On the variability of the Antarctic Circumpolar Current
Typescript (photocopy). A time series of net transport during 1979 of the Antarctic Circumpolar Current through the upper 2500 m of Drake Passage was obtained as part of the International Southern Ocean Studies by Whitworth (1983), and was presented in corrected form by Whitworth and Peterson (1985)...
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1987
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fttexasamuniv:oai:oaktrust.library.tamu.edu:1969.1/DISSERTATIONS-754235 2023-07-16T03:52:55+02:00 On the variability of the Antarctic Circumpolar Current Peterson, Ray George Nowlin, Worth D. Kattawar, George W. Ichiye, Takashi McGuirk, James P. Reid, Robert O. 1987 xiv, 97 leaves electronic application/pdf reformatted digital https://hdl.handle.net/1969.1/DISSERTATIONS-754235 eng eng Texas A&M University. Libraries https://hdl.handle.net/1969.1/DISSERTATIONS-754235 18942506 This thesis was part of a retrospective digitization project authorized by the Texas A&M University Libraries. Copyright remains vested with the author(s). It is the user's responsibility to secure permission from the copyright holder(s) for re-use of the work beyond the provision of Fair Use. http://rightsstatements.org/vocab/InC/1.0/ Major oceanography 1987 Dissertation P4855 Ocean-atmosphere interaction Ocean currents Antarctic Ocean Ocean circulation Thesis dissertations text 1987 fttexasamuniv 2023-06-27T23:04:22Z Typescript (photocopy). A time series of net transport during 1979 of the Antarctic Circumpolar Current through the upper 2500 m of Drake Passage was obtained as part of the International Southern Ocean Studies by Whitworth (1983), and was presented in corrected form by Whitworth and Peterson (1985). Spectral analyses are performed on records comprising the corrected series to determine the major sources for transport variability, and measurements from bottom pressure gauges at each side of the passage are used to extend the year-long series of transport, are related to fields of wind stress, and are compared with sea level observations. The net transport series is dominated in the sub-seasonal time scales by the lunar fortnightly and monthly tides and by baroclinic activity in the northern passage, processes that are independent of wind. Although the long-period lunar tides were included in the geostrophic calculations, the actual transport responses are probably ageostrophic. For seasonal time scales, transport variability is mainly barotropic, thereby allowing the use of bottom pressure records for extending the series. An extended transport series, spanning three continuous years plus an additional year, shows that seasonal changes approaching 40x10⁶ m³ s⁻¹ can occur in time intervals shorter than two months, and that the seasonal signals are not phase-locked. Seasonal fluctuations of bottom pressure at each side of the passage are consistent with what might result from changes in Sverdrup mass transport across the perimeters of the current as induced by variations in strength of the southern hemisphere subtropical and subpolar atmospheric systems. Synthetic subsurface pressure (SSP) derived from tidal and atmospheric sea level pressure series from the British Antarctic Survey base Faraday compares well with bottom pressure from the southern Drake Passage, and indicates the presence of the 18.6-year lunar nodal tide. SSP from Puerto Williams, Chile does not compare well with bottom pressure from the ... Thesis Antarc* Antarctic Antarctic Ocean British Antarctic Survey Drake Passage Southern Ocean Texas A&M University Digital Repository Antarctic Southern Ocean The Antarctic Drake Passage Antarctic Ocean Faraday ENVELOPE(-64.256,-64.256,-65.246,-65.246) |
institution |
Open Polar |
collection |
Texas A&M University Digital Repository |
op_collection_id |
fttexasamuniv |
language |
English |
topic |
Major oceanography 1987 Dissertation P4855 Ocean-atmosphere interaction Ocean currents Antarctic Ocean Ocean circulation |
spellingShingle |
Major oceanography 1987 Dissertation P4855 Ocean-atmosphere interaction Ocean currents Antarctic Ocean Ocean circulation Peterson, Ray George On the variability of the Antarctic Circumpolar Current |
topic_facet |
Major oceanography 1987 Dissertation P4855 Ocean-atmosphere interaction Ocean currents Antarctic Ocean Ocean circulation |
description |
Typescript (photocopy). A time series of net transport during 1979 of the Antarctic Circumpolar Current through the upper 2500 m of Drake Passage was obtained as part of the International Southern Ocean Studies by Whitworth (1983), and was presented in corrected form by Whitworth and Peterson (1985). Spectral analyses are performed on records comprising the corrected series to determine the major sources for transport variability, and measurements from bottom pressure gauges at each side of the passage are used to extend the year-long series of transport, are related to fields of wind stress, and are compared with sea level observations. The net transport series is dominated in the sub-seasonal time scales by the lunar fortnightly and monthly tides and by baroclinic activity in the northern passage, processes that are independent of wind. Although the long-period lunar tides were included in the geostrophic calculations, the actual transport responses are probably ageostrophic. For seasonal time scales, transport variability is mainly barotropic, thereby allowing the use of bottom pressure records for extending the series. An extended transport series, spanning three continuous years plus an additional year, shows that seasonal changes approaching 40x10⁶ m³ s⁻¹ can occur in time intervals shorter than two months, and that the seasonal signals are not phase-locked. Seasonal fluctuations of bottom pressure at each side of the passage are consistent with what might result from changes in Sverdrup mass transport across the perimeters of the current as induced by variations in strength of the southern hemisphere subtropical and subpolar atmospheric systems. Synthetic subsurface pressure (SSP) derived from tidal and atmospheric sea level pressure series from the British Antarctic Survey base Faraday compares well with bottom pressure from the southern Drake Passage, and indicates the presence of the 18.6-year lunar nodal tide. SSP from Puerto Williams, Chile does not compare well with bottom pressure from the ... |
author2 |
Nowlin, Worth D. Kattawar, George W. Ichiye, Takashi McGuirk, James P. Reid, Robert O. |
format |
Thesis |
author |
Peterson, Ray George |
author_facet |
Peterson, Ray George |
author_sort |
Peterson, Ray George |
title |
On the variability of the Antarctic Circumpolar Current |
title_short |
On the variability of the Antarctic Circumpolar Current |
title_full |
On the variability of the Antarctic Circumpolar Current |
title_fullStr |
On the variability of the Antarctic Circumpolar Current |
title_full_unstemmed |
On the variability of the Antarctic Circumpolar Current |
title_sort |
on the variability of the antarctic circumpolar current |
publisher |
Texas A&M University. Libraries |
publishDate |
1987 |
url |
https://hdl.handle.net/1969.1/DISSERTATIONS-754235 |
long_lat |
ENVELOPE(-64.256,-64.256,-65.246,-65.246) |
geographic |
Antarctic Southern Ocean The Antarctic Drake Passage Antarctic Ocean Faraday |
geographic_facet |
Antarctic Southern Ocean The Antarctic Drake Passage Antarctic Ocean Faraday |
genre |
Antarc* Antarctic Antarctic Ocean British Antarctic Survey Drake Passage Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctic Ocean British Antarctic Survey Drake Passage Southern Ocean |
op_relation |
https://hdl.handle.net/1969.1/DISSERTATIONS-754235 18942506 |
op_rights |
This thesis was part of a retrospective digitization project authorized by the Texas A&M University Libraries. Copyright remains vested with the author(s). It is the user's responsibility to secure permission from the copyright holder(s) for re-use of the work beyond the provision of Fair Use. http://rightsstatements.org/vocab/InC/1.0/ |
_version_ |
1771547673977946112 |