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1 No pp Climatological Characteristics of Local Wind in the Tokachi District, Hokkaido, JAPAN Takashige KAWAI, Mai NAKAJYO, Hisashi KATO and Shuji YAMAKAWA Received September 30, 2007 Climatological characteristics of local strong wind in the Tokachi district are analyzed. Strong wind appeared most frequently in April, while not in January and August. Approximately 70% of strong wind blew in the wind direction of WNW. The strong winds are classified into 4 types judging from air temperature and water vapour pressure. These are 1) Type Fw accompanies Foehn with rain on the windward mountain side. 2) Type Fd, Foehn without rain on the windward mountain side. 3) Type B, Bora. 4) Type N, no substantial change of air temperature and water vapour pressure. The strong wind is also classified into 3 types depending on the wind flow patterns in Tokachi district. Type 1 is divergence pattern both in south and north side of Tokachi district. Type 2 is divergence pattern in south side. Type 3 is divergence pattern in the northern part. Type 1 occurred under the stable layer in the lower troposphere and accompanies foehn phenomenon. Type 2 occurred under the strong stable layer in the lower troposphere with a north wind. Type 3 appeared in the unstable layer in the lower troposphere. From these results, the various strong wind flow patterns in the Tokachi district are mainly controlled by the stability in the lower atmosphere and 850hPa wind direction. Keywords: local Wind, Tokachi, Foehn, Bora, hydraulic jump km Kato, km 3 : : : Department of Geosystem Sciences, College of Humanities and Sciences, Nihon University32540 Sakurajosui Setagaya-ku, Tokyo, Japan Focus System Corporation: Higashi-Gotanda, Shinagawa-ku, Tokyo, Japan Central Research Institute of Electric Power Industry: Ohtemachi, Chiyoda-ku, Tokyo, Japan

2 m hPa NCEP NCAR km 7 9km Ishihara et al., m/s 0.1m/s10m/s

3 m/s 7.5m/s 3 7.5m/s m/s 1 7.5m/s 7.5m/s 7.5m/s m/s

4 Fw 2 Fd 3 B 4 N hPa Fd 1514 Fd Fw Fw B B N N

5 3 4 Fw 7 27Fd 312B 5 19N 1142 Fw Fd A B C A C 1 AB CB C B A A B CB

6 Temperature [deg C] Vapor Pressure [hpa] Fd Temperature [deg C] Vapor Pressure [hpa] Fw Temperature [deg C] Vapor Pressure [hpa] B Temperature [deg C] Vapor Pressure [hpa] N m/s 5m/s

7 4 N N FwFdBN AC 14-1 C C B A C A I

8 Richardson,1920 Ri g z 2 U z K Um/szm g9.8m/s 2 Ri 1 Ri 1 Holland Ri 1/4 2000/z 2006 Ri U/z Ri 49m 1614m 49m 1614m 6 850hPa 12 49m 1614m 5 1/ Fw m/s m/s Fw Fd Fw FdB N Fw FdB

9

10

11

12 5 49m 1614m hPa NCEP/NCAR Temperature [deg C] Temperature [deg C]

13 北海道十勝地方の局地風 十勝風 の気候学的特徴 図6 ウインドプロファイラ観測による上空の風 2002 年 6 月 9 日 10 日

14

15 7 850hPa 8 850hPa 850hPa 850hPa 850hPa 850hPa hPa hPa 5 11/ hPa

16 3 850hPa 1/ p. Holland, J.Z.(1952) : The diffusion problem in hilly terrain. Air Pollution, Ishihara, M., Kato, Y., Abo, T., Kobayashi, K. and Izumikawa, Y. (2006) : Characteristics and Performance of the Operational Wind Profiler Network of the Japan Meteorological Agency. Journal of the Meteorological Society of Japan, 84(6), Kato, H. (1983) : Air Current System in Hokkaido An Analysis Using Wind Vector Composition Method. Reprinted from the Environmental Science, Hokkaido, 6(2), and p p. Richardson, L. F. (1920) : The supply of energy from and to atmospheric eddies. Proc. Roy. Soc., A97, A p p p

No pp The Relationship between Southeast Asian Summer Monsoon and Upper Atmospheric Field over Eurasia Takeshi MORI and Shuji YAMAKAWA

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