Multi-Instrument Rainfall-Rate Estimation in the Peruvian Central Andes

Agriculture is one of the main economic activities in the Peruvian Andes; rainwater alone irrigates more than 80% of the fields used for agriculture purposes. However, the cloud and rain generation mechanisms in the Andes still remain mostly unknown. In early 2014, the Instituto Geofísico del Perú (IGP) decided to intensify studies in the central Andes to better understand cloud microphysics; the Atmospheric Microphysics And Radiation Laboratory officially started operations in 2015 at IGP’s Huancayo Observatory. In this work, a Ka-band cloud profiler [cloud and precipitation profiler (MIRA-35c)], a UHF wind profiler [Clear-Air and Rainfall Estimation (CLAIRE)], and a VHF wind profiler [Boundary Layer and Tropospheric Radar (BLTR)] are used to estimate rainfall rate at different conditions. The height dependence of the drop size diameter versus the terminal velocity, obtained by the radars, in the central Andes (3350 m MSL) was evaluated. The estimates of rainfall rate are validated to ground measurements through a disdrometer [second-generation Particle, Size, and Velocity (PARSIVEL2)] and two rain gauges. The biases in the cumulative rainfall totals for the PARSIVEL2, MIRA-35c, and CLAIRE were 18%, 23%, and −32%, respectively, and their respective absolute biases were 19%, 36%, and 63%. These results suggest that a real-time calibration of the radars, MIRA-35c and CLAIRE, is necessary for better estimation of precipitation at the ground. They also show that the correction of the raindrop terminal fall velocity, obtained by separating the vertical wind velocity (BLTR), used in the estimation the raindrop diameter is not sufficient, especially in convective conditions.

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Bibliographic Details
Main Author: 350221 Valdivia, Jairo M. autor
Format: Texto biblioteca
Language:eng
Published: American Meteorological Society 2020
Subjects:LLUVIA, RAIN, PRECIPITACION ATMOSFERICA, PRECIPITATION, AGUA DE LLUVIA, RAINWATER, DEFICIT PLUVIOMETRICO, PRECIPITATION DEFICIT,
Online Access:https://doi.org/10.1175/JTECH-D-19-0105.1
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spelling KOHA-OAI-BVE:1500742022-09-01T20:36:42ZMulti-Instrument Rainfall-Rate Estimation in the Peruvian Central Andes 350221 Valdivia, Jairo M. autor textAmerican Meteorological Society2020engAgriculture is one of the main economic activities in the Peruvian Andes; rainwater alone irrigates more than 80% of the fields used for agriculture purposes. However, the cloud and rain generation mechanisms in the Andes still remain mostly unknown. In early 2014, the Instituto Geofísico del Perú (IGP) decided to intensify studies in the central Andes to better understand cloud microphysics; the Atmospheric Microphysics And Radiation Laboratory officially started operations in 2015 at IGP’s Huancayo Observatory. In this work, a Ka-band cloud profiler [cloud and precipitation profiler (MIRA-35c)], a UHF wind profiler [Clear-Air and Rainfall Estimation (CLAIRE)], and a VHF wind profiler [Boundary Layer and Tropospheric Radar (BLTR)] are used to estimate rainfall rate at different conditions. The height dependence of the drop size diameter versus the terminal velocity, obtained by the radars, in the central Andes (3350 m MSL) was evaluated. The estimates of rainfall rate are validated to ground measurements through a disdrometer [second-generation Particle, Size, and Velocity (PARSIVEL2)] and two rain gauges. The biases in the cumulative rainfall totals for the PARSIVEL2, MIRA-35c, and CLAIRE were 18%, 23%, and −32%, respectively, and their respective absolute biases were 19%, 36%, and 63%. These results suggest that a real-time calibration of the radars, MIRA-35c and CLAIRE, is necessary for better estimation of precipitation at the ground. They also show that the correction of the raindrop terminal fall velocity, obtained by separating the vertical wind velocity (BLTR), used in the estimation the raindrop diameter is not sufficient, especially in convective conditions.Agriculture is one of the main economic activities in the Peruvian Andes; rainwater alone irrigates more than 80% of the fields used for agriculture purposes. However, the cloud and rain generation mechanisms in the Andes still remain mostly unknown. In early 2014, the Instituto Geofísico del Perú (IGP) decided to intensify studies in the central Andes to better understand cloud microphysics; the Atmospheric Microphysics And Radiation Laboratory officially started operations in 2015 at IGP’s Huancayo Observatory. In this work, a Ka-band cloud profiler [cloud and precipitation profiler (MIRA-35c)], a UHF wind profiler [Clear-Air and Rainfall Estimation (CLAIRE)], and a VHF wind profiler [Boundary Layer and Tropospheric Radar (BLTR)] are used to estimate rainfall rate at different conditions. The height dependence of the drop size diameter versus the terminal velocity, obtained by the radars, in the central Andes (3350 m MSL) was evaluated. The estimates of rainfall rate are validated to ground measurements through a disdrometer [second-generation Particle, Size, and Velocity (PARSIVEL2)] and two rain gauges. The biases in the cumulative rainfall totals for the PARSIVEL2, MIRA-35c, and CLAIRE were 18%, 23%, and −32%, respectively, and their respective absolute biases were 19%, 36%, and 63%. These results suggest that a real-time calibration of the radars, MIRA-35c and CLAIRE, is necessary for better estimation of precipitation at the ground. They also show that the correction of the raindrop terminal fall velocity, obtained by separating the vertical wind velocity (BLTR), used in the estimation the raindrop diameter is not sufficient, especially in convective conditions.LLUVIARAINPRECIPITACION ATMOSFERICAPRECIPITATIONAGUA DE LLUVIARAINWATERDEFICIT PLUVIOMETRICOPRECIPITATION DEFICIThttps://doi.org/10.1175/JTECH-D-19-0105.1
institution IICA
collection Koha
country Costa Rica
countrycode CR
component Bibliográfico
access En linea
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databasecode cat-sibiica
tag biblioteca
region America Central
libraryname Sistema de Bibliotecas IICA/CATIE
language eng
topic LLUVIA
RAIN
PRECIPITACION ATMOSFERICA
PRECIPITATION
AGUA DE LLUVIA
RAINWATER
DEFICIT PLUVIOMETRICO
PRECIPITATION DEFICIT
LLUVIA
RAIN
PRECIPITACION ATMOSFERICA
PRECIPITATION
AGUA DE LLUVIA
RAINWATER
DEFICIT PLUVIOMETRICO
PRECIPITATION DEFICIT
spellingShingle LLUVIA
RAIN
PRECIPITACION ATMOSFERICA
PRECIPITATION
AGUA DE LLUVIA
RAINWATER
DEFICIT PLUVIOMETRICO
PRECIPITATION DEFICIT
LLUVIA
RAIN
PRECIPITACION ATMOSFERICA
PRECIPITATION
AGUA DE LLUVIA
RAINWATER
DEFICIT PLUVIOMETRICO
PRECIPITATION DEFICIT
350221 Valdivia, Jairo M. autor
Multi-Instrument Rainfall-Rate Estimation in the Peruvian Central Andes
description Agriculture is one of the main economic activities in the Peruvian Andes; rainwater alone irrigates more than 80% of the fields used for agriculture purposes. However, the cloud and rain generation mechanisms in the Andes still remain mostly unknown. In early 2014, the Instituto Geofísico del Perú (IGP) decided to intensify studies in the central Andes to better understand cloud microphysics; the Atmospheric Microphysics And Radiation Laboratory officially started operations in 2015 at IGP’s Huancayo Observatory. In this work, a Ka-band cloud profiler [cloud and precipitation profiler (MIRA-35c)], a UHF wind profiler [Clear-Air and Rainfall Estimation (CLAIRE)], and a VHF wind profiler [Boundary Layer and Tropospheric Radar (BLTR)] are used to estimate rainfall rate at different conditions. The height dependence of the drop size diameter versus the terminal velocity, obtained by the radars, in the central Andes (3350 m MSL) was evaluated. The estimates of rainfall rate are validated to ground measurements through a disdrometer [second-generation Particle, Size, and Velocity (PARSIVEL2)] and two rain gauges. The biases in the cumulative rainfall totals for the PARSIVEL2, MIRA-35c, and CLAIRE were 18%, 23%, and −32%, respectively, and their respective absolute biases were 19%, 36%, and 63%. These results suggest that a real-time calibration of the radars, MIRA-35c and CLAIRE, is necessary for better estimation of precipitation at the ground. They also show that the correction of the raindrop terminal fall velocity, obtained by separating the vertical wind velocity (BLTR), used in the estimation the raindrop diameter is not sufficient, especially in convective conditions.
format Texto
topic_facet LLUVIA
RAIN
PRECIPITACION ATMOSFERICA
PRECIPITATION
AGUA DE LLUVIA
RAINWATER
DEFICIT PLUVIOMETRICO
PRECIPITATION DEFICIT
author 350221 Valdivia, Jairo M. autor
author_facet 350221 Valdivia, Jairo M. autor
author_sort 350221 Valdivia, Jairo M. autor
title Multi-Instrument Rainfall-Rate Estimation in the Peruvian Central Andes
title_short Multi-Instrument Rainfall-Rate Estimation in the Peruvian Central Andes
title_full Multi-Instrument Rainfall-Rate Estimation in the Peruvian Central Andes
title_fullStr Multi-Instrument Rainfall-Rate Estimation in the Peruvian Central Andes
title_full_unstemmed Multi-Instrument Rainfall-Rate Estimation in the Peruvian Central Andes
title_sort multi-instrument rainfall-rate estimation in the peruvian central andes
publisher American Meteorological Society
publishDate 2020
url https://doi.org/10.1175/JTECH-D-19-0105.1
work_keys_str_mv AT 350221valdiviajairomautor multiinstrumentrainfallrateestimationintheperuviancentralandes
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