Articles | Volume 22, issue 5
https://doi.org/10.5194/hess-22-2811-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-22-2811-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Comparison of precipitation measurements by OTT Parsivel2 and Thies LPM optical disdrometers
Marta Angulo-Martínez
Estación Experimental de Aula Dei, Consejo Superior de Investigaciones Científicas (EEAD-CSIC), Avda. Montanana 1005, Zaragoza, 50059, Spain
Santiago Beguería
CORRESPONDING AUTHOR
Estación Experimental de Aula Dei, Consejo Superior de Investigaciones Científicas (EEAD-CSIC), Avda. Montanana 1005, Zaragoza, 50059, Spain
Borja Latorre
Estación Experimental de Aula Dei, Consejo Superior de Investigaciones Científicas (EEAD-CSIC), Avda. Montanana 1005, Zaragoza, 50059, Spain
María Fernández-Raga
Dept. of Physics, University of León, León, Spain
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75 citations as recorded by crossref.
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74 citations as recorded by crossref.
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- Snowfall Microphysics Characterized by PARSIVEL Disdrometer Observations in Beijing from 2020 to 2022 Y. Shen et al. 10.3390/rs14236025
- Precipitation adjustment by the OTT Parsivel2 in the central Qinghai–Tibet Plateau C. Wang et al. 10.1002/esp.5836
- Evaluating and modeling a rainfall kinetic energy and erosivity: a case study of a humid watershed in the Ethiopian highlands K. Tilahun et al. 10.1007/s40808-023-01921-0
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- Evaluation of the raindrop size distribution representation of microphysics schemes in typhoon lekima using disdrometer network observations L. Lin et al. 10.1016/j.atmosres.2022.106346
- Machine Learning Approach to Classify Rain Type Based on Thies Disdrometers and Cloud Observations W. Ghada et al. 10.3390/atmos10050251
- The Use of High-Speed Cameras as a Tool for the Characterization of Raindrops in Splash Laboratory Studies M. Fernández-Raga et al. 10.3390/w13202851
- Triple‐Frequency Doppler Retrieval of Characteristic Raindrop Size K. Mróz et al. 10.1029/2019EA000789
- Shapes and Fall Speeds of Freezing and Frozen Raindrops K. Rahman & F. Testik 10.1175/JHM-D-19-0204.1
- Measurement and modelling of kinetic energy and erosivity of rainfall and throughfall in a tropical semiarid region J. Brasil et al. 10.1016/j.jhydrol.2024.132088
- Error investigation of rain retrievals from disdrometer data using triple colocation C. Annella et al. 10.1002/asl.1127
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- Sensitivity of simulated rain intensity and kinetic energy to aerosols and warm‐rain microphysics during the extreme event of July 2021 in Belgium K. Van Weverberg et al. 10.1002/qj.4761
- Seasonal dependence of characteristics of rain drop size distribution over two different climatic zones of India D. Shaik et al. 10.1007/s00703-024-01012-4
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- Tephra sedimentation and grainsize associated with pulsatory activity: the 2021 Tajogaite eruption of Cumbre Vieja (La Palma, Canary Islands, Spain) C. Bonadonna et al. 10.3389/feart.2023.1166073
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- Scale invariant relationship between rainfall kinetic energy and intensity in Paris region: An evaluation using universal multifractal framework J. Jose et al. 10.1016/j.jhydrol.2022.127715
- Database of the Italian disdrometer network E. Adirosi et al. 10.5194/essd-15-2417-2023
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- A General Approach for Simulating Rain Effects on Sensor Data in Real and Virtual Environments S. Hasirlioglu & A. Riener 10.1109/TIV.2019.2960944
- Influence of Reduced Anthropogenic Activities on Rain Microphysical Properties and Related Atmospheric Parameters Over an Urban Tropical Location G. Rakshit et al. 10.1109/LGRS.2021.3093827
- Regional differences in raindrop size distribution observed from disdrometers in South Korea and their possible causes J. Lee et al. 10.1007/s00704-022-04192-4
- Corrections of Precipitation Particle Size Distribution Measured by a Parsivel OTT2 Disdrometer under Windy Conditions in the Antisana Massif, Ecuador L. Gualco et al. 10.3390/w13182576
- Atmospheric and surface observations during the Saint John River Experiment on Cold Season Storms (SAJESS) H. Thompson et al. 10.5194/essd-15-5785-2023
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- Advantage of Volume Scanning Video Disdrometer in Solid-Precipitation Observation Y. Katsuyama & M. Inatsu 10.2151/sola.2021-006
- Rain Measurement Using Nacelle-Mounted Doppler Lidar X. Liu et al. 10.1109/TGRS.2024.3494248
- Parametrization of drop size distribution with rain rate for microwave and millimeter wave applications in Central Africa P. Ntanguen et al. 10.1007/s12648-023-02664-5
- Exploring the statistical characteristics of coastal winter precipitation measured using a Parsivel2 disdrometer: A case study in North Carolina L. Yuan et al. 10.1016/j.atmosres.2024.107487
- Long-term changes in rainfall epochs and intensity patterns of Indian summer monsoon in changing climate K. Subrahmanyam et al. 10.1016/j.atmosres.2023.106997
- Suppression of precipitation bias in wind velocities from continuous-wave Doppler lidars L. Jin et al. 10.5194/amt-16-6007-2023
- Refinements to Data Acquired by 2-Dimensional Video Disdrometers M. Larsen & C. Blouin 10.3390/atmos11080855
- Effects of Air Pollution on Rainfall Microphysics Over the Yangtze River Delta Q. Yang et al. 10.1029/2021JD035934
- Development of quantitative precipitation estimation (QPE) relations for dual-polarization radars based on raindrop size distribution measurements in Metro Manila, Philippines M. Ibañez et al. 10.1007/s44195-023-00056-0
- Effect of disdrometer type on rain drop size distribution characterisation: a new dataset for south-eastern Australia A. Guyot et al. 10.5194/hess-23-4737-2019
Latest update: 26 Dec 2024
Short summary
Two optical disdrometers, OTT Parsivel2 disdrometer and Thies Clima laser precipitation monitor (LPM), are compared. Analysis of 2 years of one-minute replicated data showed significant differences. Thies LPM recorded a larger number of particles than Parsivel2 and a higher proportion of small particles, resulting in higher rain rates and amounts and differences in radar reflectivity and kinetic energy. Possible causes for these differences, and their practical consequences, are discussed.
Two optical disdrometers, OTT Parsivel2 disdrometer and Thies Clima laser precipitation monitor...