首页|基于TVDI的不同类型岩溶区干旱时空演变及其影响因素分析

基于TVDI的不同类型岩溶区干旱时空演变及其影响因素分析

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干旱对岩溶区的农业生产和生态环境建设的影响不可忽视.研究岩溶区的干旱对科学防旱抗旱、石漠化治理与生态建设具有重要意义.以分布有典型岩溶地貌的都安县、巧家县和印江县为研究区,计算了该地区的温度植被干旱指数(TVDI),并结合研究区岩溶地貌特点对干旱的时空变化及其与气象、地形的关系进行了分析讨论.结果表明,研究区主要遭受轻旱影响,而相对干旱主要分布于岩溶发育较强烈的区域;近20 a来,3个县的干旱趋缓,较干旱年份主要集中在2001~2010年;通过相关分析发现,3个县的TVDI与年平均温度、年降水量仅表现为中度相关或弱相关,与非岩溶区相比,研究区的TVDI与气象因子的相关性偏低.3个县的TVDI和DEM均呈现出负相关关系,其R2分别为0.52、0.58和0.67.TVDI与地形地貌、DEM数据的相关分析表明岩溶发育强烈、岩石裂隙广泛分布的岩溶区较非岩溶区更容易出现干旱,说明岩溶发育带来了更多的干旱胁迫;此外,在不同类型岩溶区,岩溶结构影响干旱发生的程度为岩溶槽谷>岩溶峡谷>峰丛洼地.建议在分析岩溶区干旱时应充分考虑其特有的二元结构的影响.
Spatial-temporal Evolution and Influencing Factors of Drought in Different Karst Areas based on TVDI
Drought has an important impact on agricultural production and construction of ecological environ-ments in karst areas.Study of drought in karst regions is of great significance for scientific drought prevention and drought relief,rock desertification management and ecological construction.The study area in this research comprises Du'an,Qiaojia,and Yinjiang,which are characterized by typical karst topography.The Temperature Vegetation Drought Index(TVDI)is calculated for these areas.Spatiotemporal pattern of drought and correla-tion between TVDI and meteorological and topographical factors are analyzed and discussed.The results show that the study areas mainly suffered mild drought,while moderate drought were mainly distributed in zones with karst development.The drought conditions in the three areas have been improving slightly in the last 20 years,and dry stress mainly concentrated in 2001~2010.It is found that the correlation between TVDI and the aver-age annual temperature and annual precipitation are weak or moderate,which are significantly lower than that in non-Karst areas.Negative correlations are found between TVDI in the three areas and DEM with R2 of 0.52,0.58 and 0.67 respectively.The correlation analysis of TVDI with topographic features and DEM shows that ar-eas with strong Karst development and widely distributed of rock fissures are more prone to drought than non-Karst areas,indicating that Karst development brings more drought stress.Furthermore,severity of the impact of Karst structure on occurrence of drought is Karst trough valley>Karst gorge>peak cluster depression.It is recommended that the impacts of the unique dualistic structure of Karst topography should be fully considered when analysing drought in Karst areas.

drought monitoringKarstTVDITopography and geomorphology

卢献健、黎振宝、晏红波、张焕铃、郭子扬

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桂林理工大学 测绘地理信息学院,广西 桂林 541006

干旱监测 岩溶 TVDI 地形地貌

广西自然科学基金项目国家自然科学基金项目

2022GXNSFBA03563942064003

2024

遥感技术与应用
中国科学院遥感联合中心

遥感技术与应用

CSTPCD北大核心
影响因子:0.961
ISSN:1004-0323
年,卷(期):2024.39(3)
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