Seasonality and long-term trend of Arctic Ocean surface stress in a model
Abstract A numerical ocean sea-ice model is used to demonstrate that Arctic sea ice retreat affects momen-tum transfer into the ocean. A thinner and thus weaker ice cover is more easily forced by the wind, which increases the momentum flux. In contrast, increasing open water reduces momentum transfe...
Main Authors: | , , |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.649.352 http://psc.apl.washington.edu/zhang/Pubs/Martin_etal2014_jgrc20607.pdf |
id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.649.352 |
---|---|
record_format |
openpolar |
spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.649.352 2023-05-15T14:54:47+02:00 Seasonality and long-term trend of Arctic Ocean surface stress in a model Torge Martin Michael Steele Jinlun Zhang The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.649.352 http://psc.apl.washington.edu/zhang/Pubs/Martin_etal2014_jgrc20607.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.649.352 http://psc.apl.washington.edu/zhang/Pubs/Martin_etal2014_jgrc20607.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://psc.apl.washington.edu/zhang/Pubs/Martin_etal2014_jgrc20607.pdf text ftciteseerx 2016-01-08T16:17:01Z Abstract A numerical ocean sea-ice model is used to demonstrate that Arctic sea ice retreat affects momen-tum transfer into the ocean. A thinner and thus weaker ice cover is more easily forced by the wind, which increases the momentum flux. In contrast, increasing open water reduces momentum transfer because the ice surface provides greater drag than the open water surface. We introduce the concept of optimal ice concentra-tion: momentum transfer increases with increasing ice concentration up to a point, beyond which frictional losses by floe interaction damp the transfer. For a common ice internal stress formulation, a concentration of 80–90% yields optimal amplification of momentum flux into the ocean. We study the seasonality and long-term evolution of Arctic Ocean surface stress over the years 1979–2012. Spring and fall feature optimal ice conditions for momen-tum transfer, but only in fall is the wind forcing at its maximum, yielding a peak basin-mean ocean surface stress of0.08 N/m2. Since 1979, the basin-wide annual mean ocean surface stress has been increasing by 0.004 N/m2/ decade, and since 2000 by 0.006 N/m2/decade. In contrast, summertime ocean surface stress has been decreasing at20.002 N/m2/decade. These trends are linked to the weakening of the ice cover in fall, winter and spring, and to an increase in open water fraction in summer, i.e., changes in momentum transfer rather than changes in wind forcing. In most areas, the number of days per year with optimal ice concentration is decreasing. 1. Text Arctic Arctic Ocean Sea ice Unknown Arctic Arctic Ocean |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
Abstract A numerical ocean sea-ice model is used to demonstrate that Arctic sea ice retreat affects momen-tum transfer into the ocean. A thinner and thus weaker ice cover is more easily forced by the wind, which increases the momentum flux. In contrast, increasing open water reduces momentum transfer because the ice surface provides greater drag than the open water surface. We introduce the concept of optimal ice concentra-tion: momentum transfer increases with increasing ice concentration up to a point, beyond which frictional losses by floe interaction damp the transfer. For a common ice internal stress formulation, a concentration of 80–90% yields optimal amplification of momentum flux into the ocean. We study the seasonality and long-term evolution of Arctic Ocean surface stress over the years 1979–2012. Spring and fall feature optimal ice conditions for momen-tum transfer, but only in fall is the wind forcing at its maximum, yielding a peak basin-mean ocean surface stress of0.08 N/m2. Since 1979, the basin-wide annual mean ocean surface stress has been increasing by 0.004 N/m2/ decade, and since 2000 by 0.006 N/m2/decade. In contrast, summertime ocean surface stress has been decreasing at20.002 N/m2/decade. These trends are linked to the weakening of the ice cover in fall, winter and spring, and to an increase in open water fraction in summer, i.e., changes in momentum transfer rather than changes in wind forcing. In most areas, the number of days per year with optimal ice concentration is decreasing. 1. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Torge Martin Michael Steele Jinlun Zhang |
spellingShingle |
Torge Martin Michael Steele Jinlun Zhang Seasonality and long-term trend of Arctic Ocean surface stress in a model |
author_facet |
Torge Martin Michael Steele Jinlun Zhang |
author_sort |
Torge Martin |
title |
Seasonality and long-term trend of Arctic Ocean surface stress in a model |
title_short |
Seasonality and long-term trend of Arctic Ocean surface stress in a model |
title_full |
Seasonality and long-term trend of Arctic Ocean surface stress in a model |
title_fullStr |
Seasonality and long-term trend of Arctic Ocean surface stress in a model |
title_full_unstemmed |
Seasonality and long-term trend of Arctic Ocean surface stress in a model |
title_sort |
seasonality and long-term trend of arctic ocean surface stress in a model |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.649.352 http://psc.apl.washington.edu/zhang/Pubs/Martin_etal2014_jgrc20607.pdf |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Sea ice |
genre_facet |
Arctic Arctic Ocean Sea ice |
op_source |
http://psc.apl.washington.edu/zhang/Pubs/Martin_etal2014_jgrc20607.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.649.352 http://psc.apl.washington.edu/zhang/Pubs/Martin_etal2014_jgrc20607.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766326540025462784 |