Hydrologic Visibility of Weather Radar Systems Operating in Mountainous Regions: Case Study for the Ardèche Catchment (France)
Open Access
- 1 October 2002
- journal article
- Published by American Meteorological Society in Journal of Hydrometeorology
- Vol. 3 (5), 539-555
- https://doi.org/10.1175/1525-7541(2002)003<0539:hvowrs>2.0.co;2
Abstract
A simulation procedure has been developed for use in predetermining the expected quality of rain-rate estimates that a given weather radar system operating in a mountainous region may obtain over a given hydrologic catchment. This first application of what is referred to as the “hydrologic visibility” concept focuses on the quantification of the rain-rate error resulting from the effects of ground clutter, beam blockage, and the vertical profile of reflectivity (VPR). The assessment of the impact of the space–time structure of the radar error in terms of discharge at the catchment outlet is also investigated using a distributed hydrologic model. A case study is presented for the Ardèche catchment in France using the parameters of two S-band weather radars operated by Météo-France at Nîmes and Bollène. Radar rain-rate error generation and rainfall–runoff simulations are performed using VPR and areal rainfall time series representative of the Cévennes rain climatology. The major impact of ground cl... Abstract A simulation procedure has been developed for use in predetermining the expected quality of rain-rate estimates that a given weather radar system operating in a mountainous region may obtain over a given hydrologic catchment. This first application of what is referred to as the “hydrologic visibility” concept focuses on the quantification of the rain-rate error resulting from the effects of ground clutter, beam blockage, and the vertical profile of reflectivity (VPR). The assessment of the impact of the space–time structure of the radar error in terms of discharge at the catchment outlet is also investigated using a distributed hydrologic model. A case study is presented for the Ardèche catchment in France using the parameters of two S-band weather radars operated by Météo-France at Nîmes and Bollène. Radar rain-rate error generation and rainfall–runoff simulations are performed using VPR and areal rainfall time series representative of the Cévennes rain climatology. The major impact of ground cl...Keywords
This publication has 22 references indexed in Scilit:
- Rain Measurement in Hilly Terrain with X-Band Weather Radar Systems: Accuracy of Path-Integrated Attenuation Estimates Derived from Mountain ReturnsJournal of Atmospheric and Oceanic Technology, 1999
- TOPMODEL: A critiqueHydrological Processes, 1997
- Use of a weather radar for the hydrology of a mountainous area. Part II: radar measurement validationJournal of Hydrology, 1997
- Use of a weather radar for the hydrology of a mountainous area. Part I: radar measurement interpretationJournal of Hydrology, 1997
- Simulation of Radar Mountain Returns Using a Digitized Terrain ModelJournal of Atmospheric and Oceanic Technology, 1995
- Identification of Vertical Profiles of Radar Reflectivity for Hydrological Applications Using an Inverse Method. Part II: FormulationJournal of Applied Meteorology and Climatology, 1995
- Identification of Vertical Profiles of Radar Reflectivity for Hydrological Applications Using an Inverse Method. Part I: FormulationJournal of Applied Meteorology and Climatology, 1995
- Unit hydrograph revisited: an alternate iterative approach to UH and effective precipitation identificationJournal of Hydrology, 1993
- A physically based, variable contributing area model of basin hydrology / Un modèle à base physique de zone d'appel variable de l'hydrologie du bassin versantHydrological Sciences Bulletin, 1979
- Étude des Lois de L'écoulement - Application au Calcul et à la Prévision des DébitsLa Houille Blanche, 1960