青藏高原冰冻圈温度遥感观测、反演与应用

doi:10.11947/j.AGCS.2024.20230261

测绘学报 ›› 2024, Vol. 53 ›› Issue (5): 835-847.doi: 10.11947/j.AGCS.2024.20230261

• 青藏高原冰冻圈重大变化专栏 • 上一篇下一篇

青藏高原冰冻圈温度遥感观测、反演与应用

周纪¹(), 王子卫¹, 丁利荣², 唐文彬¹, 王伟¹, 马晋¹, 蒋蕙如³, 刘双⁴, 张涛¹, 侯映旭¹

^1.电子科技大学资源与环境学院，四川　成都　611731
^2.中航（成都）无人机系统股份有限公司，四川　成都　611731
^3.同济大学测绘与地理信息学院，上海　200092
^4.中国科学院、水利部成都山地灾害与环境研究所，四川　成都　610299

收稿日期:2023-06-28 修回日期:2024-04-29 发布日期:2024-06-19
作者简介:周纪（1983—），男，博士，教授，研究方向为定量热红外遥感。E-mail：jzhou233@uestc.edu.cn
基金资助:
国家自然科学基金(42271387);四川省自然科学基金杰出青年基金(2023NSFSC1907)

Remote sensing observation, retrieval, and analysis of temperature in the Qinghai-Tibet Plateau cryosphere

Ji ZHOU¹(), Ziwei WANG¹, Lirong DING², Wenbin TANG¹, Wei WANG¹, Jin MA¹, Huiru JIANG³, Shuang LIU⁴, Tao ZHANG¹, Yingxu HOU¹

^1.School of Resources and Environment, University of Electronic Science and Technology of China, Chengdu 611731, China
^2.AVIC (Chengdu) UAS Co., Ltd., Chengdu 611731, China
^3.College of Surveying and GEO-Informatics, Tongji University, Shanghai 200092, China
^4.Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610299, China

Received:2023-06-28 Revised:2024-04-29 Published:2024-06-19
About author:ZHOU Ji (1983—), male, PhD, professor, majors in quantitative thermal infrared remote sensing. E-mail: jzhou233@uestc.edu.cn
Supported by:
The National Natural Science Foundation of China(42271387);The Science Fund for Distinguished Young Scholars of Sichuan Province(2023NSFSC1907)

摘要/Abstract

摘要：

冰冻圈是气候变化的灵敏指示器，地表温度和近地表气温则是指示器直接感测的信号，是回溯冰冻圈演化历史、监测当前状态、模拟未来变化的关键参量。受恶劣环境、复杂地形、低可达性及众多特殊下垫面等因素的综合影响，当前青藏高原温度的地面观测困难、站点稀少，而遥感已成为温度获取的有效手段。本文聚焦地表温度和近地表气温，阐明了地面观测、卫星和无人机等遥感反演估算的相关方法手段，梳理和总结了学术界围绕青藏高原冰冻圈取得的研究进展，介绍了遥感温度参量在青藏高原冻土、湖冰、冰川等方面的应用。本文总结了青藏高原冰冻圈对温度遥感获取的挑战，探讨了未来值得着重开展的研究方向。

关键词: 地表温度, 近地表气温, 青藏高原, 冰冻圈, 遥感

Abstract:

The cryosphere serves as a sensitive indicator of climate change, while land surface temperature and near-surface air temperature are signals directly sensed by the indicator. They are key parameters for tracing the evolution history of the cryosphere, monitoring the current state, and simulating future changes. Due to a combination of adverse environmental conditions, complex terrain, low accessibility, and numerous unique underlying surfaces, ground-based temperature observations are challenging and sparsely distributed in the Qinghai-Tibet Plateau. Remote sensing has become an effective means of temperature acquisition. Focusing on land surface temperature and near-surface air temperature, this paper elucidates the related methodologies for ground-based observations, satellite, and unmanned aerial vehicle (UAV) remote sensing retrievals, and summarizes the research progress made by the academic community around the cryosphere of the Qinghai-Tibet Plateau. Furthermore, this paper discusses the applications of remote sensing temperature parameters in frozen ground, lake ice, glaciers, and other aspects of the Qinghai-Tibet Plateau. Challenges in temperature remote sensing acquisition in the Qinghai-Tibet Plateau cryosphere are summarized, and future research directions worthy of emphasis are explored.

Key words: land surface temperature, near-surface air temperature, Qinghai-Tibet Plateau, cryosphere, remote sensing

中图分类号:

P237

周纪, 王子卫, 丁利荣, 唐文彬, 王伟, 马晋, 蒋蕙如, 刘双, 张涛, 侯映旭. 青藏高原冰冻圈温度遥感观测、反演与应用[J]. 测绘学报, 2024, 53(5): 835-847.

Ji ZHOU, Ziwei WANG, Lirong DING, Wenbin TANG, Wei WANG, Jin MA, Huiru JIANG, Shuang LIU, Tao ZHANG, Yingxu HOU. Remote sensing observation, retrieval, and analysis of temperature in the Qinghai-Tibet Plateau cryosphere[J]. Acta Geodaetica et Cartographica Sinica, 2024, 53(5): 835-847.

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青藏高原冰冻圈温度遥感观测、反演与应用

Remote sensing observation, retrieval, and analysis of temperature in the Qinghai-Tibet Plateau cryosphere

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