Please use this identifier to cite or link to this item: http://localhost/handle/Hannan/240140
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dc.contributor.authorSteven Michael Jachecen_US
dc.date.accessioned2013en_US
dc.date.accessioned2020-04-06T09:59:41Z-
dc.date.available2020-04-06T09:59:41Z-
dc.date.issued2008en_US
dc.identifier.urihttp://localhost/handle/Hannan/240140-
dc.description.abstractTraditionally, it has been viewed that tides dissipate 2.6 TW over the continentalshelves via the shallow bottom boundary layer, and have little impact on deep oceanmixing (Munk & Wunsch, 1998). Through their tidal maps, Egbert & Ray (2001)have confirmed that while most energy is lost in the shallow sea, nearly 1 TW isen_US
dc.relation.haspartTL72294.pdfen_US
dc.titleUNDERSTANDING THE EVOLUTION AND ENERGETICS OF INTERNAL TIDES WITHIN MONTEREY BAY VIA NUMERICAL SIMULATIONSen_US
dc.typeThesisen_US
Appears in Collections:Thesis

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Full metadata record
DC FieldValueLanguage
dc.contributor.authorSteven Michael Jachecen_US
dc.date.accessioned2013en_US
dc.date.accessioned2020-04-06T09:59:41Z-
dc.date.available2020-04-06T09:59:41Z-
dc.date.issued2008en_US
dc.identifier.urihttp://localhost/handle/Hannan/240140-
dc.description.abstractTraditionally, it has been viewed that tides dissipate 2.6 TW over the continentalshelves via the shallow bottom boundary layer, and have little impact on deep oceanmixing (Munk & Wunsch, 1998). Through their tidal maps, Egbert & Ray (2001)have confirmed that while most energy is lost in the shallow sea, nearly 1 TW isen_US
dc.relation.haspartTL72294.pdfen_US
dc.titleUNDERSTANDING THE EVOLUTION AND ENERGETICS OF INTERNAL TIDES WITHIN MONTEREY BAY VIA NUMERICAL SIMULATIONSen_US
dc.typeThesisen_US
Appears in Collections:Thesis

Files in This Item:
File Description SizeFormat 
TL72294.pdf6.82 MBAdobe PDFThumbnail
Preview File
Full metadata record
DC FieldValueLanguage
dc.contributor.authorSteven Michael Jachecen_US
dc.date.accessioned2013en_US
dc.date.accessioned2020-04-06T09:59:41Z-
dc.date.available2020-04-06T09:59:41Z-
dc.date.issued2008en_US
dc.identifier.urihttp://localhost/handle/Hannan/240140-
dc.description.abstractTraditionally, it has been viewed that tides dissipate 2.6 TW over the continentalshelves via the shallow bottom boundary layer, and have little impact on deep oceanmixing (Munk & Wunsch, 1998). Through their tidal maps, Egbert & Ray (2001)have confirmed that while most energy is lost in the shallow sea, nearly 1 TW isen_US
dc.relation.haspartTL72294.pdfen_US
dc.titleUNDERSTANDING THE EVOLUTION AND ENERGETICS OF INTERNAL TIDES WITHIN MONTEREY BAY VIA NUMERICAL SIMULATIONSen_US
dc.typeThesisen_US
Appears in Collections:Thesis

Files in This Item:
File Description SizeFormat 
TL72294.pdf6.82 MBAdobe PDFThumbnail
Preview File