The Extraction of Katsuobushi by Electrolyzed Water.

Kobayashi, Kenji; Yamasaki, Yukikazu; Tosa, Noriteru; Hara, Yasuo; Horie, Shuuji

doi:10.3136/nskkk.44.508

Cited by 4 publications

(1 citation statement)

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“…Many waterspouts (non-supercell tornadoes), occur near the coastline of Japan. Kobayashi et al (1997) described the morphology and structures of waterspouts that formed over Tosa Bay on October 4, 1994. Tornadoes not only occur along the Pacific coast of Japan, but also along the Japan Sea coast during winter.…”

Section: Introductionmentioning

confidence: 99%

Doppler Radar Observation of a Tornado Generated Over the Japan Sea Coast during a Cold Air Outbreak

Kobayashi¹,

Sugimoto²,

Suzuki³

et al. 2007

Journal of the Meteorological Society of Japan

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On January 18, 2001, a tornado formed over the Japan Sea near the Mikuni Town on the Hokuriku Coast of Japan. The ''Mikuni Tornado'' formed within a winter thundercloud, during a period of a cold air outbreak, and heavy snowfall. The detailed structure of the tornado funnel cloud, and misocyclone within the cloud are revealed from photographs, videotape, Doppler radar data, and the GPS sonde data. The tornado was generated 3 km offshore, close to the radar site. The tornado formed at the edge of a developing cell, had a single funnel, and was accompanied by a misocyclone near the cloud base; the position of the misocyclone corresponded well with a funnel cloud. The misocyclone had a diameter of 400-800 m and vorticity of 10 À1 s À1 , and coincided with the tornado funnel vortex in the cloud base. The funnel cloud had diameters of 150 m at the cloud base and 30 m near the surface, and a vorticity of 10 0 s À1 . Although the funnel diameter at the cloud base changed remarkably during the life cycle of the tornado, the diameter near the surface remained largely unchanged. The funnel cloud began to dissipate after landing. The maximum wind speed of the tornado vortex is estimated to have been approximately 30 ms À1 (F0-scale), and the lifetime of the funnel cloud was 7 minutes. No damage or strong winds were recorded at the coastal radar site, which was located about 1 km from the tornado. The environmental feature that generated the Mikuni Tornado was vertical wind shear of the sub-cloud layer (3:5 Â 10 À2 s À1 ). The tornado was a non-supercell type tornado that formed under the uniform winter monsoon. This result indicates that small-scale snowclouds can produce tornadoes during periods of cold air outbreaks.

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Section: Introductionmentioning

confidence: 99%

Doppler Radar Observation of a Tornado Generated Over the Japan Sea Coast during a Cold Air Outbreak

Kobayashi¹,

Sugimoto²,

Suzuki³

et al. 2007

Journal of the Meteorological Society of Japan

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一戸¹,

後藤²,

藤原³

2004

Nihon Chikusan Gakkaiho

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