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 ice-albed...

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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: 2006
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA612676
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA612676
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record_format openpolar
spelling ftdtic:ADA612676 2023-05-15T13:10:55+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 2006-09-30 text/html http://www.dtic.mil/docs/citations/ADA612676 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA612676 en eng http://www.dtic.mil/docs/citations/ADA612676 Approved for public release; distribution is unlimited. DTIC Snow Ice and Permafrost *SCATTERING *SEA ICE *SURFACE WATERS ALBEDO ARCTIC OCEAN ICE FORMATION MECHANICAL PROPERTIES OCEAN SURFACE OPTICAL PROPERTIES PHYSICAL PROPERTIES PONDS SHORT WAVELENGTHS SNOW COVER SOLAR RADIATION THICKNESS UNDERICE ICE COVER IOP(INHERENT OPTICAL PROPERTIES) LIGHT PENETRATION SPECTRAL TRANSMISSION Text 2006 ftdtic 2016-02-24T16:54:07Z 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 ice-albedo feedback, the mean annual cycle of ice thickness, mechanical properties of the ice, and the quality and quantity of light 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, depth and size of surface 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 albedo 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 Snow
Ice and Permafrost
*SCATTERING
*SEA ICE
*SURFACE WATERS
ALBEDO
ARCTIC OCEAN
ICE FORMATION
MECHANICAL PROPERTIES
OCEAN SURFACE
OPTICAL PROPERTIES
PHYSICAL PROPERTIES
PONDS
SHORT WAVELENGTHS
SNOW COVER
SOLAR RADIATION
THICKNESS
UNDERICE
ICE COVER
IOP(INHERENT OPTICAL PROPERTIES)
LIGHT PENETRATION
SPECTRAL TRANSMISSION
spellingShingle Snow
Ice and Permafrost
*SCATTERING
*SEA ICE
*SURFACE WATERS
ALBEDO
ARCTIC OCEAN
ICE FORMATION
MECHANICAL PROPERTIES
OCEAN SURFACE
OPTICAL PROPERTIES
PHYSICAL PROPERTIES
PONDS
SHORT WAVELENGTHS
SNOW COVER
SOLAR RADIATION
THICKNESS
UNDERICE
ICE COVER
IOP(INHERENT OPTICAL PROPERTIES)
LIGHT PENETRATION
SPECTRAL TRANSMISSION
Moritz, Richard E
Light, Bonnie
Observing and Modeling the Surface Scattering Layer of First-Year Arctic Sea Ice
topic_facet Snow
Ice and Permafrost
*SCATTERING
*SEA ICE
*SURFACE WATERS
ALBEDO
ARCTIC OCEAN
ICE FORMATION
MECHANICAL PROPERTIES
OCEAN SURFACE
OPTICAL PROPERTIES
PHYSICAL PROPERTIES
PONDS
SHORT WAVELENGTHS
SNOW COVER
SOLAR RADIATION
THICKNESS
UNDERICE
ICE COVER
IOP(INHERENT OPTICAL PROPERTIES)
LIGHT PENETRATION
SPECTRAL TRANSMISSION
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 ice-albedo feedback, the mean annual cycle of ice thickness, mechanical properties of the ice, and the quality and quantity of light 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, depth and size of surface 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 2006
url http://www.dtic.mil/docs/citations/ADA612676
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA612676
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre albedo
Arctic
Arctic Ocean
Ice
permafrost
Sea ice
genre_facet albedo
Arctic
Arctic Ocean
Ice
permafrost
Sea ice
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA612676
op_rights Approved for public release; distribution is unlimited.
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