Use of Side-Looking Airborne Radar to Determine Lake Depth on the Alaskan North Slope
Side-looking airborne radar (SLAR) imagery obtained in April-May 1974 from the North Slope of Alaska between Barrow and Harrison Bay indicates that tundra lakes can be separated into two classes based on the strength of the radar returns. Correlations between the areal patterns of the returns, limit...
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ftdtic:ADA011249 2023-05-15T15:39:41+02:00 Use of Side-Looking Airborne Radar to Determine Lake Depth on the Alaskan North Slope Sellmann,P. Weeks,W. F. Campbell,W. J. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1975-05 text/html http://www.dtic.mil/docs/citations/ADA011249 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA011249 en eng http://www.dtic.mil/docs/citations/ADA011249 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Hydrology Limnology and Potamology Snow Ice and Permafrost *ALASKA *ICE *LAKES THICKNESS COASTAL REGIONS AIRBORNE RADAR IMAGES DEPTH FRESH WATER CLASSIFICATION SIDE LOOKING RADAR BRACKISH WATER Ice cover Remote sensing Lake ice Text 1975 ftdtic 2016-02-20T09:48:24Z Side-looking airborne radar (SLAR) imagery obtained in April-May 1974 from the North Slope of Alaska between Barrow and Harrison Bay indicates that tundra lakes can be separated into two classes based on the strength of the radar returns. Correlations between the areal patterns of the returns, limited ground observations on lake depths, and information obtained from ERTS imagery strongly suggest that freshwater lakes giving weak returns are frozen completely to the bottom while lakes giving strong returns are not. Brackish lakes also give weak returns even when they are not completely frozen. This is presumably the result of the brine present in the lower portion of the ice cover limiting the penetration of the X-band radiation into the ice. Although the physical cause of the differences in radar backscatter has not been identified, several possibilities are discussed. The ability to rapidly and easily separate the tundra lakes into these two classes via SLAR should be useful in a wide variety of different problems. Text Barrow Ice north slope permafrost Tundra Alaska Defense Technical Information Center: DTIC Technical Reports database Ice Lakes ENVELOPE(-131.345,-131.345,60.413,60.413) |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Hydrology Limnology and Potamology Snow Ice and Permafrost *ALASKA *ICE *LAKES THICKNESS COASTAL REGIONS AIRBORNE RADAR IMAGES DEPTH FRESH WATER CLASSIFICATION SIDE LOOKING RADAR BRACKISH WATER Ice cover Remote sensing Lake ice |
spellingShingle |
Hydrology Limnology and Potamology Snow Ice and Permafrost *ALASKA *ICE *LAKES THICKNESS COASTAL REGIONS AIRBORNE RADAR IMAGES DEPTH FRESH WATER CLASSIFICATION SIDE LOOKING RADAR BRACKISH WATER Ice cover Remote sensing Lake ice Sellmann,P. Weeks,W. F. Campbell,W. J. Use of Side-Looking Airborne Radar to Determine Lake Depth on the Alaskan North Slope |
topic_facet |
Hydrology Limnology and Potamology Snow Ice and Permafrost *ALASKA *ICE *LAKES THICKNESS COASTAL REGIONS AIRBORNE RADAR IMAGES DEPTH FRESH WATER CLASSIFICATION SIDE LOOKING RADAR BRACKISH WATER Ice cover Remote sensing Lake ice |
description |
Side-looking airborne radar (SLAR) imagery obtained in April-May 1974 from the North Slope of Alaska between Barrow and Harrison Bay indicates that tundra lakes can be separated into two classes based on the strength of the radar returns. Correlations between the areal patterns of the returns, limited ground observations on lake depths, and information obtained from ERTS imagery strongly suggest that freshwater lakes giving weak returns are frozen completely to the bottom while lakes giving strong returns are not. Brackish lakes also give weak returns even when they are not completely frozen. This is presumably the result of the brine present in the lower portion of the ice cover limiting the penetration of the X-band radiation into the ice. Although the physical cause of the differences in radar backscatter has not been identified, several possibilities are discussed. The ability to rapidly and easily separate the tundra lakes into these two classes via SLAR should be useful in a wide variety of different problems. |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H |
format |
Text |
author |
Sellmann,P. Weeks,W. F. Campbell,W. J. |
author_facet |
Sellmann,P. Weeks,W. F. Campbell,W. J. |
author_sort |
Sellmann,P. |
title |
Use of Side-Looking Airborne Radar to Determine Lake Depth on the Alaskan North Slope |
title_short |
Use of Side-Looking Airborne Radar to Determine Lake Depth on the Alaskan North Slope |
title_full |
Use of Side-Looking Airborne Radar to Determine Lake Depth on the Alaskan North Slope |
title_fullStr |
Use of Side-Looking Airborne Radar to Determine Lake Depth on the Alaskan North Slope |
title_full_unstemmed |
Use of Side-Looking Airborne Radar to Determine Lake Depth on the Alaskan North Slope |
title_sort |
use of side-looking airborne radar to determine lake depth on the alaskan north slope |
publishDate |
1975 |
url |
http://www.dtic.mil/docs/citations/ADA011249 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA011249 |
long_lat |
ENVELOPE(-131.345,-131.345,60.413,60.413) |
geographic |
Ice Lakes |
geographic_facet |
Ice Lakes |
genre |
Barrow Ice north slope permafrost Tundra Alaska |
genre_facet |
Barrow Ice north slope permafrost Tundra Alaska |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA011249 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766371718991970304 |