【作者单位】1Institute of Geographical Science, Taiyuan Normal University, Jinzhong 030619, Shanxi, China;2State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China;3Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China;4Zhuhai Branch of State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Zhuhai 519087, Guangdong, China;5College of Urban and Environmental Sciences, Hubei Normal University, Huangshi 435002, Hubei, China;6Institute of Geographical Sciences, Henan Academy of Sciences, Zhengzhou 450052, Henan, China;7School of Geography and Tourism, Shaanxi Normal University, Xi'an 710119, China;8School of Geography and Tourism, Anhui Normal University, Wuhu 241002, Anhui, China
【摘要】 Climbing dunes are a form of topographic barrier dunes that feature in the aeolian landforms on the Qinghai-Tibetan Plateau. Topography fundamentally influences the spatial distribution and morphological characteristics of climbing dunes by modifying...