Seasonal variability of the ekman transport and pumping in the upwelling system off central-northern chile (similar to aeuro-30a degrees aeuro-s) based on a high-resolution atmospheric regional model (wrf)

dc.date.accessioned2018-12-07T13:32:57Z
dc.date.accessioned2022-10-18T21:55:47Z
dc.date.available2018-12-07T13:32:57Z
dc.date.available2022-10-18T21:55:47Z
dc.date.created2018-12-07T13:32:57Z
dc.date.issued2016
dc.identifierhttp://hdl.handle.net/10533/232166
dc.identifier1151185
dc.identifierWOS:000384011700001
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4463521
dc.description.abstractTwo physical mechanisms can contribute to coastal upwelling in eastern boundary current systems: offshore Ekman transport due to the predominant alongshore wind stress and Ekman pumping due to the cyclonic wind stress curl, mainly caused by the abrupt de
dc.languageeng
dc.relationhttps://www.ocean-sci.net/12/1049/2016/os-12-1049-2016.pdf
dc.relationhandle/10533/111557
dc.relation10.5194/os-12-1049-2016
dc.relationhandle/10533/111541
dc.relationhandle/10533/108045
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.titleSeasonal variability of the ekman transport and pumping in the upwelling system off central-northern chile (similar to aeuro-30a degrees aeuro-s) based on a high-resolution atmospheric regional model (wrf)
dc.typeArticulo


Este ítem pertenece a la siguiente institución