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...
Main Authors: | , , , |
---|---|
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 |
_version_ | 1829314285051838464 |
---|---|
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 |