Observational Evidence of the Ice-Albedo Feedback and Its Intensification Between SSTs and the Arctic Sea Ice Since 2001
Currently, modeling studies of the significance of the ice-albedo feedback process have been inconclusive. Sea surface temperatures (SSTs) in the Arctic Ocean regions of the Chukchi/Beaufort, Laptev/East Siberian and Kara/Barents Seas have been increasing since the early 1980's, with larger inc...
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ftnasantrs:oai:casi.ntrs.nasa.gov:20120011992 2023-05-15T13:10:49+02:00 Observational Evidence of the Ice-Albedo Feedback and Its Intensification Between SSTs and the Arctic Sea Ice Since 2001 Boisvert, Linette N. Markus, Thorsten Unclassified, Unlimited, Publicly available [2012] http://ntrs.nasa.gov/search.jsp?R=20120011992 unknown http://ntrs.nasa.gov/search.jsp?R=20120011992 Copyright, Distribution as joint owner in the copyright CASI 47 GSFC.JA.00347.2012 2012 ftnasantrs 2012-08-04T23:18:36Z Currently, modeling studies of the significance of the ice-albedo feedback process have been inconclusive. Sea surface temperatures (SSTs) in the Arctic Ocean regions of the Chukchi/Beaufort, Laptev/East Siberian and Kara/Barents Seas have been increasing since the early 1980's, with larger increases since the early 2000's. Since the early 2000's the minimum ice extent has been decreasing more rapidly, melt onset has become earlier in the spring and freeze onset has become later in the fall. Sea ice thickness has also been decreasing since the 1980 s. Due to these large changes seen, is the ice-albedo feedback playing larger roll in the maintenance of the ice pack? If so, what has caused this feedback to become the dominant factor? We used SST data from AVHRR along with ice concentrations from SMMR and SSM/I, ice thickness from ICEsat, and melt and freeze onset data to explore this relationship further. While the ice-albedo feedback has always had an effect on the ice pack, since 2001 this feedback began to control when the ice pack refroze in the fall. A later freeze up made the ice pack thinner and more vulnerable in the following spring. The reason for this intensification was found out to be due to a shift to a thin, first-year ice pack that made up 60% of the ice in these three regions. Other/Unknown Material albedo Arctic Arctic Ocean Chukchi ice pack laptev Sea ice NASA Technical Reports Server (NTRS) Arctic Arctic Ocean |
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NASA Technical Reports Server (NTRS) |
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47 Boisvert, Linette N. Markus, Thorsten Observational Evidence of the Ice-Albedo Feedback and Its Intensification Between SSTs and the Arctic Sea Ice Since 2001 |
topic_facet |
47 |
description |
Currently, modeling studies of the significance of the ice-albedo feedback process have been inconclusive. Sea surface temperatures (SSTs) in the Arctic Ocean regions of the Chukchi/Beaufort, Laptev/East Siberian and Kara/Barents Seas have been increasing since the early 1980's, with larger increases since the early 2000's. Since the early 2000's the minimum ice extent has been decreasing more rapidly, melt onset has become earlier in the spring and freeze onset has become later in the fall. Sea ice thickness has also been decreasing since the 1980 s. Due to these large changes seen, is the ice-albedo feedback playing larger roll in the maintenance of the ice pack? If so, what has caused this feedback to become the dominant factor? We used SST data from AVHRR along with ice concentrations from SMMR and SSM/I, ice thickness from ICEsat, and melt and freeze onset data to explore this relationship further. While the ice-albedo feedback has always had an effect on the ice pack, since 2001 this feedback began to control when the ice pack refroze in the fall. A later freeze up made the ice pack thinner and more vulnerable in the following spring. The reason for this intensification was found out to be due to a shift to a thin, first-year ice pack that made up 60% of the ice in these three regions. |
format |
Other/Unknown Material |
author |
Boisvert, Linette N. Markus, Thorsten |
author_facet |
Boisvert, Linette N. Markus, Thorsten |
author_sort |
Boisvert, Linette N. |
title |
Observational Evidence of the Ice-Albedo Feedback and Its Intensification Between SSTs and the Arctic Sea Ice Since 2001 |
title_short |
Observational Evidence of the Ice-Albedo Feedback and Its Intensification Between SSTs and the Arctic Sea Ice Since 2001 |
title_full |
Observational Evidence of the Ice-Albedo Feedback and Its Intensification Between SSTs and the Arctic Sea Ice Since 2001 |
title_fullStr |
Observational Evidence of the Ice-Albedo Feedback and Its Intensification Between SSTs and the Arctic Sea Ice Since 2001 |
title_full_unstemmed |
Observational Evidence of the Ice-Albedo Feedback and Its Intensification Between SSTs and the Arctic Sea Ice Since 2001 |
title_sort |
observational evidence of the ice-albedo feedback and its intensification between ssts and the arctic sea ice since 2001 |
publishDate |
2012 |
url |
http://ntrs.nasa.gov/search.jsp?R=20120011992 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
albedo Arctic Arctic Ocean Chukchi ice pack laptev Sea ice |
genre_facet |
albedo Arctic Arctic Ocean Chukchi ice pack laptev Sea ice |
op_source |
CASI |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=20120011992 |
op_rights |
Copyright, Distribution as joint owner in the copyright |
_version_ |
1766243788064292864 |