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dc.rights.licenseCC-BY-NC-ND
dc.contributor.advisorvon der Heydt, dr. A.S.
dc.contributor.authorVoorneveld, M.D.
dc.date.accessioned2020-07-21T18:00:29Z
dc.date.available2020-07-21T18:00:29Z
dc.date.issued2020
dc.identifier.urihttps://studenttheses.uu.nl/handle/20.500.12932/36239
dc.description.abstractWe investigate the effect of changing geometries in a simple ocean general circulation model. Using highly idealized forcings we compare the situations for every 5 Million years (Ma) time step from 65Ma to the present-day situation. The present-day simulation was used as a control. The model result shows a reversal of the flow through the Panama Seaway in the early Miocene coinciding with the closure of the Thetys seaway. We also observe a system that is sensitive to the position of the Indian Continent in the Paleocene. Furthermore, we observe large differences in the thermohaline circulations in comparison to the present-day situation. Also, significant temperature fluctuations are observed in the Eocene-Oligocene boundary.
dc.description.sponsorshipUtrecht University
dc.format.extent31965790
dc.format.mimetypeapplication/pdf
dc.language.isoen
dc.titleThe Effect of Bathymetry Changes on Major Oceanic Currents and Overturning Circulations
dc.type.contentBachelor Thesis
dc.rights.accessrightsOpen Access
dc.subject.keywordsThetys, GCM, Veros, UU, panama passage, Miocene, Pliocene, Eocene, Meridional overturning circulation, major ocean, IMAU, Marte, Voorneveld, NAST
dc.subject.courseuuNatuur- en Sterrenkunde


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