JpGU-AGU Joint Meeting 2017

Presentation information

[EE] Oral

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

[A-CG43] [EE] Air-sea interaction in the extratropics

Sat. May 20, 2017 1:45 PM - 3:15 PM 302 (International Conference Hall 3F)

convener:Kazuaki Nishii(Graduate School of Bioresources, Mie University), Yoshi N Sasaki(Hokkaido University), Shusaku Sugimoto(Graduate School of Science, Tohoku University), Shun Ohishi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Chairperson:Kazuaki Nishii(Graduate School of Bioresources, Mie University), Chairperson:Ryusuke Masunaga(Research Center for Advanced Science and Technology, The University of Tokyo)

2:15 PM - 2:30 PM

[ACG43-03] Interannual modulations of the influence of North Pacific oceanic fronts on the atmosphere
as revealed in the JRA-55 family

*Satroru Okajima1, Hisashi Nakamura1, Ryusuke Masunaga1, Hirotaka Kamahori2, Chiaki Kobayashi2 (1.Research Center for Advanced Science and Technology, 2.Meteorological Research Institute)

Keywords:Oceanic front, Air-Sea interaction, western North Pacific, Atmospheric Reanalysis

Influence of frontal SST anomalies associated with North Pacific subarctic frontal zone on the overlying atmosphere are investigated through comparison between two sub-products of a new Japanese reanalysis for the global atmosphere (JRA-55). In one sub-product, JRA-55C, all the observational data but satellite data are assimilated on horizontal resolution of ~60km with COBE SST data on 1-degree resolution prescribed over 55 years. The other sub-product, JRA-55CHS, is the same as JRA-55C, but with MGDSST data on a quarter-degree resolution only over 28 recent years.
Atmospheric response to SST anomaly associated with meridional displacement of oceanic frontal zone is investigated as an interannual modulations of the influence of North Pacific oceanic fronts. In JRA-55CHS, SST anomaly is much better collocated with anomalous heat/moisture release in October. Enhancement of convective precipitation over warm SST anomalies is larger and so is area-averaged precipitation anomaly in JRA-55CHS. Anomalous upward motion and convective heating are also enhanced over the warm SST anomaly, not only within the atmospheric boundary layer but also in free troposphere. These results suggest that assimilating high-resolution SST data has a certain impact for global atmospheric reanalysis.