The Regional Polar Ice Prediction System - Barents Sea (RPIPS-B): A technical Description

The hydraulic/thermodynamic Artic sea-ice model is designed by W.D. Hibler of the Cold Regions Research and Engineering Laboratory (CREEL) has been adapted to the Barents Sea. This model is driven by atmospheric forcing from the Naval Operational Global Atmospheric Prediction System (NOGAPS) and oce...

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Main Authors: Preller, Ruth H., Riedlinger, Shelley, Posey, Pamela G.
Other Authors: NAVAL OCEAN RESEARCH AND DEVELOPMENT ACTIVITY STENNIS SPACE CENTER MS
Format: Text
Language:English
Published: 1989
Subjects:
ICE
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA213159
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA213159
id ftdtic:ADA213159
record_format openpolar
spelling ftdtic:ADA213159 2023-05-15T15:38:06+02:00 The Regional Polar Ice Prediction System - Barents Sea (RPIPS-B): A technical Description Preller, Ruth H. Riedlinger, Shelley Posey, Pamela G. NAVAL OCEAN RESEARCH AND DEVELOPMENT ACTIVITY STENNIS SPACE CENTER MS 1989-05 text/html http://www.dtic.mil/docs/citations/ADA213159 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA213159 en eng http://www.dtic.mil/docs/citations/ADA213159 Approved for public release; distribution is unlimited. DTIC AND NTIS Physical and Dynamic Oceanography Snow Ice and Permafrost *COMPUTERIZED SIMULATION *SEA ICE *FORECASTING *COMPUTER PROGRAMS ACCURACY MELTS COLD REGIONS KARA SEA HIGH RESOLUTION BOUNDARIES ICE CONCENTRATION(COMPOSITION) BARENTS SEA SUMMER LAND AREAS CHECKOUT PROCEDURES PASSIVE SYSTEMS GROWTH(GENERAL) EDGES MODELS MICROWAVES PE63207N WUDN894428 Text 1989 ftdtic 2016-02-23T04:32:31Z The hydraulic/thermodynamic Artic sea-ice model is designed by W.D. Hibler of the Cold Regions Research and Engineering Laboratory (CREEL) has been adapted to the Barents Sea. This model is driven by atmospheric forcing from the Naval Operational Global Atmospheric Prediction System (NOGAPS) and oceanic forcing from the Hibler and Bryan coupled ice-ocean model. This high-resolution model (25 km), which covers the entire Barents Sea and the western half of the Kara Sea, uses a 6-hour time step. Model results show good agreement with such data as the Naval Polar Oceanography Center's (NPOC) analysis of ice concentration and concentrations derived from passive microwave data. The model has a tendency, however, to melt ice too quickly in summer and to grow it back too slowly in the fall. Planned improvements in the atmospheric and oceanic forcing should correct this problem. The high resolution of the Barents Sea model enables it to predict the ice edge, ice growth and decay, and the movement of ice near land boundaries with greater accuracy than does the PIPS model. The Regional Polar Ice Prediction System for the Barents Sea (RPIPS-B) is the forecast system designed to run at the Fleet Numerical Oceanography Center (FNOC) based on the Barents Sea Ice model. RPIPS-B is updated weekly by the NPOC analysis of ice concentration. The forecast system, presently in its 'operational checkout' phase, is being made ready for a winter-spring operational test. Keywords: Computer simulation; Computer programs. Text Barents Sea Cold Regions Research and Engineering Laboratory Ice Kara Sea permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Barents Sea Kara Sea
institution 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
*COMPUTERIZED SIMULATION
*SEA ICE
*FORECASTING
*COMPUTER PROGRAMS
ACCURACY
MELTS
COLD REGIONS
KARA SEA
HIGH RESOLUTION
BOUNDARIES
ICE
CONCENTRATION(COMPOSITION)
BARENTS SEA
SUMMER
LAND AREAS
CHECKOUT PROCEDURES
PASSIVE SYSTEMS
GROWTH(GENERAL)
EDGES
MODELS
MICROWAVES
PE63207N
WUDN894428
spellingShingle Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*COMPUTERIZED SIMULATION
*SEA ICE
*FORECASTING
*COMPUTER PROGRAMS
ACCURACY
MELTS
COLD REGIONS
KARA SEA
HIGH RESOLUTION
BOUNDARIES
ICE
CONCENTRATION(COMPOSITION)
BARENTS SEA
SUMMER
LAND AREAS
CHECKOUT PROCEDURES
PASSIVE SYSTEMS
GROWTH(GENERAL)
EDGES
MODELS
MICROWAVES
PE63207N
WUDN894428
Preller, Ruth H.
