Japan Geoscience Union Meeting 2022

Presentation information

[J] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS10] Stratosphere-troposphere Processes And their Role in Climate

Thu. May 26, 2022 1:45 PM - 3:15 PM 106 (International Conference Hall, Makuhari Messe)

convener:Masashi Kohma(Department of Earth and Planet Science, Graduate School of Science, The University of Tokyo), convener:Masakazu Taguchi(Aichi University of Education), Takenari Kinoshita(Japan Agency for Marine-Earth Science and Technology), convener:Nawo Eguchi(Kyushu University), Chairperson:Nawo Eguchi(Kyushu University), Masashi Kohma(Department of Earth and Planet Science, Graduate School of Science, The University of Tokyo)

2:30 PM - 2:45 PM

[AAS10-04] Application of Deep Learning to Estimate Atmospheric Gravity Wave Parameters in Reanalysis Data Sets

★Invited Papers

Daisuke Matsuoka1, *Shingo Watanabe1, Kaoru Sato2, Sho Kawazoe3, Wei Yu4, Steve Easterbrook4 (1.Japan Agency for Marine-Earth Science and Technology, 2.Department of Earth and Planetary Science, The University of Tokyo, 3.Department of Earth and Planetary Sciences, Hokkaido University, 4.Department of Computer Science, University of Toronto)

Keywords:Deep learning, Gravity waves, Reanalysis dataset

Gravity waves play an essential role in driving and maintaining the global circulation. In order to understand their contribution in the atmosphere, it is important to reproduce their distribution accurately. In this paper, we propose a deep learning method for estimating the momentum flux of gravity waves, and validate its performance at 100 hPa using low-resolution zonal wind, meridional wind, air temperature, and specific humidity (300, 700, and 850 hPa) data over the Hokkaido region. For this purpose, a deep convolutional neural network was trained on 29 years of reanalysis data sets (JRA-55 and DSJRA-55), and final 5 years of data were reserved for evaluation. The results show that the fine momentum flux distribution of gravity waves can be estimated with reasonable computational cost. In particular, the median root mean square error (RMSE) of the maximum momentum flux and the characteristic zonal wavenumber were 0.06-0.13 mPa and 1.0×10-5, respectively, during the winter season when gravity waves are stronger.