Error Analysis of Real-Time Remotely Sensed Microwave Sea-Ice Motions in the Western Arctic Ocean
An algorithm used to composite SSM/I 85.5 GHz imagery and derive sea ice motion was adapted for operational testing at Fleet Numerical Meteorology and Oceanography Command (FNMOC). A feature tracking technique was applied to a 6-month period, with data provided by FNMOC and the Naval Research Labora...
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ftdtic:ADA386446 2023-05-15T14:57:49+02:00 Error Analysis of Real-Time Remotely Sensed Microwave Sea-Ice Motions in the Western Arctic Ocean Carsten, David M. NAVAL POSTGRADUATE SCHOOL MONTEREY CA 2000-09 text/html http://www.dtic.mil/docs/citations/ADA386446 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA386446 en eng http://www.dtic.mil/docs/citations/ADA386446 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Snow Ice and Permafrost Miscellaneous Detection and Detectors *REMOTE DETECTION *SEA ICE *MICROWAVE OPTICS ALGORITHMS REAL TIME THESES ERROR ANALYSIS SONOBUOYS OCEANOGRAPHY ARCTIC OCEAN IN SITU ANALYSIS *SSMI(SPECIAL SENSOR MICROWAVE IMAGERS) Text 2000 ftdtic 2016-02-20T06:55:30Z An algorithm used to composite SSM/I 85.5 GHz imagery and derive sea ice motion was adapted for operational testing at Fleet Numerical Meteorology and Oceanography Command (FNMOC). A feature tracking technique was applied to a 6-month period, with data provided by FNMOC and the Naval Research Laboratory (NRL). Ice motions are detectable using the SSM/I motion algorithm, and fields of SSM/I motion vectors are qualitatively consistent with coincident fields of in situ buoy motion vectors. Accuracy of the SSM/I motion vectors relative to buoy motion vectors increase significantly with buoy speed. No correlation between SSM/I and buoy motion vectors is observed for speeds below 3 cm/s and correlation increases significantly above 5 cm/s. The results are very sensitive to compositing techniques used to combine SSM/I passes into a single sea ice representation. FNMOC data was composited using a "drop-in-the-bucket" technique while NRL data was composited by a bilinear interpolation technique. Significantly poorer results were found with ENMOC composited data. Text Arctic Arctic Ocean Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean |
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Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography Snow Ice and Permafrost Miscellaneous Detection and Detectors *REMOTE DETECTION *SEA ICE *MICROWAVE OPTICS ALGORITHMS REAL TIME THESES ERROR ANALYSIS SONOBUOYS OCEANOGRAPHY ARCTIC OCEAN IN SITU ANALYSIS *SSMI(SPECIAL SENSOR MICROWAVE IMAGERS) |
spellingShingle |
Physical and Dynamic Oceanography Snow Ice and Permafrost Miscellaneous Detection and Detectors *REMOTE DETECTION *SEA ICE *MICROWAVE OPTICS ALGORITHMS REAL TIME THESES ERROR ANALYSIS SONOBUOYS OCEANOGRAPHY ARCTIC OCEAN IN SITU ANALYSIS *SSMI(SPECIAL SENSOR MICROWAVE IMAGERS) Carsten, David M. Error Analysis of Real-Time Remotely Sensed Microwave Sea-Ice Motions in the Western Arctic Ocean |
topic_facet |
Physical and Dynamic Oceanography Snow Ice and Permafrost Miscellaneous Detection and Detectors *REMOTE DETECTION *SEA ICE *MICROWAVE OPTICS ALGORITHMS REAL TIME THESES ERROR ANALYSIS SONOBUOYS OCEANOGRAPHY ARCTIC OCEAN IN SITU ANALYSIS *SSMI(SPECIAL SENSOR MICROWAVE IMAGERS) |
description |
An algorithm used to composite SSM/I 85.5 GHz imagery and derive sea ice motion was adapted for operational testing at Fleet Numerical Meteorology and Oceanography Command (FNMOC). A feature tracking technique was applied to a 6-month period, with data provided by FNMOC and the Naval Research Laboratory (NRL). Ice motions are detectable using the SSM/I motion algorithm, and fields of SSM/I motion vectors are qualitatively consistent with coincident fields of in situ buoy motion vectors. Accuracy of the SSM/I motion vectors relative to buoy motion vectors increase significantly with buoy speed. No correlation between SSM/I and buoy motion vectors is observed for speeds below 3 cm/s and correlation increases significantly above 5 cm/s. The results are very sensitive to compositing techniques used to combine SSM/I passes into a single sea ice representation. FNMOC data was composited using a "drop-in-the-bucket" technique while NRL data was composited by a bilinear interpolation technique. Significantly poorer results were found with ENMOC composited data. |
author2 |
NAVAL POSTGRADUATE SCHOOL MONTEREY CA |
format |
Text |
author |
Carsten, David M. |
author_facet |
Carsten, David M. |
author_sort |
Carsten, David M. |
title |
Error Analysis of Real-Time Remotely Sensed Microwave Sea-Ice Motions in the Western Arctic Ocean |
title_short |
Error Analysis of Real-Time Remotely Sensed Microwave Sea-Ice Motions in the Western Arctic Ocean |
title_full |
Error Analysis of Real-Time Remotely Sensed Microwave Sea-Ice Motions in the Western Arctic Ocean |
title_fullStr |
Error Analysis of Real-Time Remotely Sensed Microwave Sea-Ice Motions in the Western Arctic Ocean |
title_full_unstemmed |
Error Analysis of Real-Time Remotely Sensed Microwave Sea-Ice Motions in the Western Arctic Ocean |
title_sort |
error analysis of real-time remotely sensed microwave sea-ice motions in the western arctic ocean |
publishDate |
2000 |
url |
http://www.dtic.mil/docs/citations/ADA386446 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA386446 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Ice permafrost Sea ice |
genre_facet |
Arctic Arctic Ocean Ice permafrost Sea ice |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA386446 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766329926715179008 |