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Authordc.contributor.authorGarreaud Salazar, René 
Authordc.contributor.authorRutllant Costa, José es_CL
Authordc.contributor.authorMuñoz Alvarado, Raúl es_CL
Authordc.contributor.authorRahn, David es_CL
Authordc.contributor.authorRamos, M. es_CL
Authordc.contributor.authorFigueroa, D. es_CL
Admission datedc.date.accessioned2011-10-27T15:38:00Z
Available datedc.date.available2011-10-27T15:38:00Z
Publication datedc.date.issued2011
Cita de ítemdc.identifier.citationATMOSPHERIC CHEMISTRY AND PHYSICS Volume: 11 Issue: 5 Pages: 2015-2029 Published: 2011es_CL
Identifierdc.identifier.issn1680-7316
Identifierdc.identifier.otherDOI: 10.5194/acp-11-2015-2011
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/125508
General notedc.descriptionArtículo de publicación ISIes_CL
Abstractdc.description.abstractThe VAMOS Ocean-Cloud-Atmosphere-Land Study Regional Experiment (VOCALS-REx) was a major field experiment conducted in spring of 2008 off southern Peru and northern Chile, aimed at better understanding the coupled climate systems of the southeast Pacific. Because of logistical constrains, the coastal area around 30 degrees S was not sampled during VOCALS-REx. This area not only marks the poleward edge of the subtropical stratocumulus cloud regime (thus acting as a source of transient disturbances) but is also one of the most active upwelling centers and source of surface ocean kinetic energy along the Chilean coast. To fill such an observational gap, a small, brief, but highly focused field experiment was conducted in late spring 2009 in the near-shore region around 30 degrees S. The Chilean Upwelling Experiment (CUpEx) was endorsed by VOCALS as a regional component. CUpEx included long-term monitoring, an intensive two-week field campaign and off-shore research flights. Our goal was to obtain an atmospheric/oceanic dataset with enough temporal and spatial coverage to be able to document (a) the mean diurnal cycles of the lower-troposphere and upper-ocean in a region of complex topography and coastline geometry, and (b) the ocean-atmosphere response to the rapid changes in coastal winds from strong, upwelling-favorable equatorward flow (southerly winds) to downwelling-favorable poleward flow (northerly winds). In this paper we describe the measurement platforms and sampling strategy, and provide an observational overview, highlighting some key mean-state and transient features.es_CL
Patrocinadordc.description.sponsorshipCONICYT (Chile) FONDECYT 1090492 1080606 1090791 FONDEF D03I-1104 INNOVA-Chile 07CN13IXM-150 National Weather Service (DMC) National Civil Aviation Directorate (DGAC)es_CL
Lenguagedc.language.isoenes_CL
Publisherdc.publisherCOPERNICUS GESELLSCHAFT MBHes_CL
Keywordsdc.subjectSUBTROPICAL SOUTH-AMERICAes_CL
Títulodc.titleVOCALS-CUpEx: the Chilean Upwelling Experimentes_CL
Document typedc.typeArtículo de revista


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