Assimilation of ice motion observations and comparisons with submarine ice thickness data
[1] Aided by submarine observations of ice thickness for model evaluation, we investigate the effects of assimilating buoy motion data and satellite SSM/I (85 Ghz) ice motion data on simulation of Arctic sea ice. The sea-ice model is a thickness and enthalpy distribution model and is coupled to an o...
Main Authors: | , , , , , |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.645.1468 http://psc.apl.washington.edu/zhang/Pubs/Zhang_assimilationIceMotion.pdf |
id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.645.1468 |
---|---|
record_format |
openpolar |
spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.645.1468 2023-05-15T14:57:49+02:00 Assimilation of ice motion observations and comparisons with submarine ice thickness data Jinlun Zhang D. R. Thomas D. A. Rothrock R. W. Lindsay Y. Yu R. Kwok The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.645.1468 http://psc.apl.washington.edu/zhang/Pubs/Zhang_assimilationIceMotion.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.645.1468 http://psc.apl.washington.edu/zhang/Pubs/Zhang_assimilationIceMotion.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://psc.apl.washington.edu/zhang/Pubs/Zhang_assimilationIceMotion.pdf text ftciteseerx 2016-01-08T16:08:14Z [1] Aided by submarine observations of ice thickness for model evaluation, we investigate the effects of assimilating buoy motion data and satellite SSM/I (85 Ghz) ice motion data on simulation of Arctic sea ice. The sea-ice model is a thickness and enthalpy distribution model and is coupled to an ocean model. Ice motion data are assimilated by means of optimal interpolation. Assimilating motion data, particularly from drifting buoys, significantly improves the modeled ice motion, reducing the error to 0.04 m s1 from 0.07 m s1 and increasing the correlation with observations to 0.90 from 0.66. Without data assimilation, the modeled ice moves too slowly with excessive stoppage. Assimilation leads to more robust ice motion with substantially reduced stoppage, which in turn leads to strengthened ice outflow at Fram Strait and enhanced ice deformation everywhere. Enhanced deformation doubles the production of ridged ice to an Arctic Ocean average of 0.77 m yr1, and raises the amount of ridged ice to half the total ice volume per unit area of 2.58 m. Assimilation also significantly alters the spatial distribution of ice mass and brings the modeled ice thickness into better agreement with the thickness observed in four recent submarine cruises, reducing the error to 0.66 m from Text Arctic Arctic Ocean Fram Strait Sea ice Unknown Arctic Arctic Ocean |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
[1] Aided by submarine observations of ice thickness for model evaluation, we investigate the effects of assimilating buoy motion data and satellite SSM/I (85 Ghz) ice motion data on simulation of Arctic sea ice. The sea-ice model is a thickness and enthalpy distribution model and is coupled to an ocean model. Ice motion data are assimilated by means of optimal interpolation. Assimilating motion data, particularly from drifting buoys, significantly improves the modeled ice motion, reducing the error to 0.04 m s1 from 0.07 m s1 and increasing the correlation with observations to 0.90 from 0.66. Without data assimilation, the modeled ice moves too slowly with excessive stoppage. Assimilation leads to more robust ice motion with substantially reduced stoppage, which in turn leads to strengthened ice outflow at Fram Strait and enhanced ice deformation everywhere. Enhanced deformation doubles the production of ridged ice to an Arctic Ocean average of 0.77 m yr1, and raises the amount of ridged ice to half the total ice volume per unit area of 2.58 m. Assimilation also significantly alters the spatial distribution of ice mass and brings the modeled ice thickness into better agreement with the thickness observed in four recent submarine cruises, reducing the error to 0.66 m from |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Jinlun Zhang D. R. Thomas D. A. Rothrock R. W. Lindsay Y. Yu R. Kwok |
spellingShingle |
Jinlun Zhang D. R. Thomas D. A. Rothrock R. W. Lindsay Y. Yu R. Kwok Assimilation of ice motion observations and comparisons with submarine ice thickness data |
author_facet |
Jinlun Zhang D. R. Thomas D. A. Rothrock R. W. Lindsay Y. Yu R. Kwok |
author_sort |
Jinlun Zhang |
title |
Assimilation of ice motion observations and comparisons with submarine ice thickness data |
title_short |
Assimilation of ice motion observations and comparisons with submarine ice thickness data |
title_full |
Assimilation of ice motion observations and comparisons with submarine ice thickness data |
title_fullStr |
Assimilation of ice motion observations and comparisons with submarine ice thickness data |
title_full_unstemmed |
Assimilation of ice motion observations and comparisons with submarine ice thickness data |
title_sort |
assimilation of ice motion observations and comparisons with submarine ice thickness data |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.645.1468 http://psc.apl.washington.edu/zhang/Pubs/Zhang_assimilationIceMotion.pdf |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Fram Strait Sea ice |
genre_facet |
Arctic Arctic Ocean Fram Strait Sea ice |
op_source |
http://psc.apl.washington.edu/zhang/Pubs/Zhang_assimilationIceMotion.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.645.1468 http://psc.apl.washington.edu/zhang/Pubs/Zhang_assimilationIceMotion.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766329929743466496 |