Ice Drift in Robeson Channel as Determined Using Television Moving Target Circuitry.

The movement of ice floes in Robeson Channel was followed over a one-week period during August 1973 using television moving-target circuitry from a cliffside base 350 m above sea level. The basis of the method was to subtract a current TV picture from a video tape recording of the same scene made so...

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Bibliographic Details
Main Authors: Henderson,I. H. S., Paquet,F.
Other Authors: DEFENCE RESEARCH ESTABLISHMENT OTTAWA (ONTARIO)
Format: Text
Language:English
Published: 1974
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA010397
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA010397
id ftdtic:ADA010397
record_format openpolar
spelling ftdtic:ADA010397 2023-05-15T15:03:23+02:00 Ice Drift in Robeson Channel as Determined Using Television Moving Target Circuitry. Henderson,I. H. S. Paquet,F. DEFENCE RESEARCH ESTABLISHMENT OTTAWA (ONTARIO) 1974-03 text/html http://www.dtic.mil/docs/citations/ADA010397 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA010397 en eng http://www.dtic.mil/docs/citations/ADA010397 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Snow Ice and Permafrost *DRIFT *SEA ICE MEASUREMENT OCEAN CURRENTS CANADA WIND TRACKING TIDAL CURRENTS ARCTIC REGIONS GREENLAND MOVING TARGET INDICATORS TELEVISION CAMERAS CLOSED CIRCUIT TELEVISION ELLESMERE ISLAND VIDEO TAPE RECORDING *Robeson Channel Text 1974 ftdtic 2016-02-20T09:43:05Z The movement of ice floes in Robeson Channel was followed over a one-week period during August 1973 using television moving-target circuitry from a cliffside base 350 m above sea level. The basis of the method was to subtract a current TV picture from a video tape recording of the same scene made some time previously, the difference imagery being displayed on a monitor. The TV camera was aimed to produce coincidence of a reference point selected near the center of the pre-recorded imagery, and the changes in azimuth and elevation recorded. From these, ice drift velocities were calculated. Errata sheet inserted. Text Arctic Ellesmere Island Greenland Ice permafrost Robeson channel Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic Canada Ellesmere Island Greenland Robeson Channel ENVELOPE(-61.473,-61.473,81.995,81.995)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*DRIFT
*SEA ICE
MEASUREMENT
OCEAN CURRENTS
CANADA
WIND
TRACKING
TIDAL CURRENTS
ARCTIC REGIONS
GREENLAND
MOVING TARGET INDICATORS
TELEVISION CAMERAS
CLOSED CIRCUIT TELEVISION
ELLESMERE ISLAND
VIDEO TAPE RECORDING
*Robeson Channel
spellingShingle Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*DRIFT
*SEA ICE
MEASUREMENT
OCEAN CURRENTS
CANADA
WIND
TRACKING
TIDAL CURRENTS
ARCTIC REGIONS
GREENLAND
MOVING TARGET INDICATORS
TELEVISION CAMERAS
CLOSED CIRCUIT TELEVISION
ELLESMERE ISLAND
VIDEO TAPE RECORDING
*Robeson Channel
Henderson,I. H. S.
Paquet,F.
Ice Drift in Robeson Channel as Determined Using Television Moving Target Circuitry.
topic_facet Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*DRIFT
*SEA ICE
MEASUREMENT
OCEAN CURRENTS
CANADA
WIND
TRACKING
TIDAL CURRENTS
ARCTIC REGIONS
GREENLAND
MOVING TARGET INDICATORS
TELEVISION CAMERAS
CLOSED CIRCUIT TELEVISION
ELLESMERE ISLAND
VIDEO TAPE RECORDING
*Robeson Channel
description The movement of ice floes in Robeson Channel was followed over a one-week period during August 1973 using television moving-target circuitry from a cliffside base 350 m above sea level. The basis of the method was to subtract a current TV picture from a video tape recording of the same scene made some time previously, the difference imagery being displayed on a monitor. The TV camera was aimed to produce coincidence of a reference point selected near the center of the pre-recorded imagery, and the changes in azimuth and elevation recorded. From these, ice drift velocities were calculated. Errata sheet inserted.
author2 DEFENCE RESEARCH ESTABLISHMENT OTTAWA (ONTARIO)
format Text
author Henderson,I. H. S.
Paquet,F.
author_facet Henderson,I. H. S.
Paquet,F.
author_sort Henderson,I. H. S.
title Ice Drift in Robeson Channel as Determined Using Television Moving Target Circuitry.
title_short Ice Drift in Robeson Channel as Determined Using Television Moving Target Circuitry.
title_full Ice Drift in Robeson Channel as Determined Using Television Moving Target Circuitry.
title_fullStr Ice Drift in Robeson Channel as Determined Using Television Moving Target Circuitry.
title_full_unstemmed Ice Drift in Robeson Channel as Determined Using Television Moving Target Circuitry.
title_sort ice drift in robeson channel as determined using television moving target circuitry.
publishDate 1974
url http://www.dtic.mil/docs/citations/ADA010397
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA010397
long_lat ENVELOPE(-61.473,-61.473,81.995,81.995)
geographic Arctic
Canada
Ellesmere Island
Greenland
Robeson Channel
geographic_facet Arctic
Canada
Ellesmere Island
Greenland
Robeson Channel
genre Arctic
Ellesmere Island
Greenland
Ice
permafrost
Robeson channel
Sea ice
genre_facet Arctic
Ellesmere Island
Greenland
Ice
permafrost
Robeson channel
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA010397
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766335239091650560