Japan Geoscience Union Meeting 2015

Presentation information

Oral

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

[A-CG32] Multi-scale ocean-atmosphere interaction in the tropics

Wed. May 27, 2015 9:00 AM - 10:45 AM 202 (2F)

Convener:*Hiroki Tokinaga(Disaster Prevention Research Institute/Hakubi Center, Kyoto Univesity), Takuya Hasegawa(Japan Agency for Marine-Earth Science and Technology), Ayako Seiki(Japan Agency for Marine-Earth Science and Technology), Tomoki Tozuka(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Motoki Nagura(Japan Agency for Marine-Earth Science and Technology), Masamichi Ohba(Central Research Institute of Electric Power Industry (CRIEPI), Environmental Science Research Laboratory), Yukiko Imada(Atmosphere and Ocean Research Institute, the University of Tokyo), Chair:Tomoki Tozuka(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Ayako Seiki(Japan Agency for Marine-Earth Science and Technology), Takuya Hasegawa(Japan Agency for Marine-Earth Science and Technology)

10:00 AM - 10:15 AM

[ACG32-17] 1920s tropical Pacific climate shift revisited

*Hiroki TOKINAGA1 (1.DPRI, Kyoto University)

This study revisits the mid-1920s Pacific climate shift using a wide variety of historical climate data sets including sea surface temperature (SST), nighttime marine air temperature, sea level pressure, and cloudiness. Overall the 1920s Pacific climate shift is similar to the 1976/77 Pacific Decadal Oscillation shift from cold-to-warm phase, characterized by SST cooling over the North Pacific and deepening of the Aleutian Low. On the other hand, patterns of the tropical Pacific SST change during the 1920s largely depend on SST data sets. HadISST1 shows no significant SST change in the equatorial Pacific. In contrast, COBE-SST2 exhibits a local maximum of SST warming in the central-to-eastern equatorial Pacific, resulting in a weakening of zonal SST gradient. The latter pattern of SST change is more consistent with an observed weakening of the Walker circulation obtained from SLP observations. This result suggests that the 1920s climate shift actually happened not only over the North Pacific but also over the tropical Pacific, a feature not captured by conventional SST data sets. Simulated patterns of surface air temperature and SLP changes from AGCM experiments forced with COBE-SST2 and HadISST1 will also be discussed.