永久冻土
活动层
冻土带
下沉
植被(病理学)
遥感
干涉合成孔径雷达
地质学
图层(电子)
亚北极气候
堆栈(抽象数据类型)
环境科学
大气科学
合成孔径雷达
地貌学
北极的
海洋学
材料科学
构造盆地
薄膜晶体管
病理
复合材料
医学
程序设计语言
计算机科学
作者
Roger Michaelides,Kevin Schaefer,H. A. Zebker,A. Parsekian,Lin Liu,Jingyi Chen,Susan M. Natali,S. Ludwig,Sean Robert Schaefer
标识
DOI:10.1088/1748-9326/aaf932
摘要
The Yukon-Kuskokwim (YK) Delta is a region of discontinuous permafrost in the subarctic of southwestern Alaska. Many wildfires have occurred in the YK Delta between 1971-2015, impacting vegetation cover, surface soil moisture, and the active layer. Herein, we demonstrate that the remotely sensed active layer thickness (ReSALT) algorithm can resolve the post-fire active layer dynamics of tundra permafrost. We generated a stack of Advanced Land Observing Satellite Phased Array type L-band Synthetic Aperture Radar interferograms over a study region in the YK Delta spanning 2007-2010. We applied ReSALT to this stack of interferograms to measure seasonal subsidence associated with the freezing and thawing of the active layer and subsidence trends associated with wildfire. We isolated two wildfire-induced subsidence signatures, associated with the active layer and the permafrost layer. We demonstrate that InSAR is sensitive to increases in active layer thickness following wildfire, which recovers to pre-fire values after approximately 25 years. Simultaneously, we show that fire gradually thins the permafrost layer by 4 m, which recovers to pre-fire thickness after 70 years.
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