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Vertical structure of the stable boundary layer detected by RASS-SODAR and in-situ measurements in SABLES 2006 field campaign
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dc.contributor.authorViana Jiménez, Samueles_ES
dc.contributor.authorYagüe, Carloses_ES
dc.contributor.authorMaqueda Burgos, Gregorioes_ES
dc.identifier.citationActa Geophysica. 2012, 60(5), p. 1261-1286es_ES
dc.description.abstractData from the SABLES 2006 field campaign are used in order to analyse some of the main processes present along the nocturnal periods: surface-based inversions, low level jets, katabatic winds, wave-like motions, pressure perturbations, etc. These processes have an important influence on the vertical structure (both thermal and dynamical) of the atmospheric boundary layer, and can be better described with the synergetic combination of RASS-SODAR data and in-situ measurements (such as sonic anemometer data and high-resolution pressure series from microbarometers). It is shown how the different air masses and their evolution are easily identified when pressure and RASS-SODAR wind and temperature data are presented together. Likewise, periodic pressure fluctuations observed in the surface array of microbarometers reveal the existence of gravity wave motions whose propagation is better understood after locating the wave ducting layers with the help of RASS-SODAR average wind ant temperature profiles.es_ES
dc.description.sponsorshipThis research has been funded by the Spanish Ministry of Science and Innovation (projects CGL2006-12474-C03- 03 and CGL2009-12797-C03-03). The GR58/08 program (supported by BSCH and UCM) has also partially financed this work through the Research Group “Micrometeorology and Climate Variability” (No. 910437).-
dc.publisherDe Gruyter Openes_ES
dc.subjectStable boundary layeres_ES
dc.subjectGravity waveses_ES
dc.subjectPressure perturbationses_ES
dc.titleVertical structure of the stable boundary layer detected by RASS-SODAR and in-situ measurements in SABLES 2006 field campaignes_ES
Appears in Collections:Artículos científicos 2010-2014

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