start-ver=1.4
cd-journal=joma
no-vol=20
cd-vols=
no-issue=1
article-no=
start-page=13
end-page=24
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=2013
dt-pub=20131227
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=A case study on the rainfall distribution over the Japan Islands associated with the approach of Ty0423 in late October (Comparison with that for Ty0418)
kn-title=2004年10月後半の台風23号に伴う日本列島での広域の降水（台風18号と比較して）
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=Rainfall distribution in the Japan Islands associated with the approach of Typhoon No.23 around 20 October
2004 (referred to Ty0423, hereafter) showed considerably different features from those in late summer of this
year. The present study examined the detailed rainfall features around the Japan Islands brought by Ty0423
and the atmospheric processes based on the operational observation data by the Japan Meteorological Agency
(JMA), comparing with those in association with Ty0418 around 7 September 2004.
During the stage when Ty0423 was approaching or landing on the western part of the Japan Islands, the
areal mean precipitation from Kyushu to Kanto District attained much larger than that for Ty0418, with wider
extension of the area with the large amount of precipitation. It is interesting that, although the intense rainfall
was observed only at the upstream side of the mountain range from Kyushu to Honshu District for Ty0418
except for the area near its center, strong rainfall with 10~30 mm/h persisted in wider regions from the western
to the eastern part of the Japan Islands, resulting in the considerably large total rainfall for Ty0423.
As for the case for Ty0423, the surface front with stable frontal surface was located just to the east of the
Ty0423 center just before its landing at the Japan Islands. Thus, the huge moisture inflow mainly in the eastern
region from the typhoon center seems to be redistributed widely over the Japan Islands area associated with
the large-scale convergence around the stable frontal surface. In late October, the colder air associated with
the high pressure system in the eastern Siberia can cover the northern part of the Japan Sea area as the seasonal
march. Such basic field might be favorable for sustaining the synoptic-scale front just around the southern
coast of the Japan Islands, even when the strong southerly wind invades associated with the typhoon approach
there.
en-copyright=
kn-copyright=

en-aut-name=SatakeAi
en-aut-sei=Satake
en-aut-mei=Ai
kn-aut-name=佐竹愛
kn-aut-sei=佐竹
kn-aut-mei=愛
aut-affil-num=1
ORCID=

en-aut-name=KatoKuranoshin
en-aut-sei=Kato
en-aut-mei=Kuranoshin
kn-aut-name=加藤　内藏進
kn-aut-sei=加藤　
kn-aut-mei=内藏進
aut-affil-num=2
ORCID=

en-aut-name=MoriYoshinori
en-aut-sei=Mori
en-aut-mei=Yoshinori
kn-aut-name=盛宣誠
kn-aut-sei=盛
kn-aut-mei=宣誠
aut-affil-num=3
ORCID=

en-aut-name=GodaYasuhiro
en-aut-sei=Goda
en-aut-mei=Yasuhiro
kn-aut-name=合田泰弘
kn-aut-sei=合田
kn-aut-mei=泰弘
aut-affil-num=4
ORCID=

en-aut-name=IkedaShoichiro
en-aut-sei=Ikeda
en-aut-mei=Shoichiro
kn-aut-name=池田祥一郎
kn-aut-sei=池田
kn-aut-mei=祥一郎
aut-affil-num=5
ORCID=

en-aut-name=TsukamotoOsamu
en-aut-sei=Tsukamoto
en-aut-mei=Osamu
kn-aut-name=塚本修
kn-aut-sei=塚本
kn-aut-mei=修
aut-affil-num=6
ORCID=

affil-num=1
en-affil=
kn-affil=

affil-num=2
en-affil=
kn-affil=岡山大学大学院教育学研究科

affil-num=3
en-affil=
kn-affil=

affil-num=4
en-affil=
kn-affil=

affil-num=5
en-affil=
kn-affil=岡山大学大学院自然科学研究科

affil-num=6
en-affil=
kn-affil=岡山大学大学院自然科学研究科
en-keyword=Ty0423
kn-keyword=Ty0423
en-keyword=Ty0418
kn-keyword=Ty0418
en-keyword=rainfall in Japan associated with a typhoon in mid-autumn
kn-keyword=rainfall in Japan associated with a typhoon in mid-autumn
en-keyword=effects of a typhoon on the synoptic climatology in Japan in October
kn-keyword=effects of a typhoon on the synoptic climatology in Japan in October
END

start-ver=1.4
cd-journal=joma
no-vol=19
cd-vols=
no-issue=1
article-no=
start-page=39
end-page=50
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=2012
dt-pub=20121226
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=A case study on persistent appearance of the ensemble of precipitation bands in the warm sector of the Baiu front in the western Japan around 19 June 2001
kn-title=地上梅雨前線の南方の九州における 線状降水帯の集団の維持について （2001年6月19日頃の事例解析）
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=A case study on persistent appearance of the ensemble of precipitation bands in the warm sector of the Baiu front in
Kyushu District, the western part of Japan around 19 June 2001 was performed based on the operational observational
data. Around 00UTC (09JST) 19 June when the Baiu front on the surface weather map was still located about a few
100kms to the north of Kyushu, the number and the total area of the meso-β or γ-scale line-shaped precipitation
bands increased around Kyushu rapidly. These precipitation bands had been sustained there and gradually gathered
each other to change into the Baiu frontal precipitation zone extending from the northern Kyushu to Seto-Naikai (Seto
Inland Sea) around 09UTC (18JST) 19 June (the intense rainfall zone was still located in the warm sector of the Baiu
front).
Until ~09UTC (18JST) 19 June, the moist air flow with the latently unstable stratification had been sustained
around Kyushu corresponding to the low-level southerly wind toward the surface Baiu front to the north of Kyushu.
This large-scale situation would contribute greatly to the maintenance of the ensemble of the line-shaped precipitation
bands in the warm sector of the Baiu front.
en-copyright=
kn-copyright=

en-aut-name=GodaYasuhiro
en-aut-sei=Goda
en-aut-mei=Yasuhiro
kn-aut-name=合田泰弘
kn-aut-sei=合田
kn-aut-mei=泰弘
aut-affil-num=1
ORCID=

en-aut-name=KatoKuranoshin
en-aut-sei=Kato
en-aut-mei=Kuranoshin
kn-aut-name=加藤内藏進
kn-aut-sei=加藤
kn-aut-mei=内藏進
aut-affil-num=2
ORCID=

en-aut-name=TsukamotoOsamu
en-aut-sei=Tsukamoto
en-aut-mei=Osamu
kn-aut-name=塚本修
kn-aut-sei=塚本
kn-aut-mei=修
aut-affil-num=3
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学大学院教育学研究科

affil-num=2
en-affil=
kn-affil=岡山大学大学院教育学研究科自然教育学系理科教育講座

affil-num=3
en-affil=
kn-affil=岡山大学大学院自然科学研究科
en-keyword=ensemble of line-shaped precipitation bands
kn-keyword=ensemble of line-shaped precipitation bands
en-keyword=precipitation in the warm sector of the Baiu front
kn-keyword=precipitation in the warm sector of the Baiu front
en-keyword=Baiu fronal rainfall
kn-keyword=Baiu fronal rainfall
END