Quantifying landscape change in an arctic coastal lowland using repeat airborne LiDAR

Increases in air, permafrost, and sea surface temperature, loss of sea ice, the potential for increased wave energy, and higher river discharge may all be interacting to escalate erosion of arctic coastal lowland landscapes. Here we use airborne light detection and ranging (LiDAR) data acquired in 2...

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Published in:Environmental Research Letters
Main Authors: Benjamin M Jones, Jason M Stoker, Ann E Gibbs, Guido Grosse, Vladimir E Romanovsky, Thomas A Douglas, Nicole E M Kinsman, Bruce M Richmond
Format: Article in Journal/Newspaper
Language:English
Published: IOP Publishing 2013
Subjects:
Q
Ice
Online Access:https://doi.org/10.1088/1748-9326/8/4/045025
https://doaj.org/article/4e388589586d41bc91a945ed39ee6ba4
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spelling ftdoajarticles:oai:doaj.org/article:4e388589586d41bc91a945ed39ee6ba4 2023-09-05T13:16:53+02:00 Quantifying landscape change in an arctic coastal lowland using repeat airborne LiDAR Benjamin M Jones Jason M Stoker Ann E Gibbs Guido Grosse Vladimir E Romanovsky Thomas A Douglas Nicole E M Kinsman Bruce M Richmond 2013-01-01T00:00:00Z https://doi.org/10.1088/1748-9326/8/4/045025 https://doaj.org/article/4e388589586d41bc91a945ed39ee6ba4 EN eng IOP Publishing https://doi.org/10.1088/1748-9326/8/4/045025 https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/8/4/045025 1748-9326 https://doaj.org/article/4e388589586d41bc91a945ed39ee6ba4 Environmental Research Letters, Vol 8, Iss 4, p 045025 (2013) Arctic coasts LiDAR permafrost thermokarst Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 article 2013 ftdoajarticles https://doi.org/10.1088/1748-9326/8/4/045025 2023-08-13T00:37:31Z Increases in air, permafrost, and sea surface temperature, loss of sea ice, the potential for increased wave energy, and higher river discharge may all be interacting to escalate erosion of arctic coastal lowland landscapes. Here we use airborne light detection and ranging (LiDAR) data acquired in 2006 and 2010 to detect landscape change in a 100 km ^2 study area on the Beaufort Sea coastal plain of northern Alaska. We detected statistically significant change (99% confidence interval), defined as contiguous areas (>10 m ^2 ) that had changed in height by at least 0.55 m, in 0.3% of the study region. Erosional features indicative of ice-rich permafrost degradation were associated with ice-bonded coastal, river, and lake bluffs, frost mounds, ice wedges, and thermo-erosional gullies. These features accounted for about half of the area where vertical change was detected. Inferred thermo-denudation and thermo-abrasion of coastal and river bluffs likely accounted for the dominant permafrost-related degradational processes with respect to area (42%) and volume (51%). More than 300 thermokarst pits significantly subsided during the study period, likely as a result of storm surge flooding of low-lying tundra (<1.4 m asl) as well as the lasting impact of warm summers in the late-1980s and mid-1990s. Our results indicate that repeat airborne LiDAR can be used to detect landscape change in arctic coastal lowland regions at large spatial scales over sub-decadal time periods. Article in Journal/Newspaper Arctic Beaufort Sea Ice permafrost Sea ice Thermokarst Tundra wedge* Alaska Directory of Open Access Journals: DOAJ Articles Arctic Environmental Research Letters 8 4 045025
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Arctic
coasts
LiDAR
permafrost
thermokarst
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
spellingShingle Arctic
coasts
LiDAR
permafrost
thermokarst
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
Benjamin M Jones
Jason M Stoker
Ann E Gibbs
Guido Grosse
Vladimir E Romanovsky
Thomas A Douglas
Nicole E M Kinsman
Bruce M Richmond
Quantifying landscape change in an arctic coastal lowland using repeat airborne LiDAR
topic_facet Arctic
coasts
LiDAR
permafrost
thermokarst
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
description Increases in air, permafrost, and sea surface temperature, loss of sea ice, the potential for increased wave energy, and higher river discharge may all be interacting to escalate erosion of arctic coastal lowland landscapes. Here we use airborne light detection and ranging (LiDAR) data acquired in 2006 and 2010 to detect landscape change in a 100 km ^2 study area on the Beaufort Sea coastal plain of northern Alaska. We detected statistically significant change (99% confidence interval), defined as contiguous areas (>10 m ^2 ) that had changed in height by at least 0.55 m, in 0.3% of the study region. Erosional features indicative of ice-rich permafrost degradation were associated with ice-bonded coastal, river, and lake bluffs, frost mounds, ice wedges, and thermo-erosional gullies. These features accounted for about half of the area where vertical change was detected. Inferred thermo-denudation and thermo-abrasion of coastal and river bluffs likely accounted for the dominant permafrost-related degradational processes with respect to area (42%) and volume (51%). More than 300 thermokarst pits significantly subsided during the study period, likely as a result of storm surge flooding of low-lying tundra (<1.4 m asl) as well as the lasting impact of warm summers in the late-1980s and mid-1990s. Our results indicate that repeat airborne LiDAR can be used to detect landscape change in arctic coastal lowland regions at large spatial scales over sub-decadal time periods.
format Article in Journal/Newspaper
author Benjamin M Jones
Jason M Stoker
Ann E Gibbs
Guido Grosse
Vladimir E Romanovsky
Thomas A Douglas
Nicole E M Kinsman
Bruce M Richmond
author_facet Benjamin M Jones
Jason M Stoker
Ann E Gibbs
Guido Grosse
Vladimir E Romanovsky
Thomas A Douglas
Nicole E M Kinsman
Bruce M Richmond
author_sort Benjamin M Jones
title Quantifying landscape change in an arctic coastal lowland using repeat airborne LiDAR
title_short Quantifying landscape change in an arctic coastal lowland using repeat airborne LiDAR
title_full Quantifying landscape change in an arctic coastal lowland using repeat airborne LiDAR
title_fullStr Quantifying landscape change in an arctic coastal lowland using repeat airborne LiDAR
title_full_unstemmed Quantifying landscape change in an arctic coastal lowland using repeat airborne LiDAR
title_sort quantifying landscape change in an arctic coastal lowland using repeat airborne lidar
publisher IOP Publishing
publishDate 2013
url https://doi.org/10.1088/1748-9326/8/4/045025
https://doaj.org/article/4e388589586d41bc91a945ed39ee6ba4
geographic Arctic
geographic_facet Arctic
genre Arctic
Beaufort Sea
Ice
permafrost
Sea ice
Thermokarst
Tundra
wedge*
Alaska
genre_facet Arctic
Beaufort Sea
Ice
permafrost
Sea ice
Thermokarst
Tundra
wedge*
Alaska
op_source Environmental Research Letters, Vol 8, Iss 4, p 045025 (2013)
op_relation https://doi.org/10.1088/1748-9326/8/4/045025
https://doaj.org/toc/1748-9326
doi:10.1088/1748-9326/8/4/045025
1748-9326
https://doaj.org/article/4e388589586d41bc91a945ed39ee6ba4
op_doi https://doi.org/10.1088/1748-9326/8/4/045025
container_title Environmental Research Letters
container_volume 8
container_issue 4
container_start_page 045025
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