SSI MUCAPE3km SReH 3kmMEANSHR VGP EHIMAX (a) (b) 1 ae (c)
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1 No pp The Characteristics of Tornados Accompanied with Typhoons in Japan from the Viewpoint of their Generating Field Patterns and their Indices Kazuaki OKABE and Shuji YAMAKAWA Received October 31, 2008 We classified tornados outbreak into three patterns, i.e. the inner-band pattern, the outer-band pattern and the coastal front pattern, based on the outbreak position of tornados associated with typhoons. 37 tornados occurred in Japan during were analyzed form the viepoint of atomospheric parameters of the observation data at upper air observatories. As a result, a spacial peak of the outbreak was found in the vicinity of 300km and 500km to the north through eastnortheast of the typhoon center, and the number of the tornados for each pattern was 4, 19, 11, respectively. In addition, the relationships between the pattern of tornados and the atmospheric parameters were not clearly recognized, because of the spatial, tempral gaps. Keywords: typhoon, tornado, inner-band, outer-band, coastal front, Atomospheric parameter m/s 34knot/s km McCaul, km 1000km 2007 coastal front : : Graduate School of Integrated Basic Sciences, Nihon University: Sakurajosui Setagaya-ku, Tokyo, Japan Department of Geosystem Science, College of Humanities and Sciences, Nihon University: Sakurajosui Setagaya-ku, Tokyo, Japan
2 SSI MUCAPE3km SReH 3kmMEANSHR VGP EHIMAX (a) (b) 1 ae (c)
3 (d) 3.1 W. M. Frank 1977 (e) 3.2 CAPE LFC LNB CAPE Z LCL Z LNB gr Tp Ta 1/p [J/kg] R 287J/kg K Tp [ ] Ta [ ] U V W
4 SSI 500hPa 850hPa LCL 500hPa U V W SReH 積乱雲に流入 上昇する気塊が運び込む回転 ( 渦 ) の 大きさの目安を表す SReH h kv Z CV Z / Z dz 0 Vm/s C m/s h km SReH 150 SReH F0 F1 SReH F2 F3 U V W MEANSEAR MEANSEAR hkm SReH MEANSEAR 0-h { h 0 V/ Z dz}/{ h 0 dz} VGP Vorticity Generation Parameter VGP / tilt VGP S CAPE 1/2 S h wcape 1/2 VGPd /dt tilt , 300km 500km 2, 1000km 1200km EHI EHI CAPE SREH EHI CAPE SReH / EHI 1.0 EHI 2.0 EHI 4.0 Raumussen and Blanchard 1998 U V W
5 km 2 300km 500km 3 500km km /h 1 5m/smm/h
6 km /h 1 5m/s mm/h
7 /h 1 5m/smm/h m/s SSI CAPE SReH MEANSHR BRNshr VGP EHI 2 MEANSHR SSI CAPE BRNshr McCaul 1991 SSI 3.0 CAPE 2500J/kg 1 McCaul 1991 BRNshr Weisman and Klemp <BRN<35 SReH SReH 150m 2 /s 2 VGP EHI km 500km,
8 2 SSI CAPE SReH MEANSHR BRNshr VGP EHIMX 1998/1017/ /0924/ /0905/ /0903/ /0903/ /0916/ /0924/ /0822/ /0910/ /0619/ /0807/ /0808/ /0808/ /0929/ /0917/ /0918/ /0921/ /0911/ /0710/ /0912/ /0916/ /0911/ /0930/ km SReH BRNshr CAPE CIN
9 GMS B McCaul, E.W., Jr 1991Buoyancy and shear characteristics of hurricane-tornado environments. Mon,Wea Rev, pp B Weisman, M.L. and Klemp, J.B. 1982The dependence of numerically simulated convective storms on vertical wind shear and buoyancy. Mon. Wea. Rev., 110,
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