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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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 |
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Open Polar |
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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 |
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1766027600899080192 |