气候变化领域集成服务门户(CCPortal): Frozen debris lobe morphology and movement: An overview of eight dynamic features, southern Brooks Range, Alaska

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DOI	10.5194/tc-10-977-2016
	Frozen debris lobe morphology and movement: An overview of eight dynamic features, southern Brooks Range, Alaska
	Darrow M.M.; Gyswyt N.L.; Simpson J.M.; Daanen R.P.; Hubbard T.D.
发表日期	2016
ISSN	19940416
卷号	10 期号:3
英文摘要	Frozen debris lobes (FDLs) are elongated, lobate permafrost features that mostly move through shear in zones near their bases. We present a comprehensive overview of eight FDLs within the Dalton Highway corridor (southern Brooks Range, Alaska), including their catchment geology and rock strengths, lobe soil characteristics, surface movement measurements collected between 2012 and 2015, and analysis of historic and modern imagery from 1955 to 2014. Field mapping and rock strength data indicate that the metasedimentary and metavolcanic bedrock forming the majority of the lobe catchments has very low to medium strength and is heavily fractured, thus easily contributing to FDL formation. The eight investigated FDLs consist of platy rocks typical of their catchments, organic debris, and an ice-poor soil matrix; massive ice, however, is present within FDLs as infiltration ice, concentrated within cracks open to the surface. Exposure of infiltration ice in retrogressive thaw slumps (RTSs) and associated debris flows leads to increased movement and various stages of destabilization, resulting in morphological differences among the lobes. Analysis of historic imagery indicates that movement of the eight investigated FDLs has been asynchronous over the study period, and since 1955, there has been an overall increase in movement rates of the investigated FDLs. The formation of surface features, such as cracks, scarps, and RTSs, suggests that the increased movement rates correlate to general instability, and even at their current distances, FDLs are impacting infrastructure through increased sediment mobilization. FDL-A is the largest of the investigated FDLs. As of August 2015, FDL-A was 39.2 m from the toe of the Dalton Highway embankment. Based on its current distance and rate of movement, we predict that FDL-A will reach the Dalton Highway alignment by 2023. © 2016 Author(s).
学科领域	bedrock; catchment; embankment; geological mapping; geomorphology; glacial debris; glacier dynamics; ice movement; image analysis; measurement method; metasedimentary rock; metavolcanic rock; permafrost; road; shear band; slumping; soil property; Alaska; Brooks Range; United States
语种	英语
scopus关键词	bedrock; catchment; embankment; geological mapping; geomorphology; glacial debris; glacier dynamics; ice movement; image analysis; measurement method; metasedimentary rock; metavolcanic rock; permafrost; road; shear band; slumping; soil property; Alaska; Brooks Range; United States
来源期刊	Cryosphere
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/119650
作者单位	Department of Mining and Geological Engineering, University of Alaska Fairbanks, Fairbanks, AK 99775, United States; Alaska Division of Geological, Geophysical Surveys, Fairbanks, AK 99709, United States
推荐引用方式 GB/T 7714	Darrow M.M.,Gyswyt N.L.,Simpson J.M.,et al. Frozen debris lobe morphology and movement: An overview of eight dynamic features, southern Brooks Range, Alaska[J],2016,10(3).
APA	Darrow M.M.,Gyswyt N.L.,Simpson J.M.,Daanen R.P.,&Hubbard T.D..(2016).Frozen debris lobe morphology and movement: An overview of eight dynamic features, southern Brooks Range, Alaska.Cryosphere,10(3).
MLA	Darrow M.M.,et al."Frozen debris lobe morphology and movement: An overview of eight dynamic features, southern Brooks Range, Alaska".Cryosphere 10.3(2016).