Japan Geoscience Union Meeting 2025

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-CG Complex & General

[A-CG36] Extratropical oceans and atmosphere

Mon. May 26, 2025 3:30 PM - 5:00 PM 101 (International Conference Hall, Makuhari Messe)

convener:Yuta Ando(Department of Earth and Planetary Sciences, Kyushu University), Tong Wang(Japan Agency for Marine-Earth Science and Technology), Kenta Tamura(National Research Institute for Earth Science and Disaster Resilience), Shota Katsura(Department of Geophysics, Graduate School of Science, Tohoku University), Chairperson:Kenta Tamura(National Research Institute for Earth Science and Disaster Resilience), Yuta Ando(Department of Earth and Planetary Sciences, Kyushu University)


4:30 PM - 4:45 PM

[ACG36-17] Future Changes in the Western Pacific Pattern Under Global Warming

*Shiozaki Masahiro1, Hiroki Tokinaga1, Masato Mori1 (1.Research Institute for applied mechanics, Kyushu university)

Keywords:Global warming, Teleconnection, Western Pacific (WP) pattern

Several previous studies have suggested that global warming may alter the location and intensity of atmospheric teleconnections. This study examines the effects of global warming on the Western Pacific (WP) pattern, utilizing past and future climate simulations from the Database for Policy Decision-Making for Future Climate Change (d4PDF) and the Coupled Model Intercomparison Project Phase 6 (CMIP6).

The WP pattern appears similar in both historical and future climate simulations. However, the future climate simulations are characterized by increased amplitudes of 500 hPa geopotential height (Z500) anomalies in the southern part of the WP pattern while decreased amplitudes in the northern part, indicating a northward shift of the WP pattern under global warming. Meanwhile, a comparison between CMIP6 and d4PDF shows a non-negligible difference in Z500 anomaly associated with the WP pattern. The increased amplitudes in the southern part of WP are much larger in CMIP6 than in d4PDF. This difference is likely due to changes in tropical forcing between CMIP6 and d4PDF.

In this talk, we will present a more detailed analysis of the factors contributing to future changes in the WP pattern.