Rapid degradation of permafrost underneath waterbodies in tundra   landscapes-Toward a representation of thermokarst in land surface models

doi:10.1002/2016JF003956

CORC > 北京大学 > 城市与环境学院

	Rapid degradation of permafrost underneath waterbodies in tundra landscapes-Toward a representation of thermokarst in land surface models
	Langer, M. ; Westermann, S. ; Boike, J. ; Kirillin, G. ; Grosse, G. ; Peng, S. ; Krinner, G.
刊名	JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE
	2016
关键词	LENA RIVER DELTA ARCTIC COASTAL-PLAIN ICE-RICH PERMAFROST NORTHERN SIBERIA THAW LAKES CARBON-DIOXIDE WATER TEMPERATURE THERMAL REGIME ENERGY BALANCE SNOW COVER
DOI	10.1002/2016JF003956
英文摘要	Waterbodies such as lakes and ponds are abundant in vast Arctic landscapes and strongly affect the thermal state of the surrounding permafrost. In order to gain a better understanding of the impact of small-and medium-sized waterbodies on permafrost and the formation of thermokarst, a land surface model was developed that can represent the vertical and lateral thermal interactions between waterbodies and permafrost. The model was validated using temperature measurements from two typical waterbodies located within the Lena River delta in northern Siberia. Impact simulations were performed under current climate conditions as well as under a moderate and a strong climate-warming scenario. The performed simulations demonstrate that small waterbodies can rise the sediment surface temperature by more than 10 degrees C and accelerate permafrost thaw by a factor of between 4 and 5. Up to 70% of this additional heat flux into the ground was found to be dissipated into the surrounding permafrost by lateral ground heat flux in the case of small, shallow, and isolated waterbodies. Under moderate climate warming, the lateral heat flux was found to reduce permafrost degradation underneath waterbodies by a factor of 2. Under stronger climatic warming, however, the lateral heat flux was too small to prevent rapid permafrost degradation. The lateral heat flux was also found to strongly impede the formation of thermokarst. Despite this stabilizing effect, our simulations have demonstrated that underneath shallow waterbodies (<1 m), thermokarst initiation happens 30 to 40 years earlier than in simulations without preexisting waterbody.; Feodor Lynen Fellowship of the Alexander von Humboldt Foundation; European Union FP7-ENV project PAGE21 [GA282700]; COUP [244903/E10]; COUP (JPI Climate); COUP (Research Council of Norway); ERC [338335]; SCI(E); ARTICLE; moritz.langer@geo.hu-berlin.de; 12; 2446-2470; 121
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/458165]
专题	城市与环境学院
推荐引用方式 GB/T 7714	Langer, M.,Westermann, S.,Boike, J.,et al. Rapid degradation of permafrost underneath waterbodies in tundra landscapes-Toward a representation of thermokarst in land surface models[J]. JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE,2016.
APA	Langer, M..,Westermann, S..,Boike, J..,Kirillin, G..,Grosse, G..,...&Krinner, G..(2016).Rapid degradation of permafrost underneath waterbodies in tundra landscapes-Toward a representation of thermokarst in land surface models.JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE.
MLA	Langer, M.,et al."Rapid degradation of permafrost underneath waterbodies in tundra landscapes-Toward a representation of thermokarst in land surface models".JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE (2016).