAO Hongbin¹; 1. Qinghai Institute of Meteorological Science, Xining 810001, China;
2. Institute of Plateau Meteorology, CMA, Chengdu 610072, China

Keywords:: wind erosion climatic erosivity; wind erosion climatic erosivity factor; relative contribution rate; Mann-Kendall test; Qinghai Province

CLC:: P425.6

DOI:: -

Abstract:: By making use of calculation method of wind erosion climatic erosivity factor index developed by FAO and observation data from 43 meteorological stations during 1961 to 2010 in Qinghai Province, we analyzed the basic features of wind erosion climatic erosivity. The results showed that the range of wind erosion climatic erosivity factor index of C value varied from -12.9 to 160.1; the average of C value was 32.4 in Qinghai Province. Spatially, C value displayed the decrease trend from northwest to southeast and the maximum of C value appeared at Mangai in the Qaidam Basin. Wind erosion climatic erosivity factor had seasonal and inter-monthly variation, the highest value showed in spring, the second one in winter and the lowest one in summer. Wind erosion climatic erosivity factor had the decrease tendency in recent 50 years which revealed that wind erosion climatic erosivity was reducing. Wind speed was main restricting factors of wind erosion climatic erosivity. The relationship between wind erosion climatic erosivity, precipitation and sandstorm days was not significant.

References:: [1] 董玉祥.沙漠化灾害危险度评价的初步研究[J].自然灾害学报,1993,2(3):103-109.
[2] Chepil W S, Siddoway F H, Armbrust D V. Climatic factor for estimating wind erodibility fields[J]. Journal of Soil and Water Conservation,1962,17(4):162-165.
[3] Skidmore E L. Wind erosion climatic erosivity[J]. Climatic change,1986,9(1/2):195-208.
[4] 柯克比M J, 摩根R P C.土壤侵蚀[M].王礼先,吴斌,洪惜英,译.北京:水利电力出版社,1987.
[5] 拉尔R.土壤侵蚀研究方法[M].北京:科学出版社,1991.
[6] 董玉祥,康国定.中国干旱半干旱地区风蚀气候侵蚀力的计算和分析[J].水土保持学报,1994,8(3):1-7.
[7] 方祖光,谢皎如.福建沿海地区干燥度和风蚀气候侵蚀力的计算与分析[J].福建师范大学学报:自然科学版,1997,13(3):96-103.
[8] 王永,赵举,程玉臣.阴山北麓农牧交错带风蚀气候侵蚀力的计算与分析[J].华北农学报,2005,20(专辑):57-60.
[9] 朱丽,秦富仓,杨翠林,等.阴山北麓农牧交错带土壤侵蚀驱动机制研究[J].水土保持研究,2008,15(5):34-37.
[10] 冯伟,张兴昌,高照良.风力侵蚀对西气东输(甘肃段)工程影响分析[J].水土保持研究,2008,15(2):244-251.
[11] 何清,胡文峰,杨兴华,等.拐子湖地区沙尘天气风蚀起沙量的估算[J].水土保持研究,2012,19(1):6-10.
[12] 蒋冲,陈爱芳,喻小勇,等.黄土高原风蚀与水蚀复合区的风蚀气候侵蚀力变化[J].干旱区研究,2013,30(3):477-483.
[13] 杨兴华,何清,李红军,等.塔里木盆地风蚀气候侵蚀力的计算和分析[J].中国沙漠,2012,32(4):990-995.
[14] 郑度.青藏高原形成环境与发展[M].石家庄:河北科学技术出版社,2003.
[15] 王根绪,李元寿,王一博.青藏高原河源区地表过程与环境变化[M].北京:科学出版社,2010.
[16] 李林,汪青春,时兴合,等.青海省太阳能风能监测评估服务技术[M].北京:气象出版社,2013.
[17] 中国气象局.生态质量气象评价规范[M].北京:中国气象局,2005.
[18] 魏凤英.现代气候统计诊断与预测技术[M].北京:气象出版社,2007.
[19] 方精云.地理要素对我国温度分布影晌的数量评价[J].地理学报,1992,12(2):97-104.
[20] 张嘉琪,任志远.1977-2010年柴达木盆地地表潜在蒸散时空演变趋势[J].资源科学,2014,36(10):2103-2112.
[21] 王江山,李锡福.青海天气气候[M].北京:气象出版社,2004.

Similar References:

Memo

Last Update: 1900-01-01