研究者詳細 - 篠田　太郎

論文 - 篠田　太郎

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Future increase of super-typhoon intensity associated with climate change. 査読有り

Tsuboki, K, M. K. Yoshioka, T. Shinoda, M. Kato, S. Kanada, A. Kitoh

Geophys. Res. Lett. 2014年12月

Polarimetric Doppler radar analysis of organization of a stationary rainband with changing orientations in July 2010. 査読有り

Oue, M., K. Inagaki, T. Shinoda, T. Ohigashi, T. Kouketsu, M. Kato, K. Tsuboki, H. Uyeda

J. Meteor. Soc. Japan 92 巻頁： 457-481 2014年10月

A comparison between the effects of artificial land cover and anthropogenic heat on a localized heavy rain event in 2008 in Zoshigaya, Tokyo, Japan 査読有り

Kazuyoshi Souma, Kenji Tanaka, Tadashi Suetsugi, Kengo Sunada, Kazuhisa Tsuboki, Taro Shinoda, Yuqing Wang, Atsushi Sakakibara, Koichi Hasegawa, Qoosaku Moteki, and Eiichi Nakakita

Journal of Geophysical Research - Atmosphere 118 巻頁： 11600-11610 2013年11月

Maintenance mechanisms of a precipitation band formed along the Ibuki-Suzuka Mountains on September 2-3, 2008 査読有り

Morotomi K., T. Shinoda, Y. Shusse, T. Kouketsu, T. Ohigashi, K. Tsuboki, H. Uyeda, I. Tamagawa

Journal of the Meteorological Society of Japan 90 巻 ( 5 ) 頁： 737-753 2012年10月

Impact of sedimentation of cloud ice on cloud-top height and precipitation intensity of precipitation systems simulated by a cloud-resolving model 査読有り

Nomura, M., K. Tsuboki, T. Shinoda

Journal of the Meteorological Society of Japan 90 巻 ( 5 ) 頁： 791-806 2012年10月

Characteristics of rainfall systems accompanied with Changma front at Chejado in Korea 査読有り

You, C.-H., D.-I. Lee, S.-M. Jang, M. Jang, H. Uyeda, T. Shinoda, F. Kobayashi

Asia-Pacific Journal of Atmospheric Sciences 46 巻頁： 41-51 2010年

*中国華中域における大気境界層・降水システム研究の進展～ GAME/HUBEX 特別集中観測からの10 年～査読有り

篠田太郎・山田広幸・遠藤智史・田中広樹・上田博

天気 56 巻 ( 12 ) 頁： 739-745 2009年12月

担当区分：筆頭著者記述言語：日本語

1998年に中国華中域（淮河流域）で実施されたGAME-HUBEX特別集中観測以降に出版された大気境界層と降水システムについての研究成果のレビューを行った。レビューを行うに際して、水田上の大気境界層過程、梅雨前線帯の南側の領域における大気境界層過程が梅雨前線帯の降水システムに与える影響、梅雨前線帯周辺の降水セルの特徴という３つの視点からまとめた。

Structure of convective circulation in the atmospheric boundary layer over the northwestern Pacific Ocean under a subtropical high. 査読有り

Shinoda, T., A. Higuchi, K. Tsuboki, T. Hiyama, H. Tanaka, S. Endo, H. Minda, H. Uyeda, K. Nakamura

J. Meteor. Soc. Japan 87 巻 ( 6 ) 頁： 979-996 2009年12月

担当区分：筆頭著者記述言語：英語掲載種別：研究論文（学術雑誌）

To confirm the structure of convective circulation in the atmospheric boundary layer (ABL) over the northwestern Pacific Ocean around the Southwest Islands of Japan under a subtropical high, we perform intensive observations using radiosonde and Aerosonde in August 2002 and high-resolution three-dimensional numerical simulations. A well-mixed subcloud layer exists below 0.7 km during the observation period. The absolute values of the correlation coefficient between anomalies in potential temperature and mixing ratio of water vapor are mainly small (less than 0.3) in the lower subcloud layer. The frequency of a positive correlation coefficient at a height of 0.1 km is only 46%. This suggests that fewer warm moist thermals exist in the lower subcloud layer.