Riedlinger, Shelley
Posey, Pamela G.
The Regional Polar Ice Prediction System - Barents Sea (RPIPS-B): A technical Description
topic_facet Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*COMPUTERIZED SIMULATION
*SEA ICE
*FORECASTING
*COMPUTER PROGRAMS
ACCURACY
MELTS
COLD REGIONS
KARA SEA
HIGH RESOLUTION
BOUNDARIES
ICE
CONCENTRATION(COMPOSITION)
BARENTS SEA
SUMMER
LAND AREAS
CHECKOUT PROCEDURES
PASSIVE SYSTEMS
GROWTH(GENERAL)
EDGES
MODELS
MICROWAVES
PE63207N
WUDN894428
description The hydraulic/thermodynamic Artic sea-ice model is designed by W.D. Hibler of the Cold Regions Research and Engineering Laboratory (CREEL) has been adapted to the Barents Sea. This model is driven by atmospheric forcing from the Naval Operational Global Atmospheric Prediction System (NOGAPS) and oceanic forcing from the Hibler and Bryan coupled ice-ocean model. This high-resolution model (25 km), which covers the entire Barents Sea and the western half of the Kara Sea, uses a 6-hour time step. Model results show good agreement with such data as the Naval Polar Oceanography Center's (NPOC) analysis of ice concentration and concentrations derived from passive microwave data. The model has a tendency, however, to melt ice too quickly in summer and to grow it back too slowly in the fall. Planned improvements in the atmospheric and oceanic forcing should correct this problem. The high resolution of the Barents Sea model enables it to predict the ice edge, ice growth and decay, and the movement of ice near land boundaries with greater accuracy than does the PIPS model. The Regional Polar Ice Prediction System for the Barents Sea (RPIPS-B) is the forecast system designed to run at the Fleet Numerical Oceanography Center (FNOC) based on the Barents Sea Ice model. RPIPS-B is updated weekly by the NPOC analysis of ice concentration. The forecast system, presently in its 'operational checkout' phase, is being made ready for a winter-spring operational test. Keywords: Computer simulation; Computer programs.
author2 NAVAL OCEAN RESEARCH AND DEVELOPMENT ACTIVITY STENNIS SPACE CENTER MS
format Text
author Preller, Ruth H.
Riedlinger, Shelley
Posey, Pamela G.
author_facet Preller, Ruth H.
Riedlinger, Shelley
Posey, Pamela G.
author_sort Preller, Ruth H.
title The Regional Polar Ice Prediction System - Barents Sea (RPIPS-B): A technical Description
title_short The Regional Polar Ice Prediction System - Barents Sea (RPIPS-B): A technical Description
title_full The Regional Polar Ice Prediction System - Barents Sea (RPIPS-B): A technical Description
title_fullStr The Regional Polar Ice Prediction System - Barents Sea (RPIPS-B): A technical Description
title_full_unstemmed The Regional Polar Ice Prediction System - Barents Sea (RPIPS-B): A technical Description
title_sort regional polar ice prediction system - barents sea (rpips-b): a technical description
publishDate 1989
url http://www.dtic.mil/docs/citations/ADA213159
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA213159
geographic Barents Sea
Kara Sea
geographic_facet Barents Sea
Kara Sea
genre Barents Sea
Cold Regions Research and Engineering Laboratory
Ice
Kara Sea
permafrost
Sea ice
genre_facet Barents Sea
Cold Regions Research and Engineering Laboratory
Ice
Kara Sea
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA213159
op_rights Approved for public release; distribution is unlimited.
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