Preliminary Diagnosis of Primary Factors for an Unprecedented Heatwave over Japan in 2023 Summer-Reference-Cited by-同舟云学术

Preliminary Diagnosis of Primary Factors for an Unprecedented Heatwave over Japan in 2023 Summer

Published:2024 Issue:0 Volume:20 Page:69-78
ISSN:1349-6476
Container-title:SOLA
language:en
Short-container-title:SOLA

Author:

Takemura Kazuto¹²,Sato Hirotaka¹²,Ito Akira¹,Umeda Takafumi¹,Maeda Shuhei¹²,Hirai Masayuki¹,Tamaki Yuko¹,Murai Hirokazu¹,Nakamigawa Hiroshi¹,Takayabu Yukari N.³,Ueda Hiroaki⁴,Kawamura Ryuichi⁵,Tanimoto Youichi⁶,Naoe Hiroaki²,Nonaka Masami⁷,Hirooka Toshihiko⁵,Mukougawa Hitoshi⁸,Watanabe Masahiro³,Nakamura Hisashi⁹

Affiliation:

1. Japan Meteorological Agency

2. Meteorological Research Institute, Japan Meteorological Agency

3. Atmosphere and Ocean Research Institute, University of Tokyo

4. Faculty of Life and Environmental Sciences, University of Tsukuba

5. Department of Earth and Planetary Sciences, Kyushu University

6. Faculty of Environmental Earth Science, Hokkaido University

7. Application Laboratory, Japan Agency for Marine-Earth Science and Technology

8. Graduate School of Science, Kyoto University

9. Research Center for Advanced Science and Technology, University of Tokyo

Publisher

Meteorological Society of Japan

Link

https://www.jstage.jst.go.jp/article/sola/20/0/20_2024-010/_pdf

Reference33 articles.

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2. Enomoto, T., 2004: Interannual variability of the Bonin high associated with the propagation of Rossby waves along the Asian jet. J. Meteor. Soc. Japan, 82, 1019-1034.

3. Enomoto, T., B. J. Hoskins, and Y. Matsuda, 2003: The formation mechanism of the Bonin high in August. Quart. J. Roy. Meteor. Soc., 129, 157-178.

4. Fire and Disaster Management Agency of Japan, 2023: A report on emergency transport due to heat stroke (Available online at: https://www.fdma.go.jp/disaster/heatstroke/post3.html, accessed 28 September 2023, in Japanese).

5. Hamaguchi, Y., and Y. N. Takayabu, 2021: An initiation process of tropical depression–type disturbances under the influence of upper-level troughs. J. Atmos. Sci., 78, 4001-4019.

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