Moored observations of shelfbreak processes at the inflow to and outflow from the Arctic Ocean
Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution February 2013 Two high-resolution mooring arrays extending from the outer shelf to the mid continental slope are used...
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Massachusetts Institute of Technology and Woods Hole Oceanographic Institution
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/5822 2023-05-15T14:29:02+02:00 Moored observations of shelfbreak processes at the inflow to and outflow from the Arctic Ocean von Appen, Wilken-Jon 152°W Arctic Ocean Beaufort Sea 65°N Denmark Strait 2013-02 application/pdf https://hdl.handle.net/1912/5822 en_US eng Massachusetts Institute of Technology and Woods Hole Oceanographic Institution WHOI Theses https://hdl.handle.net/1912/5822 doi:10.1575/1912/5822 doi:10.1575/1912/5822 Ocean currents Deep-sea moorings Oceanus (Ship : 1975-) Cruise OC369 Thesis 2013 ftwhoas https://doi.org/10.1575/1912/5822 2022-05-28T22:58:49Z Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution February 2013 Two high-resolution mooring arrays extending from the outer shelf to the mid continental slope are used to elucidate shelf-basin exchange at the inflow to and the outflow from the Arctic Ocean. Pacific Water entering the Arctic Ocean forms the Western Arctic shelfbreak current along the Beaufort Sea slope. Data from the mooring array at 152°W—approximately 150 km east of Pt. Barrow, AK—reveals that this current has two distinct states in summer depending on the water mass it transports. When advecting Alaskan Coastal Water it is surface-intensified and both baroclinically and barotropically unstable. This configuration lasts about a month with an average transport of 0.7 Sv. When advecting Chukchi Summer Water the current is bottom-intensified and is only baroclinically unstable. This state also exists for approximately a month with an average transport of 0.6 Sv. The strong mean-to-eddy energy conversion causes both configurations of the current to spin down over a distance of a few hundred kilometers, suggesting that warm Pacific Water does not enter the Canadian Arctic Archipelago via this route. Dense water formed in the Nordic Seas overflows the Denmark Strait and undergoes vortex stretching, forming intense cyclones that propagate along the East Greenland slope. Data from the mooring array at 65°N—roughly 300 km downstream of Denmark Strait—was used to determine the full water column structure of the cyclones. On average a cyclone passes the array every other day in the vicinity of the 900 m isobath, although the depth range of individual cyclones ranges between the 500 m and 1600 m isobaths. The cyclones self-propagate at 0.45 m/s and are also advected by the mean flow of 0.27 m/s, resulting in a total propagation speed of 0.72 m/s. They have a peak azimuthal speed of 0.22 m/s at a radius of 7.8 km and contain ... Thesis Arctic Archipelago Arctic Arctic Ocean Beaufort Sea Canadian Arctic Archipelago Chukchi Denmark Strait East Greenland Greenland Nordic Seas Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Arctic Arctic Ocean Canadian Arctic Archipelago Greenland Pacific Woods Hole, MA |
institution |
Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
topic |
Ocean currents Deep-sea moorings Oceanus (Ship : 1975-) Cruise OC369 |
spellingShingle |
Ocean currents Deep-sea moorings Oceanus (Ship : 1975-) Cruise OC369 von Appen, Wilken-Jon Moored observations of shelfbreak processes at the inflow to and outflow from the Arctic Ocean |
topic_facet |
Ocean currents Deep-sea moorings Oceanus (Ship : 1975-) Cruise OC369 |
description |
Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution February 2013 Two high-resolution mooring arrays extending from the outer shelf to the mid continental slope are used to elucidate shelf-basin exchange at the inflow to and the outflow from the Arctic Ocean. Pacific Water entering the Arctic Ocean forms the Western Arctic shelfbreak current along the Beaufort Sea slope. Data from the mooring array at 152°W—approximately 150 km east of Pt. Barrow, AK—reveals that this current has two distinct states in summer depending on the water mass it transports. When advecting Alaskan Coastal Water it is surface-intensified and both baroclinically and barotropically unstable. This configuration lasts about a month with an average transport of 0.7 Sv. When advecting Chukchi Summer Water the current is bottom-intensified and is only baroclinically unstable. This state also exists for approximately a month with an average transport of 0.6 Sv. The strong mean-to-eddy energy conversion causes both configurations of the current to spin down over a distance of a few hundred kilometers, suggesting that warm Pacific Water does not enter the Canadian Arctic Archipelago via this route. Dense water formed in the Nordic Seas overflows the Denmark Strait and undergoes vortex stretching, forming intense cyclones that propagate along the East Greenland slope. Data from the mooring array at 65°N—roughly 300 km downstream of Denmark Strait—was used to determine the full water column structure of the cyclones. On average a cyclone passes the array every other day in the vicinity of the 900 m isobath, although the depth range of individual cyclones ranges between the 500 m and 1600 m isobaths. The cyclones self-propagate at 0.45 m/s and are also advected by the mean flow of 0.27 m/s, resulting in a total propagation speed of 0.72 m/s. They have a peak azimuthal speed of 0.22 m/s at a radius of 7.8 km and contain ... |
format |
Thesis |
author |
von Appen, Wilken-Jon |
author_facet |
von Appen, Wilken-Jon |
author_sort |
von Appen, Wilken-Jon |
title |
Moored observations of shelfbreak processes at the inflow to and outflow from the Arctic Ocean |
title_short |
Moored observations of shelfbreak processes at the inflow to and outflow from the Arctic Ocean |
title_full |
Moored observations of shelfbreak processes at the inflow to and outflow from the Arctic Ocean |
title_fullStr |
Moored observations of shelfbreak processes at the inflow to and outflow from the Arctic Ocean |
title_full_unstemmed |
Moored observations of shelfbreak processes at the inflow to and outflow from the Arctic Ocean |
title_sort |
moored observations of shelfbreak processes at the inflow to and outflow from the arctic ocean |
publisher |
Massachusetts Institute of Technology and Woods Hole Oceanographic Institution |
publishDate |
2013 |
url |
https://hdl.handle.net/1912/5822 |
op_coverage |
152°W Arctic Ocean Beaufort Sea 65°N Denmark Strait |
geographic |
Arctic Arctic Ocean Canadian Arctic Archipelago Greenland Pacific |
geographic_facet |
Arctic Arctic Ocean Canadian Arctic Archipelago Greenland Pacific |
genre |
Arctic Archipelago Arctic Arctic Ocean Beaufort Sea Canadian Arctic Archipelago Chukchi Denmark Strait East Greenland Greenland Nordic Seas |
genre_facet |
Arctic Archipelago Arctic Arctic Ocean Beaufort Sea Canadian Arctic Archipelago Chukchi Denmark Strait East Greenland Greenland Nordic Seas |
op_source |
doi:10.1575/1912/5822 |
op_relation |
WHOI Theses https://hdl.handle.net/1912/5822 doi:10.1575/1912/5822 |
op_doi |
https://doi.org/10.1575/1912/5822 |
op_publisher_place |
Woods Hole, MA |
_version_ |
1766303142764347392 |