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Online ISSN : 1349-6476
ISSN-L : 1349-6476

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Preliminary diagnosis of primary factors for an unprecedented heatwave over Japan in 2023 summer
Kazuto TakemuraHirotaka SatoAkira ItoTakafumi UmedaShuhei MaedaMasayuki HiraiYuko TamakiHirokazu MuraiHiroshi NakamigawaYukari N. TakayabuHiroaki UedaRyuichi KawamuraYouichi TanimotoHiroaki NaoeMasami NonakaToshihiko HirookaHitoshi MukougawaMasahiro WatanabeHisashi Nakamura
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ジャーナル オープンアクセス 早期公開

論文ID: 2024-010

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In summer 2023, record-high temperatures were observed in many parts of the Northern Hemisphere, including Japan, where summer-mean temperature was the highest over the last 126 years. Under an unprecedented heatwave in late July through September, record-high temperatures were successively observed particularly over northern and eastern Japan. The late-July heatwave is attributable primarily to the markedly-intensified North Pacific Subtropical High over Japan, accompanied by the poleward-deflected subtropical jet (STJ). This situation occurred under the influence of the Pacific–Japan pattern driven by northwestward-moving enhanced tropical convection over the western North Pacific and the Silk-Road pattern. The enhanced convection was influenced by upper-level cyclonic vortices detached from the intensified mid-Pacific trough. Seemingly, it was also under the remote influence from positive sea-surface temperature (SST) anomalies in the western equatorial Pacific as well as negative ones in the central–eastern equatorial Indian Ocean, considered as remnant and delayed impacts of long-lasted La Niña until the preceding winter. The August heatwave occurred under the persistent poleward-shift of STJ as well as warm, moist low-level southerlies and their downslope-wind effects. Both extremely high SST around northern Japan and a long-term warming trend in air temperature could also contribute to the record-setting air temperature.

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© The Author(s) 2024. 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.
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