1950–2002 remotely sensed images

[1] Over the past 50 years, Alaska has experienced a warming climate with longer growing seasons, increased potential evapotranspiration, and permafrost warming. Research from the Seward Peninsula and Kenai Peninsula has demonstrated a substantial landscape-level trend in the reduction of surface wa...

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Main Authors: Brian Riordan, David Verbyla, A. David Mcguire
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.8545
http://www.lter.uaf.edu/pdf/1055_Riordan_Verbyla.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.419.8545 2023-05-15T15:00:28+02:00 1950–2002 remotely sensed images Brian Riordan David Verbyla A. David Mcguire The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.8545 http://www.lter.uaf.edu/pdf/1055_Riordan_Verbyla.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.8545 http://www.lter.uaf.edu/pdf/1055_Riordan_Verbyla.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.lter.uaf.edu/pdf/1055_Riordan_Verbyla.pdf text ftciteseerx 2016-01-08T03:54:19Z [1] Over the past 50 years, Alaska has experienced a warming climate with longer growing seasons, increased potential evapotranspiration, and permafrost warming. Research from the Seward Peninsula and Kenai Peninsula has demonstrated a substantial landscape-level trend in the reduction of surface water and number of closed-basin ponds. We investigated whether this drying trend occurred at nine other regions throughout Alaska. One study region was from the Arctic Coastal Plain where deep permafrost occurs continuously across the landscape. The other eight study regions were from the boreal forest regions where discontinuous permafrost occurs. Mean annual precipitation across the study regions ranged from 100 to over 700 mm yr 1. We used remotely sensed imagery from the 1950s to 2002 to inventory over 10,000 closed-basin ponds from at least three periods from this time span. We found a reduction in the area and number of shallow, closed-basin ponds for all boreal regions. In contrast, the Arctic Coastal Plain region had negligible change in the area of closed-basin ponds. Since the 1950s, surface water area of closed-basin ponds included in this analysis decreased by 31 to 4 percent, and the total number of closed-basin ponds surveyed within each study region decreased from 54 to 5 percent. There was a significant increasing trend in annual mean temperature and potential evapotranspiration since the 1950s for all study regions. There was no significant trend in annual precipitation during the same period. The regional trend of shrinking ponds may be due to increased drainage as permafrost warms, or increased evapotranspiration during a warmer and extended growing season. Citation: Riordan, B., D. Verbyla, and A. D. McGuire (2006), Shrinking ponds in subarctic Alaska based on 1950–2002 remotely Text Arctic permafrost Seward Peninsula Subarctic Alaska Unknown Arctic
institution Open Polar
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language English
description [1] Over the past 50 years, Alaska has experienced a warming climate with longer growing seasons, increased potential evapotranspiration, and permafrost warming. Research from the Seward Peninsula and Kenai Peninsula has demonstrated a substantial landscape-level trend in the reduction of surface water and number of closed-basin ponds. We investigated whether this drying trend occurred at nine other regions throughout Alaska. One study region was from the Arctic Coastal Plain where deep permafrost occurs continuously across the landscape. The other eight study regions were from the boreal forest regions where discontinuous permafrost occurs. Mean annual precipitation across the study regions ranged from 100 to over 700 mm yr 1. We used remotely sensed imagery from the 1950s to 2002 to inventory over 10,000 closed-basin ponds from at least three periods from this time span. We found a reduction in the area and number of shallow, closed-basin ponds for all boreal regions. In contrast, the Arctic Coastal Plain region had negligible change in the area of closed-basin ponds. Since the 1950s, surface water area of closed-basin ponds included in this analysis decreased by 31 to 4 percent, and the total number of closed-basin ponds surveyed within each study region decreased from 54 to 5 percent. There was a significant increasing trend in annual mean temperature and potential evapotranspiration since the 1950s for all study regions. There was no significant trend in annual precipitation during the same period. The regional trend of shrinking ponds may be due to increased drainage as permafrost warms, or increased evapotranspiration during a warmer and extended growing season. Citation: Riordan, B., D. Verbyla, and A. D. McGuire (2006), Shrinking ponds in subarctic Alaska based on 1950–2002 remotely
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Brian Riordan
David Verbyla
A. David Mcguire
spellingShingle Brian Riordan
David Verbyla
A. David Mcguire
1950–2002 remotely sensed images
author_facet Brian Riordan
David Verbyla
A. David Mcguire
author_sort Brian Riordan
title 1950–2002 remotely sensed images
title_short 1950–2002 remotely sensed images
title_full 1950–2002 remotely sensed images
title_fullStr 1950–2002 remotely sensed images
title_full_unstemmed 1950–2002 remotely sensed images
title_sort 1950–2002 remotely sensed images
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.8545
http://www.lter.uaf.edu/pdf/1055_Riordan_Verbyla.pdf
geographic Arctic
geographic_facet Arctic
genre Arctic
permafrost
Seward Peninsula
Subarctic
Alaska
genre_facet Arctic
permafrost
Seward Peninsula
Subarctic
Alaska
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http://www.lter.uaf.edu/pdf/1055_Riordan_Verbyla.pdf
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