Articles | Volume 11, issue 3
Research article
26 Mar 2018
Research article |  | 26 Mar 2018

High-resolution humidity profiles retrieved from wind profiler radar measurements

Frédérique Saïd, Bernard Campistron, and Paolo Di Girolamo

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Cited articles

Angevine, W. M., White, A. B., and Avery, S. K.: Boundary-layer depth and entrainment zone characterization with a boundary-layer profiler, Bound.-Lay. Meteorol., 68, 375–385, 1994. a
Atlas, D., Srivastava, R., and Sekhon, R.: Doppler radar characteristics of precipitation at vertical incidence, Rev. Geophys. Space Ge., 11, 1–35, 1973. a
Bianco, L., Cimini, D., Marzano, F. S., and Ware, R.: Combining Microwave Radiometer and Wind Profiler Radar Measurements for High-Resolution Atmospheric Humidity Profiling, J. Atmos. Ocean. Tech., 22, 949–965,, 2005. a, b
Campistron, B. and Réchou, A.: Rain kinetic energy measurement with a UHF wind profiler, 13th workshop on Technical and Scientific Aspects of MST Radar (MST13), Kühlungsborn, 19–23 March, Germany, 2012. a
Campistron, B., Saïd, F., Delbarre, H., Augustin, P., and Lambert, D.: Rain Profiling with a UHF Wind Profiler and its Application to Soil Erosion Study, HyMeX 7th international conference, Cassis, France, 2013. a, b
Short summary
Vertical profiles of the atmospheric water vapor mixing ratio are retrieved with an algorithm based on the combination of measurements from a wind profiler radar and radiosoundings at a coarser time resolution. The major advance with respect to previous works is the use of the radar capacity to detect transition levels, such as the top level of the boundary layer, marked by a maximum in the radar reflectivity.