An analysis of hydrographic data collected off Point Sur, California in June 1990

The data collected in June 1990 from the R/V Point Sur are used to study the California Undercurrent and California Current in the area off Point Sur. The area of study is a coastal region starting 3 km off Point Sur and extending westward 102 km. At that distance the orientation of the line of the...

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Main Author: Tziagidia, Georgios Th.
Other Authors: Garfield, Newell, Naval Postgraduate School (U.S.), Oceanography, Collins, Curtis A.
Format: Thesis
Language:English
Published: Monterey, California. Naval Postgraduate School 1991
Subjects:
Online Access:https://hdl.handle.net/10945/27963
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spelling ftnavalpschool:oai:calhoun.nps.edu:10945/27963 2024-06-09T07:49:51+00:00 An analysis of hydrographic data collected off Point Sur, California in June 1990 Tziagidia, Georgios Th. Garfield, Newell Naval Postgraduate School (U.S.) Oceanography Collins, Curtis A. 1991-09 application/pdf https://hdl.handle.net/10945/27963 en_US eng Monterey, California. Naval Postgraduate School https://hdl.handle.net/10945/27963 Copyright is reserved by the copyright owner California Undercurrent Current June 1990 Thesis 1991 ftnavalpschool 2024-05-15T00:54:32Z The data collected in June 1990 from the R/V Point Sur are used to study the California Undercurrent and California Current in the area off Point Sur. The area of study is a coastal region starting 3 km off Point Sur and extending westward 102 km. At that distance the orientation of the line of the stations changes to southwest, extending to 228 km offshore. The cruise took place from 16-22 of June under upwelling favorable weather conditions. The results of this study help illustrate the great variability of the currents in the area. In June 1990 the California Undercurrent exists, is strong (max speed is 36 cm/sec), is confined to the first 65 km from the shore, and carries equatorial type waters northward in depths less that 650 dbars. the estimated transport is 2.9 Sv. the California Current is broad, slower than the Undercurrent (max speed 28 cm/sec), shallower and carries Subarctic North Pacific waters. The coastal upwelling looks strong starting from the depth of 100 dbars, and contributes to the inshore coastal jet which it is observed in the first 8 km from the shore and in the upper 20 dbars. Unlike previous analyses based on CalCOFI data, the Undercurrent appears robust in June. Its strong surface and subsurface signature had not previously been reported for this month. This may be in part due to the determination made in this thesis that 700 dbar is a more appropriate reference level than either 500 or 1000 dbar. Approved for public release; distribution is unlimited. Lieutenant, Hellenic Navy http://archive.org/details/annalysisofhydro1094527963 Thesis Subarctic Naval Postgraduate School: Calhoun Pacific
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language English
topic California Undercurrent
Current
June 1990
spellingShingle California Undercurrent
Current
June 1990
Tziagidia, Georgios Th.
An analysis of hydrographic data collected off Point Sur, California in June 1990
topic_facet California Undercurrent
Current
June 1990
description The data collected in June 1990 from the R/V Point Sur are used to study the California Undercurrent and California Current in the area off Point Sur. The area of study is a coastal region starting 3 km off Point Sur and extending westward 102 km. At that distance the orientation of the line of the stations changes to southwest, extending to 228 km offshore. The cruise took place from 16-22 of June under upwelling favorable weather conditions. The results of this study help illustrate the great variability of the currents in the area. In June 1990 the California Undercurrent exists, is strong (max speed is 36 cm/sec), is confined to the first 65 km from the shore, and carries equatorial type waters northward in depths less that 650 dbars. the estimated transport is 2.9 Sv. the California Current is broad, slower than the Undercurrent (max speed 28 cm/sec), shallower and carries Subarctic North Pacific waters. The coastal upwelling looks strong starting from the depth of 100 dbars, and contributes to the inshore coastal jet which it is observed in the first 8 km from the shore and in the upper 20 dbars. Unlike previous analyses based on CalCOFI data, the Undercurrent appears robust in June. Its strong surface and subsurface signature had not previously been reported for this month. This may be in part due to the determination made in this thesis that 700 dbar is a more appropriate reference level than either 500 or 1000 dbar. Approved for public release; distribution is unlimited. Lieutenant, Hellenic Navy http://archive.org/details/annalysisofhydro1094527963
author2 Garfield, Newell
Naval Postgraduate School (U.S.)
Oceanography
Collins, Curtis A.
format Thesis
author Tziagidia, Georgios Th.
author_facet Tziagidia, Georgios Th.
author_sort Tziagidia, Georgios Th.
title An analysis of hydrographic data collected off Point Sur, California in June 1990
title_short An analysis of hydrographic data collected off Point Sur, California in June 1990
title_full An analysis of hydrographic data collected off Point Sur, California in June 1990
title_fullStr An analysis of hydrographic data collected off Point Sur, California in June 1990
title_full_unstemmed An analysis of hydrographic data collected off Point Sur, California in June 1990
title_sort analysis of hydrographic data collected off point sur, california in june 1990
publisher Monterey, California. Naval Postgraduate School
publishDate 1991
url https://hdl.handle.net/10945/27963
geographic Pacific
geographic_facet Pacific
genre Subarctic
genre_facet Subarctic
op_relation https://hdl.handle.net/10945/27963
op_rights Copyright is reserved by the copyright owner
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