Publication list

Reviewed papers

[28] Campbell, L.S., W. J. Steenburgh, Y. Yamada, M. Kawashima, and Y. Fujiyoshi 2018: Influences of orography and coastal geometry on a transverse-mode sea-effect snowstorm over Hokkaido Island, Japan. Mon. Wea. Rev., 146, 2201-2220, doi:10.1175/MWR-D-17-0286.1.
[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--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.


Last updated: August 19, 2012

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