The simulation results using 100-m horizontal grid resolution show a moist airmass in updraft regions. These thermals are driven by positive buoyant flux, and this positive buoyancy is contributed by moisture, i.e., density anomalies in water vapor and dry air, instead of heat. This should be attributed to the supply of small sensible and abundant latent heat fluxes from the sea surface under the small air-sea temperature difference.

Structure of line-shaped convective systems obliquely training to the Baiu front observed around the Southwest Islands of Japan 査読有り

T. Shinoda, T. Amano, H. Uyeda, K. Tsuboki, H. Minda

J. Meteor. Soc. Japan 87 巻 ( 4 ) 頁： 739-745 2009年8月

担当区分：筆頭著者記述言語：英語掲載種別：研究論文（学術雑誌）

This study reveals a structure of line-shaped convective systems (LSCSs) observed around the Southwest Islands of Japan on June 10, 2006 using dual-Doppler analyses obtained from two X-band Doppler radars installed on Shimoji and Tarama Islands. Many LSCSs with lengths ranging from 20 km to 40 km form in a band-shaped precipitation system with a length exceeding 300 km along the Baiu front. The alignment directions of the Baiu front and the LSCSs are west-southwest to east-northeast and south-southwest to north-northeast, respectively. Thus, the alignment direction of the LSCSs is oblique to that of the Baiu front, and is parallel to the vertical wind shear vector between 0.5 km and 3 km in altitude.

These LSCSs consist of several precipitation cells. The precipitation cells generate only to the south of the southern edge of each LSCS, and move northward and decayed at the northern edge. The pre-existing cells in each LSCS hardly affect the successive generation of new cells. The generation area of precipitation cells coincides with low-level convergence along the Baiu front. The successive generation mechanism of new cells in the observed LSCSs and their structure shown in this study correspond to those in a humid environment, suggested in a previous numerical study.

*Characteristics of vertical circulation in the convective boundary layer over the Huaihe River Basin in China in the early summer of 2004 査読有り

Endo, S., T. Shinoda, H. Tanaka, T. Hiyama, K. Tsuboki, H. Uyeda, K. Nakamura

J. Appl. Meteor. Climatol. 47 巻頁： 2911-2928 2008年

Detailed structure of wind and moisture fields around the Baiu frontal zone over the East China Sea 査読有り

S. Maeda, K. Tsuboki, Q. Moteki, T. Shinoda, H. Minda, H. Uyeda

SOLA(Scientific Online Letters on the Atmosphere) 4 巻頁： 141-144 2008年

Surface flux and atmospheric boundary layers observations from the LAPS project over the middle of the Huaihe River basin in China 査読有り

Tanaka, H., T. Hiyama, K. Yamamoto, H. Fujinami, T. Shinoda, A. Higuchi, S. Endo, S. Ikeda, W. Li and K. Nakamura

Hydrol. Process. 21 巻頁： 1997-2008 2007年

Multiple Frontal Structures in the Baiu Frontal Zone Observed by Aircraft on 27 June 2004 査読有り

Moteki, Q., T. Shinoda, S. Shimizu, S. Maeda, H. Minda, K. Tsuboki, and H. Uyeda

SOLA(Scientific Online Letters on the Atmosphere) 2 巻頁： 132-135 2006年

Structure of moist layer and sources of water over the southern region far from the Meiyu/Baiu front 査読有り

Shinoda, T., H. Uyeda, and K. Yoshimura

J. Meteor. Soc. Japan 83 巻頁： 137-152 2005年

Structure and development of two merged rainbands observed over the East China Sea during X-BAIU-99 Part I: Meso-β-scale structure and development processes 査読有り

Moteki, Q., H. Uyeda, T. Maesaka, T. Shinoda, M. Yoshizaki, and T. Kato

J. Meteor. Soc. Japan 82 巻頁： 45-65 2004年

Structure and development of two merged rainbands observed over the East China Sea during X-BAIU-99 Part II: Meso-α-scale structure and build-up processes of convergence in the Baiu frontal region 査読有り

Moteki, Q., H. Uyeda, T. Maesaka, T. Shinoda, M. Yoshizaki, and T. Kato

J. Meteor. Soc. Japan 82 巻頁： 45-65 2004年

*Effective factors in the development of deep convective clouds over the wet region of eastern China during the summer monsoon season. 査読有り

Shinoda, T. and H. Uyeda

J.Mereor. Soc. Japan 80 巻頁： 1395-1414 2002年

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