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-P14] Large-scale atmospheric response to warm SST anomalies in the North Pacific in the 2021-22 winter

*Kazuaki Nishii1, Bunmei Taguchi2, Hisashi Nakamura3 (1.Graduate School of Bioresources, Mie University, 2.Faculty of Sustainable Design, Toyama University, 3.Research Center for Advanced Science and Technology, The University of Tokyo)

Keywords:AGCM resolution, PDO, blocking, stratospheric vortex

Sea surface temperatures (SST) in the North Pacific were extremely warm in the 2021-22 winter associated with the negative phase of the Pacific Decadal Oscillation (PDO). We investigate the large-scale atmospheric responses to the warm SST anomalies through ensemble time-slice experiments of an atmospheric general circulation model (AGCM) with two different horizontal resolution settings: 100 km and 50 km. In both the 100-km and 50-km experiments, anticyclonic responses in the winter-mean 500-hPa geopotential height fields are found over the North Pacific. The anticyclonic response is stronger in the 50-km AGCM, and its center is located slightly to the west of that obtained in the 100-km AGCM. Blocking frequency over the North Pacific in the 50-km AGCM is significantly increased under the influence of the warm SST anomalies, which may cool the lower stratosphere in the Arctic through suppressing upward planetary-wave propagation from the troposphere. Such increased blocking and cooling in the polar stratosphere are not observed in the response in the 100-km AGCM, suggesting the need for a high-resolution model to obtain a realistic blocking response to midlatitude SST anomalies.