論文リスト

原著論文

[27] Kawashima, M. 2016: The role of vertically propagating gravity waves forced by melting-induced cooling in the formation and evolution of wide cold-frontal rainbands J. Atmos. Sci., 73, 2803-2836, doi:10.1175/JAS-D-15-0163.1.
 
[26] Yagnesh, R. Y., T. Nakamura, H. Mitsudera, and M. Kawashima, 2014: Formation and maintenance mechanisms of a thick snow band along the Okhotsk Sea coast of Hokkaido Island, Japan. Hydrological Res. Lett.,8 (2), 84-89. doi: 10.3178/hrl.8.84.
   
[25] Sakurai, N., S. Mori, M. Kawashima, Y. Fujiyoshi, J.-I. Hamada, S. Shimizu, H. Fudeyasu, Y. Tabata, W. Harjupa, H. Hashiguchi, M. D., Yamanaka, J. Matsumoto, Emirizal, and F. Syamsudin, 2011: Migration process and 3D wind field of precipitation systems associated with a diurnal cycle in west Sumatera: Dual Doppler radar analysis during the HARIMAU2006 campaign. J. Meteor. Soc. Japan, 89, 341-361.
   
[24] Kawashima, M. 2011: Numerical study of horizontal shear instability waves along narrow cold frontal rainbands.J. Atmos. Sci., 68, 878-903.
   
[23] Kawashima, M. ,Y. Fujiyoshi, M. Ohi, S. Mori, N. Sakurai,Y. Abe, W. Harjupa, F.  Syamsudin, and M. D. Yamanaka, 2011: Case study an intense wind event associated with a mesoscale convective system in west Sumatera during the HARIMAU2006 campaign.J. Meteor. Soc. Japan,  89A, 239-257.
   
[22] Mori, S., J. I. Hamada, N. Sakurai, H. Fudeyasu, M. Kawashima, H. Hashiguchi, F. Syamsudin, A. A. Arbain, R. Sulistyowati, J. Matsumoto, and M. D. Yamanaka, 2011: Convective systems developed along the coastline of Sumatera island,Indonesia, observed with an X-band Doppler radar during the HARIMAU2006 campaign. J. Meteor. Soc. Japan, 89(A), 61-81.
   
[21] Ohtake, H, M. Kawashima and Y. Fujiyoshi, 2009: The formation mechanism of a thick cloud band over the northern part of the Sea of Japan during cold air outbreaks.J. Meteor. Soc. Japan, 87(2), 289-306.
   
[20] Kozu, T., Y. Kodama, Y. Shibagaki, T. Shimonai, M. Kawashima, and S. Alexander, 2008: Diurnal and intraseasonal variation of UTLS vertical wind disturbance in equatorial region and its relation to tropospheric convective activities. Earth, Planets and Space, 61(4), 535-544.
   
[19] Sakurai, N., M. Kawashima, Y. Fujiyoshi, H. Hashiguchi, T. Shimomai, S. Mori, J.-I. Hamada, F. Murata, M. D. Yamanaka, Y-I Tauhid, T. Sribimawati and B. Suhardi, 2008: Internal structures of migratory cloud systems with diurnal cycle over Sumatera Island during CPEA-I campaign.J. Meteor. Soc. Japan, 87 (1), 157-170
   
[18] Yamanaka, M. D., H. Hashiguchi, S. Mori, P. Wu, F. Syamsudin, T. Manik, Hamada J.-I., M.K.Yamamoto, M. Kawashima, Y. Fujiyoshi, N. Sakurai, M. Ohi, R. Shirooka,M. Katsumata, Y. Shibagaki, T. Shimomai, Erlansyah, W. Setiawan,Bambang Tejasukmana, Yusuf S. Djajadihardja,and J. T. Anggadiredja, 2008: HARIMAU Radar-Profiler Network over the Indonesian Maritime Continent: A GEOSS early achievement for hydrological cycle and disaster prevention.Journal of Disaster Research, 3(1), 78-88.
   
[17] Kawashima. M., 2007: Numerical study of precipitation core-gap structure along cold fronts. J. Atmos. Sci., 64, 2355-2377
   
[16] Li, Z., T. Takeda, K. Tsuboki, K. Kato, M. Kawashima and Y. Fujiyoshi, 2007: Nocturnal evolution of cloud clusters over eastern China during the intensive observation periods of GAME/HUBEX in 1998 and 1999. J. Meteor. Soc. Japan, 85, 25-45.
   
[15] Renggono, F., M. K. Yamamoto, H. Hashiguchi, S. Fukao, T. Shimomai, M. Kawashima, and M. Kudsy, 2006: Raindrop size distribution observed with the Equatorial Atmosphere Radar (EAR) during the CPEA-I observation campaign. Radio Sci., 41, RS5002, doi:10.1029/2005RS003333.
   
[14] Mori, S., J. Hamada, M.-D. Yamanaka, Y.-M. Kodama, M. Kawashima, T. Shimomai, Y. Shibagaki, H. Hashiguchi, T. Sribimawati and B. Suhardi, 2006: Vertical wind characteristics in precipitating cloud systems over west Sumatera, Indonesia, observed with Equatorial Atmosphere Radar: Case study of 23-24 April 2004 during the first CPEA campaign period. J. Meteor. Soc. Japan, 84A, 113-131.
   
