メカニズム と 数値モデル            山 岬 正 紀      ...

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2011.9.13 -14 (京都). ( 台風セミナー) 台風の 発生過程 と 非軸対称構造 の力学. メカニズム と 数値モデル            山 岬 正 紀       海洋研究開発機構          地球環境変動領域. この資料での紫色での記述は講演後の追記である。. 講演資料と参考文献は、実行委員の配慮で、 事前に参加者が見れるようになっていたので、 通常の講演形式ではなく、ごく要点のみにふれ、 多くの時間を質問、議論に充てる形式をとった。 したがって、 2時間30分 (休憩時間を除いて) の - PowerPoint PPT Presentation

Transcript of メカニズム と 数値モデル            山 岬 正 紀      ...

  • 2011.9.13 -14

  • [ (CISK) ] Conditional Instability of the Second Kind (1) 1960 CISK Ooyama (1964), Charney and Eliassen (1964) CISK Syono (1949), Charney and Eliassen (1949) (1996)

  • (2) 197080 Yamasaki (1975, 77a,b, 79, 83) * 5-6 m/s 10 m/s frictional inflow 1960 CISK CISK) (15-20m/s * 1960CISK 1 m/s)

  • (3) Rotunno and Emanuel (1987) wind induced surface heat exchange (WISHE) Ooyama (1969) Malkus and Riehl (1960) Yamasaki 60 WISHE CISK CISK Yamasaki (1989b) Emanuel (1987) Ooyama CISK CISK Yamasaki (1989b)

  • (2007) ALCLLFCLCL

  • CISK Yamasaki (1983, 84) wave-CISKCISK Yamasaki (1983, 86) (1) CISK (2) frictional inflow CISK ( frictional inflow CISK )(3) frictional convergence CISK ( frictional convergence CISK ) eyewall circulation 1960CISK (1) 1950CISK Yamasaki (1975) CISK

  • CISK (2003) CISK ( frictionally controlled CISK )CISK ( frictional (frictional inflow) convergence) CISK CISK CISK Kelvin wave CISK gravity wave CISK CISK (ageostrophic CISK) CISK CISK CISK (quasi-geostrophic or quasi-balanced Rossby wave CISK CISK ) CISK 6-10m/s

  • [] (Yamasaki, 1975, 2004) 23 cumulus-convection-resolving model (CCRM) (1 km 100 m) (5 20 km) (1-2 km) mesoscale-convection-resolving model (MCRM) (Yamasaki, 1986, 2001) (Yamasaki, 2010)

  • (cumulus convection) (moist convection) 10 ~ 1930 (mesoscale convection) MC (mesoscale organized convection) (Yamasaki, 1983,1984) . ( 10 and/or MCS

  • (lifetime) ( 3 ) 3 ~ 10 (Yamasaki, 1983,1984)

  • 1950 1950-60 Senn and Hiser (1959) (1961, 1962)

    1940

  • (Matsumoto and Tsuneoka, 1969) 10 (Y(1983) 11 ) (Yamasaki, 1983,1984)

  • 1970 1 (e.g., Takeda, 1971) 1-2

  • and/or

  • (Orlanski, 1975) Yamasaki (1983) (2007)1~2 .. Orlanski (1975) meso- 2 ~ 20 km meso- 20 ~ 200 km meso- 200 ~ 2,000 km

  • meso- (20-100 km) meso-(100-200 km) meso-(200-500 km) meso- (500-2,000 km)

  • [ ] (Yamasaki, 1986) (Yamasaki, 1975, 77a,b, 79, 83, 84) 50 km 20 km

  • [ ]1980 1 km 20 km 1960

  • Manabe et al. (1965), Kuo (1965), Ooyama (1969), Kurihara (1973) Arakawa and Schubert (1974) (1) Ooyama (1964)Kuo (1965)Kurihara (1973) 19601970 (2) Yamasaki (1968a,b,c, 1969, 1971) (3) modify 1970

