THE VERTICAL STRUCTURE OF SUMMER FOG IN THE DICKSON ISLAND REGION
IN July-August 1957 a number of meteorographs on moored balloons at two points, Dickson Island and Tadibe-Yakha were used to study the vertical structure of the atmosphere during sea and monsoon fogs. Results of t e inve tigations at Dickson Island are given. Meteorograph ascents to a height of 500...
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ftdtic:AD0264582 2023-05-15T15:05:10+02:00 THE VERTICAL STRUCTURE OF SUMMER FOG IN THE DICKSON ISLAND REGION VORONTSOV,P.A. SELITSKAIA,V.I. AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS 1961-06 text/html http://www.dtic.mil/docs/citations/AD0264582 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0264582 en eng http://www.dtic.mil/docs/citations/AD0264582 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS *FOG *METEOROLOGY MEASUREMENT METEOROLOGICAL BALLOONS MOISTURE POLAR REGIONS RADIOSONDES RECORDING SYSTEMS SOURCES TEMPERATURE INVERSION WIND DIRECTION INDICATORS Text 1961 ftdtic 2016-02-18T15:19:38Z IN July-August 1957 a number of meteorographs on moored balloons at two points, Dickson Island and Tadibe-Yakha were used to study the vertical structure of the atmosphere during sea and monsoon fogs. Results of t e inve tigations at Dickson Island are given. Meteorograph ascents to a height of 500 m were made every two hours with five-minute stops at 25, 50, 100, 15 , 200, 300, 400, and 500 m. The most favorable conditions for the development of sea fog were in Arctic air (AA) masses transferred from the Kara Sea. Monsoon fog developed with polar air (PA) movement above a cold ea surface. Under Dickson Island conditions, this could occur only with winds directed along the shore. Fog in AA masse us ally develops in anticyclones. As a rule, there is no fog in PA masses in the Dickson Island region; evidently it is formed over the sea at some distance from the coast. (Author) Text Arctic Kara Sea Defense Technical Information Center: DTIC Technical Reports database Arctic Kara Sea |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
*FOG *METEOROLOGY MEASUREMENT METEOROLOGICAL BALLOONS MOISTURE POLAR REGIONS RADIOSONDES RECORDING SYSTEMS SOURCES TEMPERATURE INVERSION WIND DIRECTION INDICATORS |
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*FOG *METEOROLOGY MEASUREMENT METEOROLOGICAL BALLOONS MOISTURE POLAR REGIONS RADIOSONDES RECORDING SYSTEMS SOURCES TEMPERATURE INVERSION WIND DIRECTION INDICATORS VORONTSOV,P.A. SELITSKAIA,V.I. THE VERTICAL STRUCTURE OF SUMMER FOG IN THE DICKSON ISLAND REGION |
topic_facet |
*FOG *METEOROLOGY MEASUREMENT METEOROLOGICAL BALLOONS MOISTURE POLAR REGIONS RADIOSONDES RECORDING SYSTEMS SOURCES TEMPERATURE INVERSION WIND DIRECTION INDICATORS |
description |
IN July-August 1957 a number of meteorographs on moored balloons at two points, Dickson Island and Tadibe-Yakha were used to study the vertical structure of the atmosphere during sea and monsoon fogs. Results of t e inve tigations at Dickson Island are given. Meteorograph ascents to a height of 500 m were made every two hours with five-minute stops at 25, 50, 100, 15 , 200, 300, 400, and 500 m. The most favorable conditions for the development of sea fog were in Arctic air (AA) masses transferred from the Kara Sea. Monsoon fog developed with polar air (PA) movement above a cold ea surface. Under Dickson Island conditions, this could occur only with winds directed along the shore. Fog in AA masse us ally develops in anticyclones. As a rule, there is no fog in PA masses in the Dickson Island region; evidently it is formed over the sea at some distance from the coast. (Author) |
author2 |
AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS |
format |
Text |
author |
VORONTSOV,P.A. SELITSKAIA,V.I. |
author_facet |
VORONTSOV,P.A. SELITSKAIA,V.I. |
author_sort |
VORONTSOV,P.A. |
title |
THE VERTICAL STRUCTURE OF SUMMER FOG IN THE DICKSON ISLAND REGION |
title_short |
THE VERTICAL STRUCTURE OF SUMMER FOG IN THE DICKSON ISLAND REGION |
title_full |
THE VERTICAL STRUCTURE OF SUMMER FOG IN THE DICKSON ISLAND REGION |
title_fullStr |
THE VERTICAL STRUCTURE OF SUMMER FOG IN THE DICKSON ISLAND REGION |
title_full_unstemmed |
THE VERTICAL STRUCTURE OF SUMMER FOG IN THE DICKSON ISLAND REGION |
title_sort |
vertical structure of summer fog in the dickson island region |
publishDate |
1961 |
url |
http://www.dtic.mil/docs/citations/AD0264582 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0264582 |
geographic |
Arctic Kara Sea |
geographic_facet |
Arctic Kara Sea |
genre |
Arctic Kara Sea |
genre_facet |
Arctic Kara Sea |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0264582 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
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1766336915955515392 |