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Authordc.contributor.authorAstudillo, O. 
Authordc.contributor.authorDewitte, B. 
Authordc.contributor.authorMallet, M. 
Authordc.contributor.authorFrappart, F. 
Authordc.contributor.authorRutllant Costa, José 
Authordc.contributor.authorRamos, M. 
Authordc.contributor.authorBravo, L. 
Authordc.contributor.authorGoubanova, K. 
Authordc.contributor.authorIllig, S. 
Admission datedc.date.accessioned2019-05-29T13:10:41Z
Available datedc.date.available2019-05-29T13:10:41Z
Publication datedc.date.issued2017
Cita de ítemdc.identifier.citationRemote Sensing of Environment 191 (2017) 179–196
Identifierdc.identifier.issn00344257
Identifierdc.identifier.other10.1016/j.rse.2017.01.010
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/168854
Abstractdc.description.abstractThe near-shore surface mesoscale atmospheric circulation in the upwelling systems off Peru and Chile is influen-tial on the Sea Surface Temperature through Ekman transport and pumping. There has been a debate whether ornot the so-called“wind drop-off”, that isa shoreward decrease of the surface wind speed nearthe coast, can act asan effective forcing of upwelling through Ekman pumping. Although the wind drop-off has been simulated byhigh-resolution atmospheric models, it has not been well documented due to uncertainties in thescatterometry-derived wind estimates associated with land contamination. Here we use the along-track altime-try-derived surface wind speed data from ENVISAT, Jason-1, Jason-2, and SARAL satellites, to document the spa-tial variability of the mean wind drop-off near the coast as estimated from the inversion of the radarbackscattering coefficient. The data arefirst calibrated so as tofit with the scatterometer observations of previousand current satellite missions (QuikSCAT, ASCAT). The calibrated data are then analyzed near the coast and awind drop-offscaleisestimated. The results indicate that the wind drop-off takes placeall alongthe coast, thoughwith a significant alongshore variability in its magnitude. Differences between products are shown to be relatedboth to the differences in repeat cycle between the different altimetry missions and to the peculiarities of thecoastline shape at the coastal latitudes of the incident tracks. The relative contribution of Ekman pumping andEkman transport to the total transport is also estimated indicating a comparable contribution off Chile whiletransport associated to Ekman pumping is on average ~1.4 larger than Ekman transport off Peru. Despite thealiasing effect associated with the weak repetitivity of the satellite orbit and the high frequency variability ofthe winds in this region, the analysis suggests that the seasonal cycle of the surface winds near the coast couldbe resolved at least off Peru.
Lenguagedc.language.isoen
Publisherdc.publisherElsevier.
Type of licensedc.rightsAttribution-NonCommercial-NoDerivs 3.0 Chile
Link to Licensedc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
Sourcedc.sourceRemote Sensing of Environment
Keywordsdc.subjectCoastal surface winds
Keywordsdc.subjectPeru-Chile upwelling system
Keywordsdc.subjectSatellite altimetry
Keywordsdc.subjectWind drop-off
Títulodc.titleSurface winds off Peru-Chile: Observing closer to the coast from radar altimetry
Document typedc.typeArtículo de revista
Catalogueruchile.catalogadorlaj
Indexationuchile.indexArtículo de publicación SCOPUS
uchile.cosechauchile.cosechaSI


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Attribution-NonCommercial-NoDerivs 3.0 Chile
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 Chile