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DOI | 10.1016/j.rse.2024.114075 |
Augmenting daily MODIS LST with AIRS surface temperature retrievals to estimate ground temperature and permafrost extent in High Mountain Asia | |
Kim, Kyung Y.; Haagenson, Ryan; Kansara, Prakrut; Rajaram, Harihar; Lakshmi, Venkataraman | |
发表日期 | 2024 |
ISSN | 0034-4257 |
EISSN | 1879-0704 |
起始页码 | 305 |
卷号 | 305 |
英文摘要 | Permafrost in High Mountain Asia (HMA) is becoming increasingly vulnerable to thaw due to climate change. However, the lack of either in situ ground surface or borehole temperature data beyond the Tibetan Plateau prevents comprehensive assessments of its impact on the regional hydrologic cycle and local cascading hazards. Although past studies have generated estimates of permafrost extent in Central Asia, many are limited to the Tibetan Plateau, excluding the more remote reaches of the Tien Shan, Pamirs, and Himalayas. By leveraging surface temperatures from both the Moderate Resolution Imaging Spectroradiometer (MODIS) and Atmospheric Infra-Red Sounder (AIRS), this study advances further understanding of remotely sensed permafrost occurrence at high altitudes, which are prone to error due to frequent cloud cover. We demonstrate that the fusion of MODIS and AIRS products can accurately estimate long-term thermal regimes of the subsurface, with reported correlation coefficients of 0.773 and 0.560, RMSEs of 0.890 degree celsius and 0.680 degree celsius, and biases of 0.003 degree celsius and 0.462 degree celsius, respectively, for the ground surface and the depth of zero annual amplitude, during a reference period of 2003-2016. Furthermore, we provide a range of possible permafrost extents based on established equations for calculating the temperature at the top of the permafrost to demonstrate temperature sensitivity to soil moisture and snow cover. The MODIS-AIRS product is recommended to be a robust source of ground temperature estimates, which may be sufficient for inferring mountain permafrost presence in HMA. Incorporating the influence of soil moisture and snow depth, although limited by biased estimates, also produces estimates of permafrost regional areas comparable to previously reported permafrost indices. A total permafrost area of 1.69 (+/- 0.32) million km(2) is estimated for the entire HMA, across 15 mountain subregions. |
英文关键词 | Permafrost; MODIS land surface temperature; AIRS surface skin temperature; High Mountain Asia |
语种 | 英语 |
WOS研究方向 | Environmental Sciences & Ecology ; Remote Sensing ; Imaging Science & Photographic Technology |
WOS类目 | Environmental Sciences ; Remote Sensing ; Imaging Science & Photographic Technology |
WOS记录号 | WOS:001206803600001 |
来源期刊 | REMOTE SENSING OF ENVIRONMENT
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/307176 |
作者单位 | University of Virginia; Johns Hopkins University |
推荐引用方式 GB/T 7714 | Kim, Kyung Y.,Haagenson, Ryan,Kansara, Prakrut,et al. Augmenting daily MODIS LST with AIRS surface temperature retrievals to estimate ground temperature and permafrost extent in High Mountain Asia[J],2024,305. |
APA | Kim, Kyung Y.,Haagenson, Ryan,Kansara, Prakrut,Rajaram, Harihar,&Lakshmi, Venkataraman.(2024).Augmenting daily MODIS LST with AIRS surface temperature retrievals to estimate ground temperature and permafrost extent in High Mountain Asia.REMOTE SENSING OF ENVIRONMENT,305. |
MLA | Kim, Kyung Y.,et al."Augmenting daily MODIS LST with AIRS surface temperature retrievals to estimate ground temperature and permafrost extent in High Mountain Asia".REMOTE SENSING OF ENVIRONMENT 305(2024). |
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