RADIATION CHARACTERISTICS OF THE MOST IMPORTANT CLASSES OF LOCAL WEATHER IN THE ARCTIC

The radiant energy of the sun is of very great importance in shaping local weather. Therefore in the description of climate in terms of classes of weather it is necessary to take into account not only radiation data for considerable intervals of time (for the month or year) but also the day-to-day c...

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Bibliographic Details
Main Author: Suzyumova,G. N.
Other Authors: DEFENCE SCIENTIFIC INFORMATION SERVICE OTTAWA (ONTARIO)
Format: Text
Language:English
Published: 1970
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0706551
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0706551
id ftdtic:AD0706551
record_format openpolar
spelling ftdtic:AD0706551 2023-05-15T14:29:08+02:00 RADIATION CHARACTERISTICS OF THE MOST IMPORTANT CLASSES OF LOCAL WEATHER IN THE ARCTIC Suzyumova,G. N. DEFENCE SCIENTIFIC INFORMATION SERVICE OTTAWA (ONTARIO) 1970-04 text/html http://www.dtic.mil/docs/citations/AD0706551 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0706551 en eng http://www.dtic.mil/docs/citations/AD0706551 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Meteorology (*WEATHER FORECASTING SOLAR RADIATION) (*SOLAR RADIATION ARCTIC REGIONS) SCATTERING ICE ISLANDS STATISTICAL DATA BRIGHTNESS FREEZING ARCTIC OCEAN USSR TRANSLATIONS Text 1970 ftdtic 2016-02-18T23:20:51Z The radiant energy of the sun is of very great importance in shaping local weather. Therefore in the description of climate in terms of classes of weather it is necessary to take into account not only radiation data for considerable intervals of time (for the month or year) but also the day-to-day characterization. For purposes of this study we divided the Arctic Basin (North Polar Sea) into two regions, the first region taking in the polar area down to the 85th parallel, and the second region the eastern part of the Central Arctic Basin adjacent to the Pacific Ocean sector of the Arctic, between 85N and 75N. From the available observations for each class of weather we calculated the mean monthly values of the total and scattered radiations, and determined generalized characteristic values for the three-month period May to July, since within this period the radiation characteristics do not change very much from month to month. (Author) Trans. of Akademiya Nauk SSSR. Izvestiya. Seriya Geograficheskaya, n4 p136-138 1969, by E. R. Hope. Text Arctic Basin Arctic Arctic Ocean Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Pacific
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Meteorology
(*WEATHER FORECASTING
SOLAR RADIATION)
(*SOLAR RADIATION
ARCTIC REGIONS)
SCATTERING
ICE ISLANDS
STATISTICAL DATA
BRIGHTNESS
FREEZING
ARCTIC OCEAN
USSR
TRANSLATIONS
spellingShingle Meteorology
(*WEATHER FORECASTING
SOLAR RADIATION)
(*SOLAR RADIATION
ARCTIC REGIONS)
SCATTERING
ICE ISLANDS
STATISTICAL DATA
BRIGHTNESS
FREEZING
ARCTIC OCEAN
USSR
TRANSLATIONS
Suzyumova,G. N.
RADIATION CHARACTERISTICS OF THE MOST IMPORTANT CLASSES OF LOCAL WEATHER IN THE ARCTIC
topic_facet Meteorology
(*WEATHER FORECASTING
SOLAR RADIATION)
(*SOLAR RADIATION
ARCTIC REGIONS)
SCATTERING
ICE ISLANDS
STATISTICAL DATA
BRIGHTNESS
FREEZING
ARCTIC OCEAN
USSR
TRANSLATIONS
description The radiant energy of the sun is of very great importance in shaping local weather. Therefore in the description of climate in terms of classes of weather it is necessary to take into account not only radiation data for considerable intervals of time (for the month or year) but also the day-to-day characterization. For purposes of this study we divided the Arctic Basin (North Polar Sea) into two regions, the first region taking in the polar area down to the 85th parallel, and the second region the eastern part of the Central Arctic Basin adjacent to the Pacific Ocean sector of the Arctic, between 85N and 75N. From the available observations for each class of weather we calculated the mean monthly values of the total and scattered radiations, and determined generalized characteristic values for the three-month period May to July, since within this period the radiation characteristics do not change very much from month to month. (Author) Trans. of Akademiya Nauk SSSR. Izvestiya. Seriya Geograficheskaya, n4 p136-138 1969, by E. R. Hope.
author2 DEFENCE SCIENTIFIC INFORMATION SERVICE OTTAWA (ONTARIO)
format Text
author Suzyumova,G. N.
author_facet Suzyumova,G. N.
author_sort Suzyumova,G. N.
title RADIATION CHARACTERISTICS OF THE MOST IMPORTANT CLASSES OF LOCAL WEATHER IN THE ARCTIC
title_short RADIATION CHARACTERISTICS OF THE MOST IMPORTANT CLASSES OF LOCAL WEATHER IN THE ARCTIC
title_full RADIATION CHARACTERISTICS OF THE MOST IMPORTANT CLASSES OF LOCAL WEATHER IN THE ARCTIC
title_fullStr RADIATION CHARACTERISTICS OF THE MOST IMPORTANT CLASSES OF LOCAL WEATHER IN THE ARCTIC
title_full_unstemmed RADIATION CHARACTERISTICS OF THE MOST IMPORTANT CLASSES OF LOCAL WEATHER IN THE ARCTIC
title_sort radiation characteristics of the most important classes of local weather in the arctic
publishDate 1970
url http://www.dtic.mil/docs/citations/AD0706551
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0706551
geographic Arctic
Arctic Ocean
Pacific
geographic_facet Arctic
Arctic Ocean
Pacific
genre Arctic Basin
Arctic
Arctic Ocean
genre_facet Arctic Basin
Arctic
Arctic Ocean
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0706551
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766303221559590912