The Optical Properties of Young Sea Ice

Eight laboratory experiments were performed to determine the optical properties of young salt ice and to examine correlations between the optical properties and the state of the ice. Ice grown at different temperatures (-10, -20, -30, and -37 C) and from water of different salinities (0, 16, and 31...

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Bibliographic Details
Main Author: Perovich,Donald Kole
Other Authors: WASHINGTON UNIV SEATTLE DEPT OF ATMOSPHERIC SCIENCES
Format: Text
Language:English
Published: 1979
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA074908
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA074908
id ftdtic:ADA074908
record_format openpolar
spelling ftdtic:ADA074908 2023-05-15T16:37:18+02:00 The Optical Properties of Young Sea Ice Perovich,Donald Kole WASHINGTON UNIV SEATTLE DEPT OF ATMOSPHERIC SCIENCES 1979-08 text/html http://www.dtic.mil/docs/citations/ADA074908 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA074908 en eng http://www.dtic.mil/docs/citations/ADA074908 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Optics *OPTICAL PROPERTIES *SEA ICE POLAR REGIONS TEMPERATURE EXPERIMENTAL DATA LABORATORY TESTS TEST METHODS THERMISTORS SALINITY COLD WEATHER TESTS WUNR307252 Text 1979 ftdtic 2016-02-20T16:57:40Z Eight laboratory experiments were performed to determine the optical properties of young salt ice and to examine correlations between the optical properties and the state of the ice. Ice grown at different temperatures (-10, -20, -30, and -37 C) and from water of different salinities (0, 16, and 31 0/00) was investigated. The experiments were conducted using a tank system which was designed to grow ice similar to that found in nature, allow an accurate determination of the state and structure of the ice, and permit in situ optical measurements to be made. A four stream discrete ordinates photometric model was developed to treat the case of a floating ice slab. The model included both anisotropic scattering and refraction at the boundaries. The effects on albedo and transmittance of vairaitions in such model parameters as the single scattering albedo and the phase function were investigated. Using one and two layer models, theoretical albedos and transmittances were compared to experimental values. The four stream model was further applied to investigate such topics as the depth dependence of irradiance, cases of direct beam incident radiation, the spectral dependence of albedo and transmittance, and the effects of surface layers. It was suggested that future laboratory research be oriented towards determination of single scattering albedos and phase functions for an extensive range of ice types. Text Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
Optics
*OPTICAL PROPERTIES
*SEA ICE
POLAR REGIONS
TEMPERATURE
EXPERIMENTAL DATA
LABORATORY TESTS
TEST METHODS
THERMISTORS
SALINITY
COLD WEATHER TESTS
WUNR307252
spellingShingle Snow
Ice and Permafrost
Optics
*OPTICAL PROPERTIES
*SEA ICE
POLAR REGIONS
TEMPERATURE
EXPERIMENTAL DATA
LABORATORY TESTS
TEST METHODS
THERMISTORS
SALINITY
COLD WEATHER TESTS
WUNR307252
Perovich,Donald Kole
The Optical Properties of Young Sea Ice
topic_facet Snow
Ice and Permafrost
Optics
*OPTICAL PROPERTIES
*SEA ICE
POLAR REGIONS
TEMPERATURE
EXPERIMENTAL DATA
LABORATORY TESTS
TEST METHODS
THERMISTORS
SALINITY
COLD WEATHER TESTS
WUNR307252
description Eight laboratory experiments were performed to determine the optical properties of young salt ice and to examine correlations between the optical properties and the state of the ice. Ice grown at different temperatures (-10, -20, -30, and -37 C) and from water of different salinities (0, 16, and 31 0/00) was investigated. The experiments were conducted using a tank system which was designed to grow ice similar to that found in nature, allow an accurate determination of the state and structure of the ice, and permit in situ optical measurements to be made. A four stream discrete ordinates photometric model was developed to treat the case of a floating ice slab. The model included both anisotropic scattering and refraction at the boundaries. The effects on albedo and transmittance of vairaitions in such model parameters as the single scattering albedo and the phase function were investigated. Using one and two layer models, theoretical albedos and transmittances were compared to experimental values. The four stream model was further applied to investigate such topics as the depth dependence of irradiance, cases of direct beam incident radiation, the spectral dependence of albedo and transmittance, and the effects of surface layers. It was suggested that future laboratory research be oriented towards determination of single scattering albedos and phase functions for an extensive range of ice types.
author2 WASHINGTON UNIV SEATTLE DEPT OF ATMOSPHERIC SCIENCES
format Text
author Perovich,Donald Kole
author_facet Perovich,Donald Kole
author_sort Perovich,Donald Kole
title The Optical Properties of Young Sea Ice
title_short The Optical Properties of Young Sea Ice
title_full The Optical Properties of Young Sea Ice
title_fullStr The Optical Properties of Young Sea Ice
title_full_unstemmed The Optical Properties of Young Sea Ice
title_sort optical properties of young sea ice
publishDate 1979
url http://www.dtic.mil/docs/citations/ADA074908
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA074908
genre Ice
permafrost
Sea ice
genre_facet Ice
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA074908
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766027600899080192