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A Numerical Simulation of the Martian Polar Cap Breeze

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dc.creatorFernández Rojas, Walter
dc.date.accessioned2023-08-11T14:27:20Z
dc.date.available2023-08-11T14:27:20Z
dc.date.issued1995
dc.description.abstractA mathematical model for the Martian polar cap breeze was constructed in part from work previously done by others on the terrestrial sea breeze. With this model a numerical simulation corresponding to the Southem Hemisphere winter season was made. The results obtained with the proposed model show that the Martian polar cap breeze is a well defined system with some similarities to the terrestrial sea breeze. At the time of maximum intensity, the largest values of vertical velocities are about 10 cm/s and occur at heights between 850-1250 m. The largest values of horizontal velocities are about 15 m/s. A "polar cap breeze front" is clearly discernible in the results. The rate of advance of this front is at an average of about I0 km/h.es_ES
dc.description.procedenceUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias Básicas::Centro de Investigaciones Geofísicas (CIGEFI)es_ES
dc.description.procedenceUCR::Vicerrectoría de Docencia::Ciencias Básicas::Facultad de Ciencias::Escuela de Físicaes_ES
dc.identifier.citationhttps://link.springer.com/article/10.1007/BF00619464es_ES
dc.identifier.doi10.1007/BF00619464
dc.identifier.issn1573-0794
dc.identifier.issn0167-9295
dc.identifier.urihttps://hdl.handle.net/10669/89852
dc.language.isoenges_ES
dc.rightsacceso embargado
dc.sourceEarth, Moon and Planets, vol.70 (1-3), pp.193-205es_ES
dc.subjectPOLAR REGIONSes_ES
dc.subjectMATHEMATICAL MODELSes_ES
dc.subjectSIMULATION MODELSes_ES
dc.titleA Numerical Simulation of the Martian Polar Cap Breezees_ES
dc.typeartículo originales_ES

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