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Evaluation of freeze-thaw erosion in Tibet based on the cloud model

在西藏的 freezethaw 侵蚀的评估基于云模型

作     者:Junfu FAN Taoying HU Xiao YU Jiahao CHEN Liusheng HAN Yuke ZHOU 

作者机构:School of Architectural EngineeringShandong University of TechnologyZibo 255000China Bureau of Natural ResourcesShiquan 725200China Ecology Observing Network and Modeling LaboratoryInstitute of Geographical Sciences and Natural Resources ResearchChinese Academy of SciencesBeijing 100101China 

出 版 物:《Frontiers of Earth Science》 (地球科学前沿(英文版))

年 卷 期:2021年第15卷第3期

页      面:495-506页

核心收录:

学科分类:09[农学] 0903[农学-农业资源与环境] 090301[农学-土壤学] 

基  金:funded by the National Key Research and Development Program of China(No.2017YFB0503500) the Shandong Provincial Natural Science Foundation(Nos.ZR2020MD015 and ZR2020MD018) the Guangdong Academy of Sciences to build First-rate Research Institution Special Fund for Action Project(No.2019GDASYL-0103003) the Young Teacher Development Support Program of Shandong University of Technology(No.4072-115016) 

主  题:freeze-thaw erosion cloud model AHP Tibet 

摘      要:Freeze-thaw erosion can lead to accelerated soil loss,which is an important factor related to soil erosion in cold *** is a typical region that is seriously affected by freeze-thaw ***,the analytic hierarchy process(AHP)method is used to calculate the weight of the factors in evaluations of freeze-thaw erosion,but this method cannot accurately depict the fuzziness and randomness of the *** overcome this disadvantage,this study proposed an improved AHP method based on the cloud model for the evaluation of the factors impacting freeze-thaw *** establish an improved evaluation method for freeze-thaw erosion in Tibet,the following six factors were selected:mean annual air temperature,mean annual ground surface temperature,average annual precipitation,aspect,vegetation coverage,and topographic *** traditional AHP and the cloud model were combined to assign the weights of the impacting factors,and a consistency check was *** comprehensive evaluation index model was used to evaluate the intensity of freeze-thaw erosion in *** results show that freeze-thaw erosion is extensive,stretching over approximately 66.1%of ***,mild erosion and moderate erosion are the most widely distributed erosion intensity levels,accounting for 36.4%and 34.4%of the total freeze-thaw erosion,*** intensity of freeze-thaw erosion gradually increased from slight erosion in the northwest to severe erosion in the southeast of the study *** evaluation results for the intensity and distribution of freeze-thaw erosion in Tibet were confirmed to be consistent with the actual *** brief,this study supplies a new approach for quantitatively evaluating the intensity of freeze-thaw erosion in Tibet.

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