LONG WAVE RADIATION AND TOTAL RADIATION BALANCE AT THE SURFACE IN THE ARCTIC
In climatology and general circulation studies, all the energy available at the surface is important and not only the short wave component. Reliable observations are available only for short wave radiation, and long wave components must be obtained by the application of radiation laws to the known s...
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ftdtic:AD0426319 2023-05-15T14:50:47+02:00 LONG WAVE RADIATION AND TOTAL RADIATION BALANCE AT THE SURFACE IN THE ARCTIC Vowinckel,E. Orvig,Svenn MCGILL UNIV MONTREAL (QUEBEC) 1963-10 text/html http://www.dtic.mil/docs/citations/AD0426319 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0426319 en eng http://www.dtic.mil/docs/citations/AD0426319 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS *EARTH(PLANET) SURFACE PROPERTIES CLIMATE ENERGY TEMPERATURE HUMIDITY CLOUDS EARTH SURFACE BALANCE Text 1963 ftdtic 2016-02-21T15:41:52Z In climatology and general circulation studies, all the energy available at the surface is important and not only the short wave component. Reliable observations are available only for short wave radiation, and long wave components must be obtained by the application of radiation laws to the known state of the atmosphere. Short wave radiation and its calculation for the Arctic was discussed in detail previously. The present report contains first the calculation of long wave radiation components, and then the radiation balance derived by the combination of all components. (Author) Text Arctic 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 |
*EARTH(PLANET) SURFACE PROPERTIES CLIMATE ENERGY TEMPERATURE HUMIDITY CLOUDS EARTH SURFACE BALANCE |
spellingShingle |
*EARTH(PLANET) SURFACE PROPERTIES CLIMATE ENERGY TEMPERATURE HUMIDITY CLOUDS EARTH SURFACE BALANCE Vowinckel,E. Orvig,Svenn LONG WAVE RADIATION AND TOTAL RADIATION BALANCE AT THE SURFACE IN THE ARCTIC |
topic_facet |
*EARTH(PLANET) SURFACE PROPERTIES CLIMATE ENERGY TEMPERATURE HUMIDITY CLOUDS EARTH SURFACE BALANCE |
description |
In climatology and general circulation studies, all the energy available at the surface is important and not only the short wave component. Reliable observations are available only for short wave radiation, and long wave components must be obtained by the application of radiation laws to the known state of the atmosphere. Short wave radiation and its calculation for the Arctic was discussed in detail previously. The present report contains first the calculation of long wave radiation components, and then the radiation balance derived by the combination of all components. (Author) |
author2 |
MCGILL UNIV MONTREAL (QUEBEC) |
format |
Text |
author |
Vowinckel,E. Orvig,Svenn |
author_facet |
Vowinckel,E. Orvig,Svenn |
author_sort |
Vowinckel,E. |
title |
LONG WAVE RADIATION AND TOTAL RADIATION BALANCE AT THE SURFACE IN THE ARCTIC |
title_short |
LONG WAVE RADIATION AND TOTAL RADIATION BALANCE AT THE SURFACE IN THE ARCTIC |
title_full |
LONG WAVE RADIATION AND TOTAL RADIATION BALANCE AT THE SURFACE IN THE ARCTIC |
title_fullStr |
LONG WAVE RADIATION AND TOTAL RADIATION BALANCE AT THE SURFACE IN THE ARCTIC |
title_full_unstemmed |
LONG WAVE RADIATION AND TOTAL RADIATION BALANCE AT THE SURFACE IN THE ARCTIC |
title_sort |
long wave radiation and total radiation balance at the surface in the arctic |
publishDate |
1963 |
url |
http://www.dtic.mil/docs/citations/AD0426319 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0426319 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0426319 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766321832638545920 |