The Effect of Bathymetry Changes on Major Oceanic Currents and Overturning Circulations
dc.rights.license | CC-BY-NC-ND | |
dc.contributor.advisor | von der Heydt, dr. A.S. | |
dc.contributor.author | Voorneveld, M.D. | |
dc.date.accessioned | 2020-07-21T18:00:29Z | |
dc.date.available | 2020-07-21T18:00:29Z | |
dc.date.issued | 2020 | |
dc.identifier.uri | https://studenttheses.uu.nl/handle/20.500.12932/36239 | |
dc.description.abstract | We 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.sponsorship | Utrecht University | |
dc.format.extent | 31965790 | |
dc.format.mimetype | application/pdf | |
dc.language.iso | en | |
dc.title | The Effect of Bathymetry Changes on Major Oceanic Currents and Overturning Circulations | |
dc.type.content | Bachelor Thesis | |
dc.rights.accessrights | Open Access | |
dc.subject.keywords | Thetys, GCM, Veros, UU, panama passage, Miocene, Pliocene, Eocene, Meridional overturning circulation, major ocean, IMAU, Marte, Voorneveld, NAST | |
dc.subject.courseuu | Natuur- en Sterrenkunde |