DETERMINATION OF HEAT BALANCE AT THE BOUNDARY LAYER OVER THE SEA
Formulas and graphs are given by which the turbulent sensible and latent heat transfer from water surface to the air can be determined from the measurements of the weather ships. From the observational data of seven North Atlantic weather ships, the heat fluxes have been calculated for four seasons...
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1961
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ftdtic:AD0273302 2023-05-15T17:30:26+02:00 DETERMINATION OF HEAT BALANCE AT THE BOUNDARY LAYER OVER THE SEA MANIER,GERHARD MOLLER,FRITZ MAINZ UNIV (WEST GERMANY) 1961-12 text/html http://www.dtic.mil/docs/citations/AD0273302 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0273302 en eng http://www.dtic.mil/docs/citations/AD0273302 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS *AIR *HEAT TRANSFER *OCEANS METEOROLOGY SHIPS STATISTICAL ANALYSIS WEATHER STATIONS Text 1961 ftdtic 2016-02-18T15:31:54Z Formulas and graphs are given by which the turbulent sensible and latent heat transfer from water surface to the air can be determined from the measurements of the weather ships. From the observational data of seven North Atlantic weather ships, the heat fluxes have been calculated for four seasons and as functions of wind speed and direction. The values are much larger than the heat fluxes derived by other authors. (Author) Text North Atlantic Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
*AIR *HEAT TRANSFER *OCEANS METEOROLOGY SHIPS STATISTICAL ANALYSIS WEATHER STATIONS |
spellingShingle |
*AIR *HEAT TRANSFER *OCEANS METEOROLOGY SHIPS STATISTICAL ANALYSIS WEATHER STATIONS MANIER,GERHARD MOLLER,FRITZ DETERMINATION OF HEAT BALANCE AT THE BOUNDARY LAYER OVER THE SEA |
topic_facet |
*AIR *HEAT TRANSFER *OCEANS METEOROLOGY SHIPS STATISTICAL ANALYSIS WEATHER STATIONS |
description |
Formulas and graphs are given by which the turbulent sensible and latent heat transfer from water surface to the air can be determined from the measurements of the weather ships. From the observational data of seven North Atlantic weather ships, the heat fluxes have been calculated for four seasons and as functions of wind speed and direction. The values are much larger than the heat fluxes derived by other authors. (Author) |
author2 |
MAINZ UNIV (WEST GERMANY) |
format |
Text |
author |
MANIER,GERHARD MOLLER,FRITZ |
author_facet |
MANIER,GERHARD MOLLER,FRITZ |
author_sort |
MANIER,GERHARD |
title |
DETERMINATION OF HEAT BALANCE AT THE BOUNDARY LAYER OVER THE SEA |
title_short |
DETERMINATION OF HEAT BALANCE AT THE BOUNDARY LAYER OVER THE SEA |
title_full |
DETERMINATION OF HEAT BALANCE AT THE BOUNDARY LAYER OVER THE SEA |
title_fullStr |
DETERMINATION OF HEAT BALANCE AT THE BOUNDARY LAYER OVER THE SEA |
title_full_unstemmed |
DETERMINATION OF HEAT BALANCE AT THE BOUNDARY LAYER OVER THE SEA |
title_sort |
determination of heat balance at the boundary layer over the sea |
publishDate |
1961 |
url |
http://www.dtic.mil/docs/citations/AD0273302 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0273302 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0273302 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766126884462002176 |