Gases in Sea Ice: A Factor Bearing on the Transmission of Sound Energy.
This research is a continuation of the previous year's work on the migration of gases through sea ice and the transport of gases across the ice-snow-air boundary. Carbon dioxide, and possibly carbon monoxide, were observed to be replenished faster than other non-water interacting gases such as...
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ftdtic:ADA056115 2023-05-15T15:39:44+02:00 Gases in Sea Ice: A Factor Bearing on the Transmission of Sound Energy. Gosink,Thomas A Kelley,John J ALASKA UNIV COLLEGE INST OF MARINE SCIENCE 1977-09 text/html http://www.dtic.mil/docs/citations/ADA056115 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA056115 en eng http://www.dtic.mil/docs/citations/ADA056115 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost *GASES *SEA ICE STRESSES TEMPERATURE AIR DYNAMICS INTERFACES CARBON MONOXIDE CARBON DIOXIDE Text 1977 ftdtic 2016-02-20T13:23:52Z This research is a continuation of the previous year's work on the migration of gases through sea ice and the transport of gases across the ice-snow-air boundary. Carbon dioxide, and possibly carbon monoxide, were observed to be replenished faster than other non-water interacting gases such as nitrogen, oxygen, neon, and methane in flushed probe holes and at the surface. Large pulses of carbon dioxide were observed and suspected as the result of internal stresses in sea ice. The flux of gases in probe holes was near 2-4 microliter/sq cm/hr, and 1-2 microliter/sq cm/hr at the surface, relatively insignificant for oxygen, but very significant for trace gases such as carbon dioxide. The ocean was observed to be a source of carbon dioxide, carbon monoxide and methane to the atmosphere by way of the sea ice. Brine content in the ice varies strongly with temperature, and may be the cause of the large variations in the transport of carbon dioxide. A late spring observation of bubbles from rotting sea ice disclosed very high levels of carbon monoxide. Observations of the atmosphere over sea ice (to 78 degrees N) through the summer tends to confirm a continued high atmospheric level of CO2 beyond the time period when it diminishes at Point Barrow, Alaska (71.4 degrees N). Original contains color plates: All DDC reproductions will be in black and white. Text Barrow Ice permafrost Point Barrow Sea ice Alaska Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
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English |
topic |
Snow Ice and Permafrost *GASES *SEA ICE STRESSES TEMPERATURE AIR DYNAMICS INTERFACES CARBON MONOXIDE CARBON DIOXIDE |
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Snow Ice and Permafrost *GASES *SEA ICE STRESSES TEMPERATURE AIR DYNAMICS INTERFACES CARBON MONOXIDE CARBON DIOXIDE Gosink,Thomas A Kelley,John J Gases in Sea Ice: A Factor Bearing on the Transmission of Sound Energy. |
topic_facet |
Snow Ice and Permafrost *GASES *SEA ICE STRESSES TEMPERATURE AIR DYNAMICS INTERFACES CARBON MONOXIDE CARBON DIOXIDE |
description |
This research is a continuation of the previous year's work on the migration of gases through sea ice and the transport of gases across the ice-snow-air boundary. Carbon dioxide, and possibly carbon monoxide, were observed to be replenished faster than other non-water interacting gases such as nitrogen, oxygen, neon, and methane in flushed probe holes and at the surface. Large pulses of carbon dioxide were observed and suspected as the result of internal stresses in sea ice. The flux of gases in probe holes was near 2-4 microliter/sq cm/hr, and 1-2 microliter/sq cm/hr at the surface, relatively insignificant for oxygen, but very significant for trace gases such as carbon dioxide. The ocean was observed to be a source of carbon dioxide, carbon monoxide and methane to the atmosphere by way of the sea ice. Brine content in the ice varies strongly with temperature, and may be the cause of the large variations in the transport of carbon dioxide. A late spring observation of bubbles from rotting sea ice disclosed very high levels of carbon monoxide. Observations of the atmosphere over sea ice (to 78 degrees N) through the summer tends to confirm a continued high atmospheric level of CO2 beyond the time period when it diminishes at Point Barrow, Alaska (71.4 degrees N). Original contains color plates: All DDC reproductions will be in black and white. |
author2 |
ALASKA UNIV COLLEGE INST OF MARINE SCIENCE |
format |
Text |
author |
Gosink,Thomas A Kelley,John J |
author_facet |
Gosink,Thomas A Kelley,John J |
author_sort |
Gosink,Thomas A |
title |
Gases in Sea Ice: A Factor Bearing on the Transmission of Sound Energy. |
title_short |
Gases in Sea Ice: A Factor Bearing on the Transmission of Sound Energy. |
title_full |
Gases in Sea Ice: A Factor Bearing on the Transmission of Sound Energy. |
title_fullStr |
Gases in Sea Ice: A Factor Bearing on the Transmission of Sound Energy. |
title_full_unstemmed |
Gases in Sea Ice: A Factor Bearing on the Transmission of Sound Energy. |
title_sort |
gases in sea ice: a factor bearing on the transmission of sound energy. |
publishDate |
1977 |
url |
http://www.dtic.mil/docs/citations/ADA056115 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA056115 |
genre |
Barrow Ice permafrost Point Barrow Sea ice Alaska |
genre_facet |
Barrow Ice permafrost Point Barrow Sea ice Alaska |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA056115 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
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1766371783175307264 |