Combined wind profiler-weather radar observations of orographic rainband around Kyushu, Japan in the Baiu season

A special observation campaign (X-BAIU), using various instruments (wind profilers, <i>C</i>-band weather radars, <i>X</i>-band Doppler radars, rawinsondes, etc.), was carried out in Kyushu (western Japan) during the Baiu season, from 1998 to 2002. In the X-BAIU-99 and -...

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Main Authors: Y. Umemoto, M. Teshiba, Y. Shibagaki, H. Hashiguchi, M. D. Yamanaka, S. Fukao, X-BAIU-99, X-BAIU-02 observational groups
Format: Article
Language:English
Published: Copernicus Publications 2004-11-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/22/3971/2004/angeo-22-3971-2004.pdf
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author Y. Umemoto
M. Teshiba
Y. Shibagaki
H. Hashiguchi
M. D. Yamanaka
M. D. Yamanaka
S. Fukao
X-BAIU-99
X-BAIU-02 observational groups
author_facet Y. Umemoto
M. Teshiba
Y. Shibagaki
H. Hashiguchi
M. D. Yamanaka
M. D. Yamanaka
S. Fukao
X-BAIU-99
X-BAIU-02 observational groups
author_sort Y. Umemoto
collection DOAJ
description A special observation campaign (X-BAIU), using various instruments (wind profilers, <i>C</i>-band weather radars, <i>X</i>-band Doppler radars, rawinsondes, etc.), was carried out in Kyushu (western Japan) during the Baiu season, from 1998 to 2002. In the X-BAIU-99 and -02 observations, a line-shaped orographic rainband extending northeastward from the Koshikijima Islands appeared in the low-level strong wind with warm-moist airs. The weather radar observation indicated that the rainband was maintained for 11h. The maximum length and width of the rainband observed in 1999 was ~200km and ~20km, respectively. The rainband observed in 2002 was not so developed compared with the case in 1999. The Froude number averaged from sea level to the top of the Koshikijima Islands (~600m) was large (&gt;1), and the lifting condensation level was below the tops of the Koshikijima Islands. Thus, it is suggested that the clouds organizing the rainband are formed by the triggering of the mountains on the airflow passing over them. The vertical profile of horizontal wind in/around the rainband was investigated in the wind profiler observations. In the downdraft region 60km from the Koshikijima Islands, strong wind and its clockwise rotation with increasing height was observed below 3km altitude. In addition, a strong wind component perpendicular to the rainband was observed when the rainband was well developed. These wind behaviors were related to the evolution of the rainband.
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spelling doaj.art-1cd8e6d46483478d91eee3636ea300d32022-12-22T03:16:00ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762004-11-01223971398210.5194/angeo-22-3971-2004Combined wind profiler-weather radar observations of orographic rainband around Kyushu, Japan in the Baiu seasonY. Umemoto0M. Teshiba1Y. Shibagaki2H. Hashiguchi3M. D. Yamanaka4M. D. Yamanaka5S. Fukao6X-BAIU-99X-BAIU-02 observational groups7Research Institute for Sustainable Humanosphere, Kyoto University, Uji, Kyoto 611–0011, JapanResearch Institute for Sustainable Humanosphere, Kyoto University, Uji, Kyoto 611–0011, JapanOsaka Electro-Communication University, Neyagawa, Osaka 572–8530, JapanResearch Institute for Sustainable Humanosphere, Kyoto University, Uji, Kyoto 611–0011, JapanGraduate School of Science and Technology, Kobe University, Kobe 657–8501, JapanInst. of Observ. Res. for Global Change, Japan Agency for Marine-Earth Science and Techn., Yokohama 236–0001, JapanResearch Institute for Sustainable Humanosphere, Kyoto University, Uji, Kyoto 611–0011, JapanMeteorological Research Institute, Japan Meteorological Agency, Tsukuba, Ibaraki 305–0052, JapanA special observation campaign (X-BAIU), using various instruments (wind profilers, <i>C</i>-band weather radars, <i>X</i>-band Doppler radars, rawinsondes, etc.), was carried out in Kyushu (western Japan) during the Baiu season, from 1998 to 2002. In the X-BAIU-99 and -02 observations, a line-shaped orographic rainband extending northeastward from the Koshikijima Islands appeared in the low-level strong wind with warm-moist airs. The weather radar observation indicated that the rainband was maintained for 11h. The maximum length and width of the rainband observed in 1999 was ~200km and ~20km, respectively. The rainband observed in 2002 was not so developed compared with the case in 1999. The Froude number averaged from sea level to the top of the Koshikijima Islands (~600m) was large (&gt;1), and the lifting condensation level was below the tops of the Koshikijima Islands. Thus, it is suggested that the clouds organizing the rainband are formed by the triggering of the mountains on the airflow passing over them. The vertical profile of horizontal wind in/around the rainband was investigated in the wind profiler observations. In the downdraft region 60km from the Koshikijima Islands, strong wind and its clockwise rotation with increasing height was observed below 3km altitude. In addition, a strong wind component perpendicular to the rainband was observed when the rainband was well developed. These wind behaviors were related to the evolution of the rainband.https://www.ann-geophys.net/22/3971/2004/angeo-22-3971-2004.pdf
spellingShingle Y. Umemoto
M. Teshiba
Y. Shibagaki
H. Hashiguchi
M. D. Yamanaka
M. D. Yamanaka
S. Fukao
X-BAIU-99
X-BAIU-02 observational groups
Combined wind profiler-weather radar observations of orographic rainband around Kyushu, Japan in the Baiu season
Annales Geophysicae
title Combined wind profiler-weather radar observations of orographic rainband around Kyushu, Japan in the Baiu season
title_full Combined wind profiler-weather radar observations of orographic rainband around Kyushu, Japan in the Baiu season
title_fullStr Combined wind profiler-weather radar observations of orographic rainband around Kyushu, Japan in the Baiu season
title_full_unstemmed Combined wind profiler-weather radar observations of orographic rainband around Kyushu, Japan in the Baiu season
title_short Combined wind profiler-weather radar observations of orographic rainband around Kyushu, Japan in the Baiu season
title_sort combined wind profiler weather radar observations of orographic rainband around kyushu japan in the baiu season
url https://www.ann-geophys.net/22/3971/2004/angeo-22-3971-2004.pdf
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