Preliminary Analysis of Laser Terrain Profiles of Sea Ice Surfaces.

The paper describes the results of a preliminary analysis of laser terrain profile data obtained with coincident photography from an altitude of 1000 feet over the sea ice fields of the Beaufort Sea in April 1968. Analysis of the data reveals that sea ice surface roughness and the nature of the roug...

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Bibliographic Details
Main Author: Ketchum, Robert D., Jr
Other Authors: NAVAL OCEANOGRAPHIC OFFICE NSTL STATION MS
Format: Text
Language:English
Published: 1970
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0871646
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0871646
id ftdtic:AD0871646
record_format openpolar
spelling ftdtic:AD0871646 2023-05-15T15:07:44+02:00 Preliminary Analysis of Laser Terrain Profiles of Sea Ice Surfaces. Ketchum, Robert D., Jr NAVAL OCEANOGRAPHIC OFFICE NSTL STATION MS 1970-05 text/html http://www.dtic.mil/docs/citations/AD0871646 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0871646 en eng http://www.dtic.mil/docs/citations/AD0871646 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Lasers and Masers (*SEA ICE AERIAL RECONNAISSANCE) (*AERIAL RECONNAISSANCE LASERS) MAPPING AERIAL PHOTOGRAPHY SURFACE PROPERTIES ROUGHNESS CRACKS THICKNESS DATA PROCESSING ICE ISLANDS ARCTIC REGIONS ICE REPORTING ICE FORECASTING *LASER TERRAIN PROFILES *REMOTE SENSING WH-4 ICE ISLAND Text 1970 ftdtic 2016-02-19T06:18:46Z The paper describes the results of a preliminary analysis of laser terrain profile data obtained with coincident photography from an altitude of 1000 feet over the sea ice fields of the Beaufort Sea in April 1968. Analysis of the data reveals that sea ice surface roughness and the nature of the roughness and relative surface reflectivities, which are both manifested in the laser terrain profile, can be used to interpret the categorical stages of ice development. The laser terrain profiler seemingly detected, with acceptable accuracy, all ice features traversed; however, ice pressure ridges, ice hummocks, or ice blocks could not be discriminated from each other on the record since the measurement is only two dimensional. These features were always detectable even when occurring in rapid succession. Cracks are very discernible on the laser terrain profile record. Useful estimations of the thickness of sea ice from the laser data were not possible. The errors possible in interpolation of the aircraft altitude variations were unacceptable for determining the ice surface elevation above sea level. (Author) Text Arctic Beaufort Sea Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
Lasers and Masers
(*SEA ICE
AERIAL RECONNAISSANCE)
(*AERIAL RECONNAISSANCE
LASERS)
MAPPING
AERIAL PHOTOGRAPHY
SURFACE PROPERTIES
ROUGHNESS
CRACKS
THICKNESS
DATA PROCESSING
ICE ISLANDS
ARCTIC REGIONS
ICE REPORTING
ICE FORECASTING
*LASER TERRAIN PROFILES
*REMOTE SENSING
WH-4 ICE ISLAND
spellingShingle Snow
Ice and Permafrost
Lasers and Masers
(*SEA ICE
AERIAL RECONNAISSANCE)
(*AERIAL RECONNAISSANCE
LASERS)
MAPPING
AERIAL PHOTOGRAPHY
SURFACE PROPERTIES
ROUGHNESS
CRACKS
THICKNESS
DATA PROCESSING
ICE ISLANDS
ARCTIC REGIONS
ICE REPORTING
ICE FORECASTING
*LASER TERRAIN PROFILES
*REMOTE SENSING
WH-4 ICE ISLAND
Ketchum, Robert D., Jr
Preliminary Analysis of Laser Terrain Profiles of Sea Ice Surfaces.
topic_facet Snow
Ice and Permafrost
Lasers and Masers
(*SEA ICE
AERIAL RECONNAISSANCE)
(*AERIAL RECONNAISSANCE
LASERS)
MAPPING
AERIAL PHOTOGRAPHY
SURFACE PROPERTIES
ROUGHNESS
CRACKS
THICKNESS
DATA PROCESSING
ICE ISLANDS
ARCTIC REGIONS
ICE REPORTING
ICE FORECASTING
*LASER TERRAIN PROFILES
*REMOTE SENSING
WH-4 ICE ISLAND
description The paper describes the results of a preliminary analysis of laser terrain profile data obtained with coincident photography from an altitude of 1000 feet over the sea ice fields of the Beaufort Sea in April 1968. Analysis of the data reveals that sea ice surface roughness and the nature of the roughness and relative surface reflectivities, which are both manifested in the laser terrain profile, can be used to interpret the categorical stages of ice development. The laser terrain profiler seemingly detected, with acceptable accuracy, all ice features traversed; however, ice pressure ridges, ice hummocks, or ice blocks could not be discriminated from each other on the record since the measurement is only two dimensional. These features were always detectable even when occurring in rapid succession. Cracks are very discernible on the laser terrain profile record. Useful estimations of the thickness of sea ice from the laser data were not possible. The errors possible in interpolation of the aircraft altitude variations were unacceptable for determining the ice surface elevation above sea level. (Author)
author2 NAVAL OCEANOGRAPHIC OFFICE NSTL STATION MS
format Text
author Ketchum, Robert D., Jr
author_facet Ketchum, Robert D., Jr
author_sort Ketchum, Robert D., Jr
title Preliminary Analysis of Laser Terrain Profiles of Sea Ice Surfaces.
title_short Preliminary Analysis of Laser Terrain Profiles of Sea Ice Surfaces.
title_full Preliminary Analysis of Laser Terrain Profiles of Sea Ice Surfaces.
title_fullStr Preliminary Analysis of Laser Terrain Profiles of Sea Ice Surfaces.
title_full_unstemmed Preliminary Analysis of Laser Terrain Profiles of Sea Ice Surfaces.
title_sort preliminary analysis of laser terrain profiles of sea ice surfaces.
publishDate 1970
url http://www.dtic.mil/docs/citations/AD0871646
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0871646
geographic Arctic
geographic_facet Arctic
genre Arctic
Beaufort Sea
Ice
permafrost
Sea ice
genre_facet Arctic
Beaufort Sea
Ice
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0871646
op_rights APPROVED FOR PUBLIC RELEASE
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