Long-Term Wintertime SST Increase around Japan: Weakening of Atmospheric Cooling Associated with the Weakening of the Aleutian Low
编号:16 访问权限:仅限参会人 更新:2026-04-22 15:13:09 浏览:10次 张贴报告

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摘要
In the western North Pacific, a marked increase in wintertime sea surface temperature (SST) has been observed around the subarctic front (SAF), with warming rates reaching approximately +3 °C per century. Remarkable SST warming trends are also observed in the Japan Sea, with zonal band structure (Matsuura and Kida 2024). However, the physical processes responsible for this rapid SST increase over the mid-latitude North Pacific remain unclear.
To investigate the cause of this increase, we focused on the winter season (January-March). Vertical hydrographic sections conducted by the Japan Meteorological Agency along 165°E during 1997–2021 showed that the warming signal extends down to a depth of 300 dbar, leading to enhanced upper-ocean stratification. While a northward shift of the SAF could potentially affect the SST increase, satellite observations indicated that the frontal position has remained nearly stationary since 1982. Atmospheric reanalysis data indicated that the SST increase is primarily driven by changes in atmospheric forcing. In particular, a reduction in cold-air outbreaks originating from the Eurasian continent, associated with large-scale atmospheric circulation changes, plays a dominant role. Consistently, a mixed-layer heat budget analysis using ocean reanalysis data demonstrated that the observed SST increase is mainly attributed to weakened atmospheric cooling, rather than enhanced warm-water transport from the Kuroshio Extension (KE) to the south. We obtained Similar results for the Subpolar front region over the Japan Sea, but a more detailed analysis is needed regarding the influence of the Tsushima Warm Current.
The SST around the SAF strongly influences storm-track activity (Taguchi et al. 2012). Furthermore, the anomalous northward meandering of the KE since 2023 has recently altered the oceanic environment near the SAF (Sugimoto et al. 2025), potentially affecting oceanic advection and the frontal structure. Continuous monitoring will therefore be essential to assess how these recent changes interact with the ongoing multidecadal trend.
关键词
Cold-air,Aleutian Low,SST
报告人
Gaku Nishihira
Research Fellow Kyushu University

稿件作者
Gaku Nishihira Kyushu University
Shusaku Sugimoto Graduate School of Science, Tohoku University;Advanced Institute for Marine Ecosystem Change, Tohoku University
Bo Qiu University of Hawaii at Manoa
Niklas Schneider University of Hawaii at Manoa
Kelvin Richard University of Hawaii at Manoa
Shinichiro Kida Kyushu University
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重要日期
  • 会议日期

    06月16日

    2026

    06月18日

    2026

  • 04月03日 2026

    初稿截稿日期

主办单位
Hokkaido University
承办单位
Hokkaido University
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