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Ricaud, P., F. Carminati, B. Plazolles, Y. Courcoux, C. Genthon, A. Pellegrini, J.-L. Attie, L. El Amraoui, T. August, J. Warner. (2012). Variabilities of temperature and water vapour above Dome C (Antarctica) from the lowermost troposphere to the lowermost stratosphere.
Abstract: SCAR 2012, 13-25 Juillet, Portland, USA
Programme: 1013
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Ricaud, Philippe. (2014).85, 35–46.
Abstract: The H2O Antarctica Microwave Stratospheric and Tropospheric Radiometers (HAMSTRAD) program aims to develop a ground-based microwave radiometer to measure tropospheric water vapor and temperature vertical profiles above the Dome C station, Concordia, Antarctica. The present article deals with the scientific results obtained with the vertical profiles of H2O and temperature from 0 to 10 km above the station coupled with other data sets (in situ, satellite, radiosonde, analyses and mesoscale model). The short-term variability (diurnal variation) has been studied in the lowermost troposphere according to the season to highlight the time evolution of the different sub-layers within the atmospheric boundary layer. Considering back-trajectory studies, the intra-seasonal variability of H2O and temperature in the troposphere comes mainly from the origin of air masses reaching the Dome C station, oceanic or continental, producing a high correlation rate between H2O and temperature. In a case study, a mesoscale model tends to calculate a wetter and warmer atmosphere than observations in the atmospheric boundary layer.
Programme: 910
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Ricaud, Philippe. (2014). 0026-1181, 84, 15–28.
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Laparie M., Lebouvier M., Lalouette L. & Renault D. (2009).
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Leglise Joris. (2015).
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