Comparison of precipitation measurements by OTT Parsivel<sup>2</sup> and Thies LPM optical disdrometers

Optical disdrometers are present weather sensors with the ability of providing detailed information on precipitation such as rain intensity, radar reflectivity or kinetic energy, together with discrete information on the particle size and fall velocity distribution (PSVD) of the hydrometeors. Di...

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Main Authors: M. Angulo-Martínez, S. Beguería, B. Latorre, M. Fernández-Raga
Format: Article
Language:English
Published: Copernicus Publications 2018-05-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/22/2811/2018/hess-22-2811-2018.pdf
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author M. Angulo-Martínez
S. Beguería
B. Latorre
M. Fernández-Raga
author_facet M. Angulo-Martínez
S. Beguería
B. Latorre
M. Fernández-Raga
author_sort M. Angulo-Martínez
collection DOAJ
description Optical disdrometers are present weather sensors with the ability of providing detailed information on precipitation such as rain intensity, radar reflectivity or kinetic energy, together with discrete information on the particle size and fall velocity distribution (PSVD) of the hydrometeors. Disdrometers constitute a step forward towards a more complete characterization of precipitation, being useful in several research fields and applications. In this article the performance of two extensively used optical disdrometers, the most recent version of OTT Parsivel<sup>2</sup> disdrometer and Thies Clima Laser Precipitation Monitor (LPM), is evaluated. During 2 years, four collocated optical disdrometers, two Thies Clima LPM and two OTT Parsivel<sup>2</sup>, collected up to 100 000 min of data and up to 30 000 min with rain in more than 200 rainfall events, with intensities peaking at 277 mm h<sup>−1</sup> in 1 minute. The analysis of these records shows significant differences between both disdrometer types for all integrated precipitation parameters, which can be explained by differences in the raw PSVD estimated by the two sensors. Thies LPM recorded a larger number of particles than Parsivel<sup>2</sup> and a higher proportion of small particles than OTT Parsivel<sup>2</sup>, resulting in higher rain rates and totals and differences in radar reflectivity and kinetic energy. These differences increased greatly with rainfall intensity. Possible causes of these differences, and their practical consequences, are discussed in order to help researchers and users in the choice of sensor, and at the same time pointing out limitations to be addressed in future studies.
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spelling doaj.art-91f04eced45a4be69f9315be5c5ba3e12022-12-22T00:38:45ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382018-05-01222811283710.5194/hess-22-2811-2018Comparison of precipitation measurements by OTT Parsivel<sup>2</sup> and Thies LPM optical disdrometersM. Angulo-Martínez0S. Beguería1B. Latorre2M. Fernández-Raga3Estación Experimental de Aula Dei, Consejo Superior de Investigaciones Científicas (EEAD-CSIC), Avda. Montanana 1005, Zaragoza, 50059, SpainEstación Experimental de Aula Dei, Consejo Superior de Investigaciones Científicas (EEAD-CSIC), Avda. Montanana 1005, Zaragoza, 50059, SpainEstación Experimental de Aula Dei, Consejo Superior de Investigaciones Científicas (EEAD-CSIC), Avda. Montanana 1005, Zaragoza, 50059, SpainDept. of Physics, University of León, León, SpainOptical disdrometers are present weather sensors with the ability of providing detailed information on precipitation such as rain intensity, radar reflectivity or kinetic energy, together with discrete information on the particle size and fall velocity distribution (PSVD) of the hydrometeors. Disdrometers constitute a step forward towards a more complete characterization of precipitation, being useful in several research fields and applications. In this article the performance of two extensively used optical disdrometers, the most recent version of OTT Parsivel<sup>2</sup> disdrometer and Thies Clima Laser Precipitation Monitor (LPM), is evaluated. During 2 years, four collocated optical disdrometers, two Thies Clima LPM and two OTT Parsivel<sup>2</sup>, collected up to 100 000 min of data and up to 30 000 min with rain in more than 200 rainfall events, with intensities peaking at 277 mm h<sup>−1</sup> in 1 minute. The analysis of these records shows significant differences between both disdrometer types for all integrated precipitation parameters, which can be explained by differences in the raw PSVD estimated by the two sensors. Thies LPM recorded a larger number of particles than Parsivel<sup>2</sup> and a higher proportion of small particles than OTT Parsivel<sup>2</sup>, resulting in higher rain rates and totals and differences in radar reflectivity and kinetic energy. These differences increased greatly with rainfall intensity. Possible causes of these differences, and their practical consequences, are discussed in order to help researchers and users in the choice of sensor, and at the same time pointing out limitations to be addressed in future studies.https://www.hydrol-earth-syst-sci.net/22/2811/2018/hess-22-2811-2018.pdf
spellingShingle M. Angulo-Martínez
S. Beguería
B. Latorre
M. Fernández-Raga
Comparison of precipitation measurements by OTT Parsivel<sup>2</sup> and Thies LPM optical disdrometers
Hydrology and Earth System Sciences
title Comparison of precipitation measurements by OTT Parsivel<sup>2</sup> and Thies LPM optical disdrometers
title_full Comparison of precipitation measurements by OTT Parsivel<sup>2</sup> and Thies LPM optical disdrometers
title_fullStr Comparison of precipitation measurements by OTT Parsivel<sup>2</sup> and Thies LPM optical disdrometers
title_full_unstemmed Comparison of precipitation measurements by OTT Parsivel<sup>2</sup> and Thies LPM optical disdrometers
title_short Comparison of precipitation measurements by OTT Parsivel<sup>2</sup> and Thies LPM optical disdrometers
title_sort comparison of precipitation measurements by ott parsivel sup 2 sup and thies lpm optical disdrometers
url https://www.hydrol-earth-syst-sci.net/22/2811/2018/hess-22-2811-2018.pdf
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