日本地球惑星科学連合2023年大会

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セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS09] 成層圏・対流圏過程とその気候への影響

2023年5月26日(金) 10:45 〜 12:00 201A (幕張メッセ国際会議場)

コンビーナ:田口 正和(愛知教育大学)、江口 菜穂(九州大学 応用力学研究所)、高麗 正史(東京大学大学院理学系研究科地球惑星科学専攻)、野口 峻佑(九州大学 理学研究院 地球惑星科学部門)、座長:高麗 正史(東京大学大学院理学系研究科地球惑星科学専攻)


11:00 〜 11:15

[AAS09-07] Sensitivity to the Initial Condition for the Prediction of Stratospheric Ozone in the Southern Hemisphere during Spring

*中村 東奈1,2廣岡 俊彦2秋吉 英治3 (1.富士通Japan株式会社、2.九州大学大学院理学研究院地球惑星科学部門、3.国立環境研究所)

キーワード:オゾン、予測可能性、データ同化

A reduction of the total ozone over the southern tip of South America lasting 3 weeks occurred in November 2009. In this event, the polar vortex was distorted to an elliptic shape due to enhanced planetary wave activity, bringing to migration of ozone depletion region associated with the Antarctic ozone hole towards the South American continent at the time of the vortex breakup. We attempt ensemble forecast experiments for the ozone reduction event, using the National Institute for Environmental Studies (NIES) chemical-climate model (NIES CCM) with 32 ensemble members whose initial data was produced by the ozone assimilated NIES CCM from the Modern-Era Retrospective analysis for Research and Applications, version 2 (MERRA-2) reanalysis data for the dynamical field, along with the Aura Ozone Monitoring Instrument (OMI) and Microwave Limb Sounder (MLS) data for the ozone field. The forecast experiments are performed from the various initial dates in October-November 2009.
To quantify the model performance, we investigate the predictability of the geopotential height and total ozone fields, on the basis of the pattern correlation coefficient (PCC) and Root Mean Square Error (RMSE) between their forecast and reanalysis values.
We investigate the predictability dependence on three kinds of assimilated initial data for the forecast experiments, i.e., (1) dynamical data, (2) dynamical and total ozone data, and (3) dynamical, total ozone, and vertical ozone profile data. Results of the forecast experiments suggest the importance of the vertical ozone profile at the initial state for accurate prediction of ozone field.