Observing and Modeling the Surface Scattering Layer of First-Year Arctic Sea Ice

The long-term goal of this work is to increase the quantitative understanding of the partitioning of incident solar radiation by sea ice. The partitioning of shortwave radiation into components backscattered to the atmosphere, absorbed by the ice, and transmitted to the ocean is central to icealbedo...

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Bibliographic Details
Main Authors: Moritz, Richard E, Light, Bonnie
Other Authors: WASHINGTON UNIV SEATTLE APPLIED PHYSICS LAB
Format: Text
Language:English
Published: 2003
Subjects:
ICE
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA630015
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA630015
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record_format openpolar
spelling ftdtic:ADA630015 2023-05-15T14:56:12+02:00 Observing and Modeling the Surface Scattering Layer of First-Year Arctic Sea Ice Moritz, Richard E Light, Bonnie WASHINGTON UNIV SEATTLE APPLIED PHYSICS LAB 2003-09-30 text/html http://www.dtic.mil/docs/citations/ADA630015 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA630015 en eng http://www.dtic.mil/docs/citations/ADA630015 Approved for public release; distribution is unlimited. DTIC Astrophysics Snow Ice and Permafrost *ARCTIC OCEAN *BACKSCATTERING *SCATTERING *SEA ICE *SOLAR RADIATION ATMOSPHERES BIOLOGY CYCLES DEPTH FEEDBACK ICE ICE FORMATION IMPACT INFRARED RADIATION LAYERS LIQUIDS MEAN MECHANICAL PROPERTIES MODELS OCEANS PHYSICAL PROPERTIES PONDS SHORT WAVELENGTHS SNOW COVER UNDERICE WATER Text 2003 ftdtic 2016-05-08T15:22:40Z The long-term goal of this work is to increase the quantitative understanding of the partitioning of incident solar radiation by sea ice. The partitioning of shortwave radiation into components backscattered to the atmosphere, absorbed by the ice, and transmitted to the ocean is central to icealbedo feedback, the mean annual cycle of ice thickness, mechanical and biological properties of the ice, and the qualitative and quantitative properties of light fields available to under-ice biological communities. This partitioning is known to depend strongly on the physical properties of the ice cover including ice concentration, snow cover, area, depth and size of liquid water ponds, and the presence of surface scattering layers. The focus of this research is to address the impact of surface scattering layers on the partitioning of incident solar radiation at the atmosphere-sea ice-ocean interface. Text Arctic Arctic Ocean Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Astrophysics
Snow
Ice and Permafrost
*ARCTIC OCEAN
*BACKSCATTERING
*SCATTERING
*SEA ICE
*SOLAR RADIATION
ATMOSPHERES
BIOLOGY
CYCLES
DEPTH
FEEDBACK
ICE
ICE FORMATION
IMPACT
INFRARED RADIATION
LAYERS
LIQUIDS
MEAN
MECHANICAL PROPERTIES
MODELS
OCEANS
PHYSICAL PROPERTIES
PONDS
SHORT WAVELENGTHS
SNOW COVER
UNDERICE
WATER
spellingShingle Astrophysics
Snow
Ice and Permafrost
*ARCTIC OCEAN
*BACKSCATTERING
*SCATTERING
*SEA ICE
*SOLAR RADIATION
ATMOSPHERES
BIOLOGY
CYCLES
DEPTH
FEEDBACK
ICE
ICE FORMATION
IMPACT
INFRARED RADIATION
LAYERS
LIQUIDS
MEAN
MECHANICAL PROPERTIES
MODELS
OCEANS
PHYSICAL PROPERTIES
PONDS
SHORT WAVELENGTHS
SNOW COVER
UNDERICE
WATER
Moritz, Richard E
Light, Bonnie
Observing and Modeling the Surface Scattering Layer of First-Year Arctic Sea Ice
topic_facet Astrophysics
Snow
Ice and Permafrost
*ARCTIC OCEAN
*BACKSCATTERING
*SCATTERING
*SEA ICE
*SOLAR RADIATION
ATMOSPHERES
BIOLOGY
CYCLES
DEPTH
FEEDBACK
ICE
ICE FORMATION
IMPACT
INFRARED RADIATION
LAYERS
LIQUIDS
MEAN
MECHANICAL PROPERTIES
MODELS
OCEANS
PHYSICAL PROPERTIES
PONDS
SHORT WAVELENGTHS
SNOW COVER
UNDERICE
WATER
description The long-term goal of this work is to increase the quantitative understanding of the partitioning of incident solar radiation by sea ice. The partitioning of shortwave radiation into components backscattered to the atmosphere, absorbed by the ice, and transmitted to the ocean is central to icealbedo feedback, the mean annual cycle of ice thickness, mechanical and biological properties of the ice, and the qualitative and quantitative properties of light fields available to under-ice biological communities. This partitioning is known to depend strongly on the physical properties of the ice cover including ice concentration, snow cover, area, depth and size of liquid water ponds, and the presence of surface scattering layers. The focus of this research is to address the impact of surface scattering layers on the partitioning of incident solar radiation at the atmosphere-sea ice-ocean interface.
author2 WASHINGTON UNIV SEATTLE APPLIED PHYSICS LAB
format Text
author Moritz, Richard E
Light, Bonnie
author_facet Moritz, Richard E
Light, Bonnie
author_sort Moritz, Richard E
title Observing and Modeling the Surface Scattering Layer of First-Year Arctic Sea Ice
title_short Observing and Modeling the Surface Scattering Layer of First-Year Arctic Sea Ice
title_full Observing and Modeling the Surface Scattering Layer of First-Year Arctic Sea Ice
title_fullStr Observing and Modeling the Surface Scattering Layer of First-Year Arctic Sea Ice
title_full_unstemmed Observing and Modeling the Surface Scattering Layer of First-Year Arctic Sea Ice
title_sort observing and modeling the surface scattering layer of first-year arctic sea ice
publishDate 2003
url http://www.dtic.mil/docs/citations/ADA630015
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA630015
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
op_relation http://www.dtic.mil/docs/citations/ADA630015
op_rights Approved for public release; distribution is unlimited.
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