AERIAL SURVEYS OF HUDSON BAY SURFACE TEMPERATURE-1967.

Aerial surveys of the surface temperature of Hudson Bay were completed in July, August and October of 1967. An airborne infrared radiation thermometer remotely sensed the surface radiation temperature. The surface temperature patterns are presented for each survey. Certain persistent surface thermal...

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Bibliographic Details
Main Authors: Wendland,Wayne M., Bryson,Reid A.
Other Authors: WISCONSIN UNIV MADISON DEPT OF METEOROLOGY
Format: Text
Language:English
Published: 1967
Subjects:
ICE
Online Access:http://www.dtic.mil/docs/citations/AD0664817
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0664817
id ftdtic:AD0664817
record_format openpolar
spelling ftdtic:AD0664817 2023-05-15T16:35:05+02:00 AERIAL SURVEYS OF HUDSON BAY SURFACE TEMPERATURE-1967. Wendland,Wayne M. Bryson,Reid A. WISCONSIN UNIV MADISON DEPT OF METEOROLOGY 1967-12 text/html http://www.dtic.mil/docs/citations/AD0664817 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0664817 en eng http://www.dtic.mil/docs/citations/AD0664817 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Meteorology (*SURFACE TEMPERATURE WATER) (*INFRARED RADIATION HUDSON BAY) AIRBORNE INFRARED EQUIPMENT THERMOMETERS MEASUREMENT DISTRIBUTION AIR MASS ANALYSIS PERIODIC VARIATIONS AIRCRAFT ICE FLIGHT PATHS ABSORPTION BOLOMETERS MAPS OCEANOGRAPHY SUMMER Text 1967 ftdtic 2016-02-18T20:47:00Z Aerial surveys of the surface temperature of Hudson Bay were completed in July, August and October of 1967. An airborne infrared radiation thermometer remotely sensed the surface radiation temperature. The surface temperature patterns are presented for each survey. Certain persistent surface thermal features were found during the first two surveys. In October, the temperature pattern was rather flat, and the large scale features mentioned above, although present, were not as well defined. Because the ice lingers on Hudson Bay into August, it leaves its 'signature' on the surface. A cold pool (presumably low salinity and therefore relatively low density) was found near the area of last ice. Due to the stratification of the upper layer of the Bay, this cold pool persists throughout most of the ice free season. (Author) Text Hudson Bay Defense Technical Information Center: DTIC Technical Reports database Hudson Bay Hudson
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Meteorology
(*SURFACE TEMPERATURE
WATER)
(*INFRARED RADIATION
HUDSON BAY)
AIRBORNE
INFRARED EQUIPMENT
THERMOMETERS
MEASUREMENT
DISTRIBUTION
AIR MASS ANALYSIS
PERIODIC VARIATIONS
AIRCRAFT
ICE
FLIGHT PATHS
ABSORPTION
BOLOMETERS
MAPS
OCEANOGRAPHY
SUMMER
spellingShingle Meteorology
(*SURFACE TEMPERATURE
WATER)
(*INFRARED RADIATION
HUDSON BAY)
AIRBORNE
INFRARED EQUIPMENT
THERMOMETERS
MEASUREMENT
DISTRIBUTION
AIR MASS ANALYSIS
PERIODIC VARIATIONS
AIRCRAFT
ICE
FLIGHT PATHS
ABSORPTION
BOLOMETERS
MAPS
OCEANOGRAPHY
SUMMER
Wendland,Wayne M.
Bryson,Reid A.
AERIAL SURVEYS OF HUDSON BAY SURFACE TEMPERATURE-1967.
topic_facet Meteorology
(*SURFACE TEMPERATURE
WATER)
(*INFRARED RADIATION
HUDSON BAY)
AIRBORNE
INFRARED EQUIPMENT
THERMOMETERS
MEASUREMENT
DISTRIBUTION
AIR MASS ANALYSIS
PERIODIC VARIATIONS
AIRCRAFT
ICE
FLIGHT PATHS
ABSORPTION
BOLOMETERS
MAPS
OCEANOGRAPHY
SUMMER
description Aerial surveys of the surface temperature of Hudson Bay were completed in July, August and October of 1967. An airborne infrared radiation thermometer remotely sensed the surface radiation temperature. The surface temperature patterns are presented for each survey. Certain persistent surface thermal features were found during the first two surveys. In October, the temperature pattern was rather flat, and the large scale features mentioned above, although present, were not as well defined. Because the ice lingers on Hudson Bay into August, it leaves its 'signature' on the surface. A cold pool (presumably low salinity and therefore relatively low density) was found near the area of last ice. Due to the stratification of the upper layer of the Bay, this cold pool persists throughout most of the ice free season. (Author)
author2 WISCONSIN UNIV MADISON DEPT OF METEOROLOGY
format Text
author Wendland,Wayne M.
Bryson,Reid A.
author_facet Wendland,Wayne M.
Bryson,Reid A.
author_sort Wendland,Wayne M.
title AERIAL SURVEYS OF HUDSON BAY SURFACE TEMPERATURE-1967.
title_short AERIAL SURVEYS OF HUDSON BAY SURFACE TEMPERATURE-1967.
title_full AERIAL SURVEYS OF HUDSON BAY SURFACE TEMPERATURE-1967.
title_fullStr AERIAL SURVEYS OF HUDSON BAY SURFACE TEMPERATURE-1967.
title_full_unstemmed AERIAL SURVEYS OF HUDSON BAY SURFACE TEMPERATURE-1967.
title_sort aerial surveys of hudson bay surface temperature-1967.
publishDate 1967
url http://www.dtic.mil/docs/citations/AD0664817
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0664817
geographic Hudson Bay
Hudson
geographic_facet Hudson Bay
Hudson
genre Hudson Bay
genre_facet Hudson Bay
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0664817
op_rights APPROVED FOR PUBLIC RELEASE
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