On the estimation of precipitation rate by a new method of analysis of meteorological radar echoes(2) (abstract)

P(論文) At Syowa Station, microwave radar echo data from clouds and precipitation have been accumulated. We have studied how to estimate precipitation rate using observed radar echoes. In this abstract, we report how to evaluate some physical characteristics of precipitation particles, which are impor...

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Main Authors: Hoshiyama,Mitsuo, Hatanaka,Masahiko, Nishitsuji ,Akira, Wada, Makoto
Language:English
Published: National Institute of Polar Research 1993
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3784/files/KJ00000035737.pdf
https://doi.org/10.15094/00003784
https://nipr.repo.nii.ac.jp/records/3784
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author Hoshiyama,Mitsuo
Hatanaka,Masahiko
Nishitsuji ,Akira
Wada, Makoto
author_facet Hoshiyama,Mitsuo
Hatanaka,Masahiko
Nishitsuji ,Akira
Wada, Makoto
author_sort Hoshiyama,Mitsuo
collection National Institute of Polar Research Repository, Japan
description P(論文) At Syowa Station, microwave radar echo data from clouds and precipitation have been accumulated. We have studied how to estimate precipitation rate using observed radar echoes. In this abstract, we report how to evaluate some physical characteristics of precipitation particles, which are important to analyze radar echoes. (1) Temperature of precipitation particles at each altitude : We are able to use temperature data at each altitude, obtained by radiosonde at Syowa Station. But the temperature is usually different from that of precipitation particles. In case of dense particles falling at high speed, this difference tends to increase. In the opposite case, it is considered that particle and air temperatures are equal. In the latter case, characteristics of a precipitation particle are determined by temperature around the particle. (2) Water volume content of precipitation particles : There is an empirical relation between water volume content of snow-flakes (Pw) and particle density ( departmental bulletin paper
genre Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
genre_facet Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
geographic Syowa Station
geographic_facet Syowa Station
id ftnipr:oai:nipr.repo.nii.ac.jp:00003784
institution Open Polar
language English
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003784
op_relation Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
7
91
AA10756213
https://nipr.repo.nii.ac.jp/record/3784/files/KJ00000035737.pdf
https://doi.org/10.15094/00003784
https://nipr.repo.nii.ac.jp/records/3784
publishDate 1993
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003784 2025-04-13T14:25:53+00:00 On the estimation of precipitation rate by a new method of analysis of meteorological radar echoes(2) (abstract) Hoshiyama,Mitsuo Hatanaka,Masahiko Nishitsuji ,Akira Wada, Makoto 1993-09 application/pdf https://nipr.repo.nii.ac.jp/record/3784/files/KJ00000035737.pdf https://doi.org/10.15094/00003784 https://nipr.repo.nii.ac.jp/records/3784 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 7 91 AA10756213 https://nipr.repo.nii.ac.jp/record/3784/files/KJ00000035737.pdf https://doi.org/10.15094/00003784 https://nipr.repo.nii.ac.jp/records/3784 1993 ftnipr https://doi.org/10.15094/00003784 2025-03-19T10:19:57Z P(論文) At Syowa Station, microwave radar echo data from clouds and precipitation have been accumulated. We have studied how to estimate precipitation rate using observed radar echoes. In this abstract, we report how to evaluate some physical characteristics of precipitation particles, which are important to analyze radar echoes. (1) Temperature of precipitation particles at each altitude : We are able to use temperature data at each altitude, obtained by radiosonde at Syowa Station. But the temperature is usually different from that of precipitation particles. In case of dense particles falling at high speed, this difference tends to increase. In the opposite case, it is considered that particle and air temperatures are equal. In the latter case, characteristics of a precipitation particle are determined by temperature around the particle. (2) Water volume content of precipitation particles : There is an empirical relation between water volume content of snow-flakes (Pw) and particle density ( departmental bulletin paper Other/Unknown Material Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan Syowa Station
spellingShingle Hoshiyama,Mitsuo
Hatanaka,Masahiko
Nishitsuji ,Akira
Wada, Makoto
On the estimation of precipitation rate by a new method of analysis of meteorological radar echoes(2) (abstract)
title On the estimation of precipitation rate by a new method of analysis of meteorological radar echoes(2) (abstract)
title_full On the estimation of precipitation rate by a new method of analysis of meteorological radar echoes(2) (abstract)
title_fullStr On the estimation of precipitation rate by a new method of analysis of meteorological radar echoes(2) (abstract)
title_full_unstemmed On the estimation of precipitation rate by a new method of analysis of meteorological radar echoes(2) (abstract)
title_short On the estimation of precipitation rate by a new method of analysis of meteorological radar echoes(2) (abstract)
title_sort on the estimation of precipitation rate by a new method of analysis of meteorological radar echoes(2) (abstract)
url https://nipr.repo.nii.ac.jp/record/3784/files/KJ00000035737.pdf
https://doi.org/10.15094/00003784
https://nipr.repo.nii.ac.jp/records/3784