JpGU-AGU Joint Meeting 2020

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-OS Ocean Sciences & Ocean Environment

[A-OS21] Dynamics of oceanic and atmospheric waves, vortices, and circulations

convener:Yuki Tanaka(Fukui Prefectural University), Ryo Furue(APL/JAMSTEC), Yukiharu Hisaki(University of the Ryukyus), Norihiko Sugimoto(Keio University, Department of Physics)

[AOS21-03] Toward practical use of EFSO for weekly weather forecasts: Dynamics of propagation of observation impacts

*Akira Yamazaki1, Takemasa Miyoshi2,1, Takeshi Enomoto3,1, Nobumasa Komori1, Jun Inoue4,1 (1.Application Laboratory, Japan Agency for Marine-Earth Science and Technology, 2.RIKEN Center for Computational Science, 3.Disaster Prevention Research Institute, Kyoto University, 4.National Institute of Polar Research)

An ensemble-based forecast sensitivity to observations (EFSO) diagnosis has implemented in an Atmospheric GCM–Ensemble Kalman Filter data assimilation system to estimate the impacts of specific observations in the quasi-operational global observing system on weekly short- and medium-range forecasts. EFSO can quantify how much each observation has improved or degraded the forecast without observing-system (another data assimilation) experiments, that is, an offline diagnosis. In order to examine whether EFSO values correctly quantify the impacts of a subset of observations performed in a specific geographical spot in 6-hour to 7-day forecasts, EFSO values were compared with actual observation impacts obtained from multiple data denial experiments in each of which a subset of three radiosonde observations launched from a geographical spot was excluded. The spots were selected from three latitudinal bands comprising (1) Arctic regions, (2) midlatitude regions in the Northern Hemisphere, and (3) tropical regions during the winter of 2015/16. The results showed that all EFSO values reasonably estimated the observation impacts on short-range (6-hour to 2-day) forecasts. Furthermore, it was found that the initial Arctic observation impacts, which could be estimated by EFSO, remained in medium-range (7-day) forecasts because the Arctic is located at the upstream of dynamical propagation toward the midlatitudes where small perturbations rapidly and spontaneously grow. Therefore, EFSO can be useful for weekly forecasts for anticipating impacts of specific observations by considering dynamical propagation.