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Volume 7, issue 2
Atmos. Meas. Tech., 7, 409–418, 2014
https://doi.org/10.5194/amt-7-409-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Tropospheric profiling (ISTP9)

Atmos. Meas. Tech., 7, 409–418, 2014
https://doi.org/10.5194/amt-7-409-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 07 Feb 2014

Research article | 07 Feb 2014

Properties of rainfall in a tropical volcanic island deduced from UHF wind profiler measurements

A. Réchou1, T. Narayana Rao2, O. Bousquet1, M. Plu1,3, and R. Decoupes4 A. Réchou et al.
  • 1Laboratoire de l'Atmosphère et des Cyclones, UMR8105 CNRS, Météo France, Université de la Réunion, Réunion Island, France
  • 2National Atmospheric Research Laboratory, Gadanki, India
  • 3CNRM-GAME, UMR3589, CNRS and Météo-France, Toulouse, France
  • 4Université de la Réunion, UMS3365, OSUR, Saint Denis, Réunion Island, France

Abstract. The microphysical properties of rainfall at the island of Réunion are analysed and quantified according to one year of wind profiler observations collected at Saint-Denis international airport. The statistical analysis clearly shows important differences in rain vertical profiles as a function of the seasons. During the dry season, the vertical structure of precipitation is driven by trade wind and boundary-layer inversions, both of which limit the vertical extension of the clouds. The rain rate is lower than 2.5 mm h−1 throughout the lower part of the troposphere (about 2 km) and decreases in the higher altitudes. During the moist season, the average rain rate is around 5 mm h−1 and nearly uniform from the ground up to 4 km.

The dynamical and microphysical properties (including drop size distributions) of four distinct rainfall events are also investigated through the analysis of four case studies representative of the variety of rain events occurring on Réunion: summer deep convection, northerly-to-northeasterly flow atmospheric pattern, cold front and winter depression embedded in trade winds. Radar-derived rain parameters are in good agreement with those obtained from collocated rain gauge observations in all cases, which demonstrates that accurate qualitative and quantitative analysis can be inferred from wind profiler data. Fluxes of kinetic energy are also estimated from wind profiler observations in order to evaluate the impact of rainfall on soil erosion. Results show that horizontal kinetic energy fluxes are systematically one order of magnitude higher than vertical kinetic energy fluxes. A simple relationship between the reflectivity factor and vertical kinetic energy fluxes is proposed based on the results of the four case studies.

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