Highlights

In 2011, new record high temperatures at 20 m depth were recorded at all permafrost observatories on the North Slope of Alaska, where measurements began in the late 1970s. During the last fifteen years, active-layer thickness has increased in the Russian European North, northern East Siberia, Chukot...

Full description

Bibliographic Details
Main Authors: V. E. Romanovsky, S. L. Smith, H. H. Christiansen, N. I. Shiklomanov, D. S. Drozdov, N. G. Oberman, A. L. Kholodov, S. S. Marchenko
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2011
Subjects:
Ice
IPY
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.6988
http://www.lter.uaf.edu/pdf/1648_Romanovsky_Smith_2011.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.419.6988
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.419.6988 2023-05-15T13:02:53+02:00 Highlights V. E. Romanovsky S. L. Smith H. H. Christiansen N. I. Shiklomanov D. S. Drozdov N. G. Oberman A. L. Kholodov S. S. Marchenko The Pennsylvania State University CiteSeerX Archives 2011 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.6988 http://www.lter.uaf.edu/pdf/1648_Romanovsky_Smith_2011.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.6988 http://www.lter.uaf.edu/pdf/1648_Romanovsky_Smith_2011.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.lter.uaf.edu/pdf/1648_Romanovsky_Smith_2011.pdf text 2011 ftciteseerx 2016-01-08T03:53:44Z In 2011, new record high temperatures at 20 m depth were recorded at all permafrost observatories on the North Slope of Alaska, where measurements began in the late 1970s. During the last fifteen years, active-layer thickness has increased in the Russian European North, northern East Siberia, Chukotka, Svalbard and Greenland. Active-layer thickness on the Alaskan North Slope and in the western Canadian Arctic was relatively stable during 1995-2008. The most direct indicators of permafrost stability and changes in permafrost state are the permafrost temperature and the active layer thickness (ALT). Permafrost temperature measured at the depth where the seasonal variations in ground temperature cease to exist is best to use as an indicator of long-term change. This depth varies from a few meters in warm, ice-rich permafrost to 20 m and more in cold permafrost and in bedrock (Smith et al. 2010; Romanovsky et al. 2010a). However, if continuous year-around temperature measurements are available, the mean annual ground temperature (MAGT) at any depth within the upper 15 m can be used as a proxy of the permafrost temperature. The recently concluded International Polar Year (IPY 2007-2009) resulted in significant enhancement of the permafrost observing system in the Arctic; there are now ~575 boreholes (Fig. HTC23; Brown et al. 2010; Romanovsky et al. 2010a). A borehole inventory, including mean annual ground temperatures for most of these boreholes, is available online Text Active layer thickness Arctic Chukotka Greenland Ice International Polar Year IPY north slope permafrost Svalbard Alaska Siberia Unknown Arctic Greenland Svalbard
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description In 2011, new record high temperatures at 20 m depth were recorded at all permafrost observatories on the North Slope of Alaska, where measurements began in the late 1970s. During the last fifteen years, active-layer thickness has increased in the Russian European North, northern East Siberia, Chukotka, Svalbard and Greenland. Active-layer thickness on the Alaskan North Slope and in the western Canadian Arctic was relatively stable during 1995-2008. The most direct indicators of permafrost stability and changes in permafrost state are the permafrost temperature and the active layer thickness (ALT). Permafrost temperature measured at the depth where the seasonal variations in ground temperature cease to exist is best to use as an indicator of long-term change. This depth varies from a few meters in warm, ice-rich permafrost to 20 m and more in cold permafrost and in bedrock (Smith et al. 2010; Romanovsky et al. 2010a). However, if continuous year-around temperature measurements are available, the mean annual ground temperature (MAGT) at any depth within the upper 15 m can be used as a proxy of the permafrost temperature. The recently concluded International Polar Year (IPY 2007-2009) resulted in significant enhancement of the permafrost observing system in the Arctic; there are now ~575 boreholes (Fig. HTC23; Brown et al. 2010; Romanovsky et al. 2010a). A borehole inventory, including mean annual ground temperatures for most of these boreholes, is available online
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author V. E. Romanovsky
S. L. Smith
H. H. Christiansen
N. I. Shiklomanov
D. S. Drozdov
N. G. Oberman
A. L. Kholodov
S. S. Marchenko
spellingShingle V. E. Romanovsky
S. L. Smith
H. H. Christiansen
N. I. Shiklomanov
D. S. Drozdov
N. G. Oberman
A. L. Kholodov
S. S. Marchenko
Highlights
author_facet V. E. Romanovsky
S. L. Smith
H. H. Christiansen
N. I. Shiklomanov
D. S. Drozdov
N. G. Oberman
A. L. Kholodov
S. S. Marchenko
author_sort V. E. Romanovsky
title Highlights
title_short Highlights
title_full Highlights
title_fullStr Highlights
title_full_unstemmed Highlights
title_sort highlights
publishDate 2011
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.6988
http://www.lter.uaf.edu/pdf/1648_Romanovsky_Smith_2011.pdf
geographic Arctic
Greenland
Svalbard
geographic_facet Arctic
Greenland
Svalbard
genre Active layer thickness
Arctic
Chukotka
Greenland
Ice
International Polar Year
IPY
north slope
permafrost
Svalbard
Alaska
Siberia
genre_facet Active layer thickness
Arctic
Chukotka
Greenland
Ice
International Polar Year
IPY
north slope
permafrost
Svalbard
Alaska
Siberia
op_source http://www.lter.uaf.edu/pdf/1648_Romanovsky_Smith_2011.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.6988
http://www.lter.uaf.edu/pdf/1648_Romanovsky_Smith_2011.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766323280041476096