Arid
项目编号41501069
近20年来青藏高原冰川雪线高度时空变化研究
郭忠明
主持机构西北大学
开始日期2016
结束日期2018
资助经费200000(CNY)
项目类别青年科学基金项目
资助机构CN-NSFC(国家自然科学基金)
语种中文
国家中国
英文简介Tibetan Plateau is a region with best developed mountain glaciers in the middle and low-latitude. Glacier is the important water resources for industry and agriculture production in arid area of Northwest China. Glaciers snowline altitudes is an important indicator of glacier changes formation and evolution. Research of the snowline altitude focused only on a single glacial or small region at present. Our study base on the high temporal and spatial resolution remote sensing images and Digital Elevation Model data, and convert the pre-processed remote sensing data into broadband albedo. We classify the glacier surface in the late summer melt season into snow cover zone (accumulation area) and bare ice zone (ablation area) according to the difference between ice and snow albedo, furthermore, decide the snowline altitude and analyze the accuracy of snowline altitude, and finally real the spatial and temporal variations in the snowline altitudes of the glaciers in the Tibetan Plateau. Moreover, we combine the meteorological data to discuss the snowline altitude response to the climate. The study have important significance to estimate glacier mass balance, understanding of regional climate change, reconstruction of the paleoclimate and assessment of glacier ablation process and its impact on water resources.
中文关键词冰川 ; 雪线高度 ; 青藏高原 ; 时空变化
来源机构西北大学
资源类型项目
条目标识符http://119.78.100.177/qdio/handle/2XILL650/346995
推荐引用方式
GB/T 7714
郭忠明.近20年来青藏高原冰川雪线高度时空变化研究.2016.
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