Establishing long‐term permafrost observatories for active‐layer and permafrost investigations in Alaska: 1977–2002

Abstract Twenty‐five years ago a programme was initiated to establish a statewide system of permafrost observatories that included boreholes drilled for the express purpose of investigating the effects of changes in climate on continuous and discontinuous permafrost. A total of 22 permafrost observa...

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Published in:Permafrost and Periglacial Processes
Main Author: Osterkamp, T. E.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2003
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.464
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.464
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spelling crwiley:10.1002/ppp.464 2024-09-09T20:02:44+00:00 Establishing long‐term permafrost observatories for active‐layer and permafrost investigations in Alaska: 1977–2002 Osterkamp, T. E. 2003 http://dx.doi.org/10.1002/ppp.464 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.464 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.464 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 14, issue 4, page 331-342 ISSN 1045-6740 1099-1530 journal-article 2003 crwiley https://doi.org/10.1002/ppp.464 2024-08-13T04:16:27Z Abstract Twenty‐five years ago a programme was initiated to establish a statewide system of permafrost observatories that included boreholes drilled for the express purpose of investigating the effects of changes in climate on continuous and discontinuous permafrost. A total of 22 permafrost observatories have been established with boreholes 15 to 80 m in depth. These sites are primarily along a north‐south transect of Alaska paralleling the Alyeska oil pipeline from Prudhoe Bay to Glennallen and are visited and serviced annually. There are seven additional borehole sites with holes 15 to 80 m in depth that are visited occasionally. The sites are in undisturbed locations with nearly uniform conditions in a wide variety of environmental settings except for a few, purposefully placed in disturbed areas (e.g. farm field, burn, etc.). Proximity to meteorological stations with long weather records has allowed reconstruction of past active‐layer and permafrost conditions using calibrated site‐specific models. The sites have been used to document a recent warming trend in permafrost and active‐layer temperatures and to investigate the characteristics of the permafrost and active layer and processes that occur in them. Recommendations are made for establishing future observatories. Copyright © 2003 John Wiley & Sons, Ltd. Article in Journal/Newspaper permafrost Permafrost and Periglacial Processes Prudhoe Bay Alaska Wiley Online Library Permafrost and Periglacial Processes 14 4 331 342
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Twenty‐five years ago a programme was initiated to establish a statewide system of permafrost observatories that included boreholes drilled for the express purpose of investigating the effects of changes in climate on continuous and discontinuous permafrost. A total of 22 permafrost observatories have been established with boreholes 15 to 80 m in depth. These sites are primarily along a north‐south transect of Alaska paralleling the Alyeska oil pipeline from Prudhoe Bay to Glennallen and are visited and serviced annually. There are seven additional borehole sites with holes 15 to 80 m in depth that are visited occasionally. The sites are in undisturbed locations with nearly uniform conditions in a wide variety of environmental settings except for a few, purposefully placed in disturbed areas (e.g. farm field, burn, etc.). Proximity to meteorological stations with long weather records has allowed reconstruction of past active‐layer and permafrost conditions using calibrated site‐specific models. The sites have been used to document a recent warming trend in permafrost and active‐layer temperatures and to investigate the characteristics of the permafrost and active layer and processes that occur in them. Recommendations are made for establishing future observatories. Copyright © 2003 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Osterkamp, T. E.
spellingShingle Osterkamp, T. E.
Establishing long‐term permafrost observatories for active‐layer and permafrost investigations in Alaska: 1977–2002
author_facet Osterkamp, T. E.
author_sort Osterkamp, T. E.
title Establishing long‐term permafrost observatories for active‐layer and permafrost investigations in Alaska: 1977–2002
title_short Establishing long‐term permafrost observatories for active‐layer and permafrost investigations in Alaska: 1977–2002
title_full Establishing long‐term permafrost observatories for active‐layer and permafrost investigations in Alaska: 1977–2002
title_fullStr Establishing long‐term permafrost observatories for active‐layer and permafrost investigations in Alaska: 1977–2002
title_full_unstemmed Establishing long‐term permafrost observatories for active‐layer and permafrost investigations in Alaska: 1977–2002
title_sort establishing long‐term permafrost observatories for active‐layer and permafrost investigations in alaska: 1977–2002
publisher Wiley
publishDate 2003
url http://dx.doi.org/10.1002/ppp.464
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.464
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.464
genre permafrost
Permafrost and Periglacial Processes
Prudhoe Bay
Alaska
genre_facet permafrost
Permafrost and Periglacial Processes
Prudhoe Bay
Alaska
op_source Permafrost and Periglacial Processes
volume 14, issue 4, page 331-342
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.464
container_title Permafrost and Periglacial Processes
container_volume 14
container_issue 4
container_start_page 331
op_container_end_page 342
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