Japan Geoscience Union Meeting 2024

Presentation information

[E] Oral

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

[A-CG32] Extratropical oceans and atmosphere

Sun. May 26, 2024 1:45 PM - 3:15 PM 201B (International Conference Hall, Makuhari Messe)

convener:Shota Katsura(Department of Geophysics, Graduate School of Science, Tohoku University), Yuta Ando(Department of Earth and Planetary Sciences, Kyushu University), Tong Wang(Japan Agency for Marine-Earth Science and Technology), Kenta Tamura(Faculty of Environmental Earth Science Hokkaido University ), Chairperson:Shota Katsura(Atmosphere and Ocean Research Institute, The University of Tokyo), Tong Wang(Japan Agency for Marine-Earth Science and Technology)


2:00 PM - 2:15 PM

[ACG32-11] Oceanic Reemergence Memory Links Atlantic and Pacific Multidecadal Variability

★Invited Papers

*BAOLAN WU1, LISAN YU2, XIAOPEI LIN3, JIANPING GAN1, BO QIU4, LIXIAO XU3 (1.HKUST, 2.WHOI, 3.OUC, 4.U Hawaii)

Keywords:mode water, multidecadal variability, Pacific , Reemergence, Oceanic memory

Understanding how the ocean provides the memory needed for maintaining decadal to multidecadal variability is key to climate prediction. An important question is what process in the ocean could provide the observed significant time-lag between the Pacific Decadal Oscillation (PDO) and the Atlantic Multidecadal Oscillation (AMO). Here we show that the Pacific Ocean could store climate anomalies within the subtropical recirculation gyre for a decadal duration, providing a “seeding” link between the AMO and PDO. The AMO-induced multidecadal temperature anomalies in the Subtropical Northwestern Pacific Ocean are subducted into the thermocline and sequestered in the North Pacific subtropical mode water. These temperature anomalies carried by the mode water would propagate southwestward along the recirculation gyre pathway to eventually re-join the Kuroshio one decade later. Once reemerged in the isopycnal outcropping area of the Kuroshio-Oyashio Extension region, the anomalies that carry the memory of the previous decade may engage with local air-sea feedback to trigger the PDO. Thus, the AMO provides important memory for prediction of decadal climate and ecosystem variability in the Pacific Ocean.