Precipitation nowcasting with three-dimensional space-time extrapolation of dense and frequent phased-array weather radar observations

The phased-array weather radar (PAWR) is a new-generation weather radar that can make a 100-m-resolution three-dimensional (3D) volume scan every 30 s for 100 vertical levels, producing ~100 times more data than the conventional parabolic-antenna radar with a volume scan typically made every 5 min f...

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Publicado: 2016
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08828156_v31_n1_p329_Otsuka
http://hdl.handle.net/20.500.12110/paper_08828156_v31_n1_p329_Otsuka
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spelling paper:paper_08828156_v31_n1_p329_Otsuka2023-06-08T15:46:26Z Precipitation nowcasting with three-dimensional space-time extrapolation of dense and frequent phased-array weather radar observations Atm/ocean structure/phenomena Convective clouds Forecasting Nowcasting Observational techniques and algorithms Radars/radar observations Extrapolation Forecasting Meteorological radar Parabolic antennas Radar Convective clouds Convective precipitation Conventional algorithms Nowcasting Radars/radar observations Three dimensional space Threedimensional (3-d) Two Dimensional (2 D) Antenna phased arrays algorithm convective cloud nowcasting precipitation (climatology) radar spatiotemporal analysis The phased-array weather radar (PAWR) is a new-generation weather radar that can make a 100-m-resolution three-dimensional (3D) volume scan every 30 s for 100 vertical levels, producing ~100 times more data than the conventional parabolic-antenna radar with a volume scan typically made every 5 min for 15 scan levels. This study takes advantage of orders of magnitude more rapid and dense observations by PAWR and explores high-precision nowcasting of 3D evolution at 1-10-km scales up to several minutes, which are compared with conventional horizontal two-dimensional (2D) nowcasting typically at O(100) km scales up to 1-6 h. A new 3D precipitation extrapolation system was designed to enhance a conventional algorithm for dense and rapid PAWR volume scans. Experiments show that the 3D extrapolation successfully captured vertical motions of convective precipitation cores and outperformed 2D nowcasting with both simulated and real PAWR data. © 2016 American Meteorological Society. 2016 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08828156_v31_n1_p329_Otsuka http://hdl.handle.net/20.500.12110/paper_08828156_v31_n1_p329_Otsuka
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Atm/ocean structure/phenomena
Convective clouds
Forecasting
Nowcasting
Observational techniques and algorithms
Radars/radar observations
Extrapolation
Forecasting
Meteorological radar
Parabolic antennas
Radar
Convective clouds
Convective precipitation
Conventional algorithms
Nowcasting
Radars/radar observations
Three dimensional space
Threedimensional (3-d)
Two Dimensional (2 D)
Antenna phased arrays
algorithm
convective cloud
nowcasting
precipitation (climatology)
radar
spatiotemporal analysis
spellingShingle Atm/ocean structure/phenomena
Convective clouds
Forecasting
Nowcasting
Observational techniques and algorithms
Radars/radar observations
Extrapolation
Forecasting
Meteorological radar
Parabolic antennas
Radar
Convective clouds
Convective precipitation
Conventional algorithms
Nowcasting
Radars/radar observations
Three dimensional space
Threedimensional (3-d)
Two Dimensional (2 D)
Antenna phased arrays
algorithm
convective cloud
nowcasting
precipitation (climatology)
radar
spatiotemporal analysis
Precipitation nowcasting with three-dimensional space-time extrapolation of dense and frequent phased-array weather radar observations
topic_facet Atm/ocean structure/phenomena
Convective clouds
Forecasting
Nowcasting
Observational techniques and algorithms
Radars/radar observations
Extrapolation
Forecasting
Meteorological radar
Parabolic antennas
Radar
Convective clouds
Convective precipitation
Conventional algorithms
Nowcasting
Radars/radar observations
Three dimensional space
Threedimensional (3-d)
Two Dimensional (2 D)
Antenna phased arrays
algorithm
convective cloud
nowcasting
precipitation (climatology)
radar
spatiotemporal analysis
description The phased-array weather radar (PAWR) is a new-generation weather radar that can make a 100-m-resolution three-dimensional (3D) volume scan every 30 s for 100 vertical levels, producing ~100 times more data than the conventional parabolic-antenna radar with a volume scan typically made every 5 min for 15 scan levels. This study takes advantage of orders of magnitude more rapid and dense observations by PAWR and explores high-precision nowcasting of 3D evolution at 1-10-km scales up to several minutes, which are compared with conventional horizontal two-dimensional (2D) nowcasting typically at O(100) km scales up to 1-6 h. A new 3D precipitation extrapolation system was designed to enhance a conventional algorithm for dense and rapid PAWR volume scans. Experiments show that the 3D extrapolation successfully captured vertical motions of convective precipitation cores and outperformed 2D nowcasting with both simulated and real PAWR data. © 2016 American Meteorological Society.
title Precipitation nowcasting with three-dimensional space-time extrapolation of dense and frequent phased-array weather radar observations
title_short Precipitation nowcasting with three-dimensional space-time extrapolation of dense and frequent phased-array weather radar observations
title_full Precipitation nowcasting with three-dimensional space-time extrapolation of dense and frequent phased-array weather radar observations
title_fullStr Precipitation nowcasting with three-dimensional space-time extrapolation of dense and frequent phased-array weather radar observations
title_full_unstemmed Precipitation nowcasting with three-dimensional space-time extrapolation of dense and frequent phased-array weather radar observations
title_sort precipitation nowcasting with three-dimensional space-time extrapolation of dense and frequent phased-array weather radar observations
publishDate 2016
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08828156_v31_n1_p329_Otsuka
http://hdl.handle.net/20.500.12110/paper_08828156_v31_n1_p329_Otsuka
_version_ 1768543329254899712