[13] Kawashima, M., Y. Fujiyoshi, M. Ohi, T. Honda, T. Kozu, T. Shimomai, and H. Hashiguchi, 2006: Overview of Doppler radar observations of precipitating cloud systems in Sumatera Island during the first CPEA campaign. J. Meteor. Soc. Japan, 84A, 33-56.
   
[12] Alexander, S., T. Tsuda, J. Furumoto, T. Shimomai, T. Kozu, and M. Kawashima, 2006: A statistical overview of tropospheric convection during the first CPEA campaign.J. Meteor. Soc. Japan, 84A, 57-93.
   
[11] Inoue, J., M. Kawashima, Y.Fujiyoshi and M. Wakatsuchi, 2005: Aircraft observations of air mass modification over the Sea of Okhotsk during sea-ice growth. Boundary Layer Meteorology, 117, 111-129.
   
[10] Inoue, J., M. Kawashima, Y.Fujiyoshi and Y. Yoshizaki, 2005: Aircraft observations of air mass modification in the upstream region of the Sea of Japan during cold-air outbreaks. J. Meteor. Soc. Japan, 83, 189-200.
   
[9] Kawashima, M., and Y. Fujiyoshi, 2005: Shear instability wave along a snowband: Instability structure, evolution and energetics derived from dual-Doppler radar data. J. Atmos. Sci., 62, 351-370.
   
[8] Yoshihara, H., M. Kawashima, K. Arai, J. Inoue and Y. Fujiyoshi, 2004: Doppler radar study on the successive development of the band-shaped snow clouds at a convergence line near the coastal region of Hokuriku district. J. Meteor. Soc. Japan, 82, 1057-1079.
   
[7] Ushiyama, T., M. Kawashima, and Y. Fujiyoshi, 2003: Heating distribution by cloud systems derived from Doppler radar observation in TOGA-COARE. J. Meteor. Soc. Japan, 81, 1407-1434.
   
[6] Kawashima, M., 2003: The role of gravity waves in the meso-β-scale cycle of squall-line type mesoscale convective systems. J. Meteor. Soc. Japan, 81, 713-746.
   
[5] Inoue, J., M. Honda and M. Kawashima, 2001: Air mass transformation processes over the southwestern region of the ice-covered Sea of Okhotsk during cold air outbreaks. J. Meteor. Soc. Japan, 79, 657-670.
   
[4] Redelsperger, J. L., P. R. A. Brown., F. Guichard., C. Hoff., M. Kawashima, S. Lang, Th. Montmerle, K. Nakamura, K. Saito, C. Seman, and W. K. Tao, 2000: A GCSS model intercomparison for a tropical squall line observed during TOGA-COARE. Part 1: Cloud-resolving models. Quart. J. Royal Meteor. Soc., 126, 823-864.
   
[3] Inoue, J., M. Kawashima, K. I. Ohsima, Y. Fujiyoshi and K. Maruyama, 2000: Wind fields over Funka bay and their effects on water circulation in the bay. J. Oceanography, 56, 507-515.
   
[2] Kawashima, M., K. Tsuboki and T. Asai, 1995: Maintenance mechanism and thermodynamic structure of a Baiu frontal rainband retrieved from dual Doppler radar observations. J. Meteor. Soc. Japan, 73, 717-735.
   
[1] Tada, T., Y. Tsuji, T. Tsukamoto, Y. Ueno, M. Kawashima, T. Egawa and Y. Yamazaki, 1992 : Comparison of observed and theoretically calculated seiches of Heda Bay, Japan, PAGEOPH, 139, 309-322.

著書

北海道大学低温科学研究所編 (2015): 低温科学便覧 第12章「雲科学〜メソスケール渦状降雪雲の力学、温帯低気圧に伴う降雨帯形成に果たす雪の融解冷却効果」263-271 (2015)

在田一則、竹下徹、見延庄士郎、渡部重十 編著 (2010): 地球惑星科学入門 第22章「天気を支配する諸現象」pp.427

川島正行 (2005): 水平風シアライン上に発生する渦状擾乱の基礎的数値実験. 気象研究ノート「メソ対流系の構造と発生・発達のメカニズム (吉崎正憲、加藤輝之、村上正隆編集)」, 285-292.

吉原華子、 川島正行、藤吉康志 (2005): ドップラーレーダ観測による北陸沿岸の収束線上における降雪バンドの連続的発達に関する研究. 気象研究ノート「メソ対流系の構造と発生・発達のメカニズム (吉崎正憲、加藤輝之、村上正隆編集)」, 333-345.

猪上淳、川島正行、藤吉康志 (2005): ロシア航空機による境界層観測. 気象研究ノート 「メソ対流系の構造と発生・発達のメカニズム(吉崎正憲、加藤輝之、村上正隆編集)」,221-232.

川島正行 (2004): 渦状降雪雲の基礎的数値実験. 月刊海洋号外, 38, 140-144.    

 

Last updated: April 21, 206