TY - JOUR
T1 - Preliminary Diagnosis of Primary Factors for an Unprecedented Heatwave over Japan in 2023 Summer
AU - Takemura, Kazuto
AU - Sato, Hirotaka
AU - Ito, Akira
AU - Umeda, Takafumi
AU - Maeda, Shuhei
AU - Hirai, Masayuki
AU - Tamaki, Yuko
AU - Murai, Hirokazu
AU - Nakamigawa, Hiroshi
AU - Takayabu, Yukari N.
AU - Ueda, Hiroaki
AU - Kawamura, Ryuichi
AU - Tanimoto, Youichi
AU - Naoe, Hiroaki
AU - Nonaka, Masami
AU - Hirooka, Toshihiko
AU - Mukougawa, Hitoshi
AU - Watanabe, Masahiro
AU - Nakamura, Hisashi
N1 - Publisher Copyright:
© 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 (http://creativecommons.org/license/by/4.0).
PY - 2024
Y1 - 2024
N2 - 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.
AB - 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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U2 - 10.2151/SOLA.2024-010
DO - 10.2151/SOLA.2024-010
M3 - Article
AN - SCOPUS:85192242295
SN - 1349-6476
VL - 20
SP - 69
EP - 78
JO - Scientific Online Letters on the Atmosphere
JF - Scientific Online Letters on the Atmosphere
ER -