  • 1980 Yamasaki (1986)

  • 1-5 km 5-20 km

  • ( subgrid-scale Ooyama (1964, 1969) Yamasaki (1968a, b, c) Yamasaki (1969, 1971) realistic

  • mass flux Ooyama (1971), Arakawa and Schubert (1974) cloud mass flux p.29

  • [ ] 5-20 km Anthes (1972), Kurihara and Tuleya (1974) (TC) TC Kurihara and Tuleya (1981)

  • Yamasaki (1986, 1987) Yamasaki (2001) diagnostic prognostic Nasuno and Yamasaki (2001) ( Y (1986) prognostic) a
  • [ ] explicit distinguish Arakawa and Schubert (1974)

  • cloud resolving model (CRM) 1 km () km cloud-resolving

  • 15 km - 20 km 1 km 10 km CPU time 100-1000 520 km

  • *

    5-20 km

    * parameterizability

    (1993)

  • CISK 20 km

  • [ ] (1a) 1987 Yamasaki (1988) xxxxx Yamasaki (1989a) 1990 1991 2004 Yamasaki (2006a) 2005 Yamasaki (2006b) (1b) 2008 Yamasaki (2010) 2008 2009 (2) 2009

  • [] [Yamasaki (1989b) TC] second WMO IWTC rapporteur report (International Workshop on Tropical Cyclones) Yamasaki (2007) 1991

  • Yamasaki (1989b, 2007) conditional instability latent instability latent instability CAPE Yamasaki (1989b) (MC, mesoscale convection) mesoscale organized convection (MCS, ) cloud band mesoscale organized convection Yamasaki (1989b) IWTC MC

  • [ CISK ]

    CISK CISK CISK

    CISK CISK

  • [ ] CISK

    (CISK)

  • MCS MCS - - - -

  • suppress affect (cold surge CISK frictional flow CISK

  • CAPE Yamasaki (1986) MCRM

  • [ ][] [] *

  • []

  • [ ]

    affect ( ISV, 40-50 )ENSO 30-60 (Gray, 1975)

  • Gray (1975) (warm core)

    Yamasaki (1969) frictional convergence CISK Yamasaki (1987)

  • Yamasaki (1989b) TC (TUTT) (UCL) Sadler (1976,1978) 1991

  • Gray (1979) seasonal genesis parameter (convective instability) (latent instability)

  • [ ] Yamasaki (1988,1989a,b) 1950

  • Hendricks et al. (2004) vortical hot tower PV anomaly merge Yamasaki (1989b) Yamasaki (1989b) [ ] merge merge Hendricks et al. Yamasaki (1989b)

  • Hendricks et al. (2004) 200920

  • Hendricks et al. (2004) TC formation stage CISK Yamasaki (1989b) frictional flow

  • [] Ooyama (1982) []

  • [] ( (1a) 1987 Yamasaki (1988) xxxxx Yamasaki (1989a) 1990 1991 2004 Yamasaki (2006a) 2005 Yamasaki (2006b) (1b) 2008 Yamasaki (2010) 2008 2009 (2) 2009

  • [ ]2009

  • []A (1) 1986 Yamasaki (1987)(2) A(1) affect B A(1)

  • []

    1996: CISK, No. 186575-962003: CISK 50, 137-160Yamasaki, M., 1989: Advances in basic understanding of tropical cyclone formation, The second WMO international workshop on tropical cyclones, Manila, WMO Tropical Meteorology Research Programme Report Series, WMO/TD-No. 319, Vol. 1, 125-142.Yamasaki, M, 2007: A view on tropical cyclones as CISK. J. Meteor. Soc. Japan, 85, 145-164.Yamasaki, M., 2010: Development of a nonhydrostatic version of the mesoscale-convection-resolving model and its application to the eyewall and spiral rainbands of tropical cyclones. J. Meteor. Soc. Japan, 88, 755-780.Yamasaki(1989) (1989b) IWTC-II rapporteur report Journal ()