SOLA
Online ISSN : 1349-6476
ISSN-L : 1349-6476
Article
The Importance of Dynamical Downscaling for Explanations of High Temperature Rises in Winter
Hidetaka Sasaki, Noriko N. Ishizaki, Akihiko Murata, Hiroaki Kawase, Masaya Nosaka
著者情報
  • Hidetaka Sasaki

    National Institute for Environmental Studies

  • Noriko N. Ishizaki

    National Institute for Environmental Studies

  • Akihiko Murata

    Meteorological Research Institute

  • Hiroaki Kawase

    Meteorological Research Institute

  • Masaya Nosaka

    Meteorological Research Institute

責任著者(Corresponding author)

ORCID
ジャーナル オープンアクセス
電子付録

2023 年 19 巻 p. 9-15

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詳細
  • Published: 2023 Received: 2022年11月02日 Released on J-STAGE: 2023年01月12日 Accepted: 2022年12月04日 Advance online publication: 2022年12月16日 Revised: -
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The surface temperature was projected to increase from 4 to 5°C in most regions around Japan in winter at the end of the 21st century, according to the Non-Hydrostatic Regional Climate Model (NHRCM) under the Representative Concentration Pathway 8.5 scenario. The melting of sea ice in the Sea of Okhotsk significantly affected the temperature around Hokkaido Prefecture, raising it by more than 8°C in some places. The temperature also rose by more than 8°C in some areas in Honshu where the atmosphere was not susceptible to sea ice. The reduction in snow-covered areas due to global warming raised the temperature further and induced changes in local wind, such as airflows over mountains and wind blowing from the sea. These changes raised the seasonal average temperature and caused the temperature to rise by over 8°C. The dynamical downscaling method played a significant role in projecting such small-scale features in the future climate.

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© The Author(s) 2023. This is an open access article published by the Meteorological Society of Japan under a Creative Commons Attribution 4.0 International (CC BY 4.0) license.

This article is licensed under a Creative Commons [Attribution 4.0 International] license.
https://creativecommons.org/licenses/by/4.0/
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