Ocean‐to‐ice heat flux at the North Pole environmental observatory
The article of record as published may be found at http://dx.doi.org/10.1029/2003GL018580 Data from drifting buoys deployed in April, 2002, as part of the North Pole Environmental Observatory project have been analysed to estimate ocean heat flux in the time period from 1 May 2002 to 11 Mar 2003. Pr...
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American Geophysical Union
2003
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ftnavalpschool:oai:calhoun.nps.edu:10945/61579 2024-06-09T07:41:08+00:00 Ocean‐to‐ice heat flux at the North Pole environmental observatory McPhee, Miles G. Kikuchi, Takashi Morison, James H. Stanton, Timothy P. Naval Postgraduate School (U.S.) 2003-12 5 p. application/pdf https://hdl.handle.net/10945/61579 unknown American Geophysical Union McPhee, Miles G., et al. "Ocean‐to‐ice heat flux at the North Pole environmental observatory." Geophysical Research Letters 30.24 (2003). https://hdl.handle.net/10945/61579 This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. 4540 Oceanography Physical Ice mechanics and air/sea/ice exchange processes 4207 Oceanography General Arctic and Antarctic oceanography 4568 Oceanography Turbulence Upper ocean processes 4594 Oceanography Instruments and techniques Article 2003 ftnavalpschool 2024-05-15T00:52:29Z The article of record as published may be found at http://dx.doi.org/10.1029/2003GL018580 Data from drifting buoys deployed in April, 2002, as part of the North Pole Environmental Observatory project have been analysed to estimate ocean heat flux in the time period from 1 May 2002 to 11 Mar 2003. Prior to late January, the observatory remained in deep water, but subsequently drifted directly over the Yermak Plateau, a relatively shallow feature north of Svalbard. While over deep water, heat flux was dominated by storage and release of solar energy in the ocean boundary layer during summer. The most likely annual average value for 2002 was 2.6 W mˉ2, less than previous determinations in the western Arctic. Over Yermak Plateau, heat flux at the interface came from mixing of warmer water into the boundary layer from below. When the observatory was in water with depths less than 1200 m, the average heat flux was around 22 W mˉ2. OPP-9910305 OPP-0084858 OPP-008426 Arctic Ocean Research Project of JAMSTEC NSF Article in Journal/Newspaper Antarc* Antarctic Arctic Arctic Ocean North Pole Sea ice Svalbard Yermak plateau Naval Postgraduate School: Calhoun Antarctic Arctic Arctic Ocean North Pole Svalbard Yermak Plateau ENVELOPE(5.000,5.000,81.250,81.250) |
institution |
Open Polar |
collection |
Naval Postgraduate School: Calhoun |
op_collection_id |
ftnavalpschool |
language |
unknown |
topic |
4540 Oceanography Physical Ice mechanics and air/sea/ice exchange processes 4207 Oceanography General Arctic and Antarctic oceanography 4568 Oceanography Turbulence Upper ocean processes 4594 Oceanography Instruments and techniques |
spellingShingle |
4540 Oceanography Physical Ice mechanics and air/sea/ice exchange processes 4207 Oceanography General Arctic and Antarctic oceanography 4568 Oceanography Turbulence Upper ocean processes 4594 Oceanography Instruments and techniques McPhee, Miles G. Kikuchi, Takashi Morison, James H. Stanton, Timothy P. Ocean‐to‐ice heat flux at the North Pole environmental observatory |
topic_facet |
4540 Oceanography Physical Ice mechanics and air/sea/ice exchange processes 4207 Oceanography General Arctic and Antarctic oceanography 4568 Oceanography Turbulence Upper ocean processes 4594 Oceanography Instruments and techniques |
description |
The article of record as published may be found at http://dx.doi.org/10.1029/2003GL018580 Data from drifting buoys deployed in April, 2002, as part of the North Pole Environmental Observatory project have been analysed to estimate ocean heat flux in the time period from 1 May 2002 to 11 Mar 2003. Prior to late January, the observatory remained in deep water, but subsequently drifted directly over the Yermak Plateau, a relatively shallow feature north of Svalbard. While over deep water, heat flux was dominated by storage and release of solar energy in the ocean boundary layer during summer. The most likely annual average value for 2002 was 2.6 W mˉ2, less than previous determinations in the western Arctic. Over Yermak Plateau, heat flux at the interface came from mixing of warmer water into the boundary layer from below. When the observatory was in water with depths less than 1200 m, the average heat flux was around 22 W mˉ2. OPP-9910305 OPP-0084858 OPP-008426 Arctic Ocean Research Project of JAMSTEC NSF |
author2 |
Naval Postgraduate School (U.S.) |
format |
Article in Journal/Newspaper |
author |
McPhee, Miles G. Kikuchi, Takashi Morison, James H. Stanton, Timothy P. |
author_facet |
McPhee, Miles G. Kikuchi, Takashi Morison, James H. Stanton, Timothy P. |
author_sort |
McPhee, Miles G. |
title |
Ocean‐to‐ice heat flux at the North Pole environmental observatory |
title_short |
Ocean‐to‐ice heat flux at the North Pole environmental observatory |
title_full |
Ocean‐to‐ice heat flux at the North Pole environmental observatory |
title_fullStr |
Ocean‐to‐ice heat flux at the North Pole environmental observatory |
title_full_unstemmed |
Ocean‐to‐ice heat flux at the North Pole environmental observatory |
title_sort |
ocean‐to‐ice heat flux at the north pole environmental observatory |
publisher |
American Geophysical Union |
publishDate |
2003 |
url |
https://hdl.handle.net/10945/61579 |
long_lat |
ENVELOPE(5.000,5.000,81.250,81.250) |
geographic |
Antarctic Arctic Arctic Ocean North Pole Svalbard Yermak Plateau |
geographic_facet |
Antarctic Arctic Arctic Ocean North Pole Svalbard Yermak Plateau |
genre |
Antarc* Antarctic Arctic Arctic Ocean North Pole Sea ice Svalbard Yermak plateau |
genre_facet |
Antarc* Antarctic Arctic Arctic Ocean North Pole Sea ice Svalbard Yermak plateau |
op_relation |
McPhee, Miles G., et al. "Ocean‐to‐ice heat flux at the North Pole environmental observatory." Geophysical Research Letters 30.24 (2003). https://hdl.handle.net/10945/61579 |
op_rights |
This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. |
_version_ |
1801369560457150464 |