DIECAST model simulation of the California coastal zone
The high resolution DIECAST ocean model is used to simulate mesoscale variability in the California coastal zone. This simulation uses realistic topography and coastal geometry with boundary forcing only in the form of an equatorward-flowing jet, structured after observations, imposed at the norther...
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Monterey, California. Naval Postgraduate School
2012
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ndltd-nps.edu-oai-calhoun.nps.edu-10945-75552014-11-27T16:07:02Z DIECAST model simulation of the California coastal zone Akahoshi, Stanley A. Haney, Robert Meteorology and Physical Oceanography The high resolution DIECAST ocean model is used to simulate mesoscale variability in the California coastal zone. This simulation uses realistic topography and coastal geometry with boundary forcing only in the form of an equatorward-flowing jet, structured after observations, imposed at the northern boundary. The mesoscale features produced by the model are qualitatively consistent with those seen in observations. Their spatial scales are somewhat larger and their intensities somewhat weaker than in observations. The jet imposed at the northern boundary increases in horizontal and vertical scale as it meanders south through the domain. Cyclones and anticyclones are shown to have preferred locations and a general tendency for non-steady southwestward propagation with a phase speed of about 10 cm/s. 2012-07-31T19:54:23Z 2012-07-31T19:54:23Z 1995-09 Thesis http://hdl.handle.net/10945/7555 en_US This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. As such, it is in the public domain, and under the provisions of Title 17, United States Code, Section 105, it may not be copyrighted. Monterey, California. Naval Postgraduate School |
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en_US |
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description |
The high resolution DIECAST ocean model is used to simulate mesoscale variability in the California coastal zone. This simulation uses realistic topography and coastal geometry with boundary forcing only in the form of an equatorward-flowing jet, structured after observations, imposed at the northern boundary. The mesoscale features produced by the model are qualitatively consistent with those seen in observations. Their spatial scales are somewhat larger and their intensities somewhat weaker than in observations. The jet imposed at the northern boundary increases in horizontal and vertical scale as it meanders south through the domain. Cyclones and anticyclones are shown to have preferred locations and a general tendency for non-steady southwestward propagation with a phase speed of about 10 cm/s. |
author2 |
Haney, Robert |
author_facet |
Haney, Robert Akahoshi, Stanley A. |
author |
Akahoshi, Stanley A. |
spellingShingle |
Akahoshi, Stanley A. DIECAST model simulation of the California coastal zone |
author_sort |
Akahoshi, Stanley A. |
title |
DIECAST model simulation of the California coastal zone |
title_short |
DIECAST model simulation of the California coastal zone |
title_full |
DIECAST model simulation of the California coastal zone |
title_fullStr |
DIECAST model simulation of the California coastal zone |
title_full_unstemmed |
DIECAST model simulation of the California coastal zone |
title_sort |
diecast model simulation of the california coastal zone |
publisher |
Monterey, California. Naval Postgraduate School |
publishDate |
2012 |
url |
http://hdl.handle.net/10945/7555 |
work_keys_str_mv |
AT akahoshistanleya diecastmodelsimulationofthecaliforniacoastalzone |
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1716721145062883328 |