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Please use this identifier to cite or link to this item: http://192.168.1.231:8080/dulieusoDHQB_123456789/3770
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dc.contributor.authorCueva, David Avalos-
dc.contributor.authorHernández, Emilio Palacios-
dc.contributor.authorCarrillo, Laura-
dc.contributor.authorVivanco, Luis A. González-
dc.date.accessioned2018-08-02T02:06:35Z-
dc.date.available2018-08-02T02:06:35Z-
dc.date.issued2017-
dc.identifier.urihttp://lrc.quangbinhuni.edu.vn:8181/dspace/handle/DHQB_123456789/3770-
dc.description.abstract.In this study performed the simulation of currents generated by the wind on the Bay of Chetumal, Quintana Roo through the use of a stationary shallow-water model. A homogeneous climatic wind was used for the entire Bay, with a velocity of 3m·s-1 , and directions North, South, Northeast, Northwest, East, Southeast, Southwest and West. The results showed a rather complex dynamics in Chetumal Bay, in which important turns were observed in deep areas, with speeds reaching up to 13 cm·s-1 .en_US
dc.publisherUniversidad Autónoma Indígena de Méxicoen_US
dc.subjectSocial Sciencesen_US
dc.subjectShallow water mode;currents, winden_US
dc.subjectnumerical simulationen_US
dc.titleNUMERICAL MODELS AS TOOLS TO UNDERSTAND THE DYNAMICS IN BAYS: CASE OF STUDY CHETUMAL BAY, QUINTANA ROOen_US
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