Article Type:
Research Article

The Optical Spectropluviometer Revisited

Christian Salles Geofluides Bassins Eau, Université de Montpellier, Montpellier, France

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Jean-Dominique Creutin Laboratoire d’Etude des Trauferts en Hydrologie et Environnement, Université de Grenoble, Grenoble, France

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Daniel Sempere-Torres Deparamento d’Enginyeria Hydràulica, Maritima i Ambiental, Universitat Politecnica de Catalunya, Barcelona, Spain

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Print Publication:
01 Oct 1998
DOI:
https://doi.org/10.1175/1520-0426(1998)015<1215:TOSR>2.0.CO;2
Page(s):
1215–1222
Restricted access

Abstract

The optical spectropluviometer is a shadowgraph instrument able to measure independently the equivalent diameter and the fall speed of raindrops at ground level. Hardware and software modifications are proposed and tested. A modern digital signal processing system allows for the simultaneous sampling and analyzing of the signal delivered by the sensor. The IR light transmission is pulsed to avoid interference with natural radiation and the protection of the optics is improved. The validation procedure consists of comparing the rain rates derived from the measured drop size distributions with rain rates delivered by nearby rain gauges. The results obtained during 65 storm events show that the proposed improvements reduce the bias of the rain-rate estimation from 34% to 16%. Suggestions are given to further improve the performance of this instrument.

Corresponding author address: Christian Salles, Laboratory for Experimental Geomorphology, Redingenstraat 16, B-3000 Leuven, Belgium.

Email: christian.salles@geo.kuleuven.ac.be

Abstract

The optical spectropluviometer is a shadowgraph instrument able to measure independently the equivalent diameter and the fall speed of raindrops at ground level. Hardware and software modifications are proposed and tested. A modern digital signal processing system allows for the simultaneous sampling and analyzing of the signal delivered by the sensor. The IR light transmission is pulsed to avoid interference with natural radiation and the protection of the optics is improved. The validation procedure consists of comparing the rain rates derived from the measured drop size distributions with rain rates delivered by nearby rain gauges. The results obtained during 65 storm events show that the proposed improvements reduce the bias of the rain-rate estimation from 34% to 16%. Suggestions are given to further improve the performance of this instrument.

Corresponding author address: Christian Salles, Laboratory for Experimental Geomorphology, Redingenstraat 16, B-3000 Leuven, Belgium.

Email: christian.salles@geo.kuleuven.ac.be

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