Japan Geoscience Union Meeting 2023

Presentation information

[E] Online Poster

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

[A-CG30] Extratropical oceans and atmosphere

Mon. May 22, 2023 1:45 PM - 3:15 PM Online Poster Zoom Room (2) (Online Poster)

convener:Shion Sekizawa(Research Center for Advanced Science and Technology, University of Tokyo), Shota Katsura(Atmosphere and Ocean Research Institute, The University of Tokyo), Yuta Ando(Kyushu University), Shoichiro Kido(JAMSTEC Application Lab)


On-site poster schedule(2023/5/21 17:15-18:45)

1:45 PM - 3:15 PM

[ACG30-P19] Cyclonic and Anticyclonic Contributions to Air-Sea Interactions around Midlatitude Oceanic Frontal Zones

*Satoru Okajima1, Hisashi Nakamura1, Thomas Spengler2 (1.Research Center for Advanced Science and Technology, The University of Tokyo, 2.University of Bergen)

Keywords:Oceanic frontal zone, transient eddy, storm track, Air-sea interaction

The Kuroshio-Oyashio Extension and Gulf Stream frontal zones are crucially important for air-sea interactions that contribute to the formation of midlatitude storm-tracks and eddy-driven westerly jets. Recent studies indicate a critical role of synoptic-scale atmospheric disturbances for these air-sea interactions. However, specific roles of cyclonic and anticyclonic disturbances in the interactions have neither been quantified nor fully understood. In this study, we quantify cyclonic and anticyclonic contributions to climatological-mean transient eddy feedback forcing onto westerly jets, surface turbulent heat fluxes, and precipitation based on a methodology using local curvature of winds. Additionally, we evaluate the impact of the oceanic frontal zones on these contributions. The anticyclonic contribution plays an important role in shaping turbulent heat fluxes along oceanic fronts and transient eddy feedback forcing onto the upper-level westerly jets, while cyclonic vortices predominantly contribute to a precipitation response. The distinctive roles of cyclonic and anticyclonic contributions in the air-sea interactions around the oceanic frontal zones are instrumental in our deeper understanding of midlatitude air-sea interactions.