日本地球惑星科学連合2024年大会

講演情報

[E] ポスター発表

セッション記号 A (大気水圏科学) » A-TT 計測技術・研究手法

[A-TT30] Machine Learning Techniques in Weather, Climate, Ocean, Hydrology and Disease Predictions

2024年5月29日(水) 17:15 〜 18:45 ポスター会場 (幕張メッセ国際展示場 6ホール)

コンビーナ:Jayanthi Venkata Ratnam(Application Laboratory, JAMSTEC)、Martineau Patrick(Japan Agency for Marine-Earth Science and Technology)、土井 威志(JAMSTEC)、Behera Swadhin(Climate Variation Predictability and Applicability Research Group, Application Laboratory, JAMSTEC, 3173-25 Showa-machi, Yokohama 236-0001)

17:15 〜 18:45

[ATT30-P01] 変分オートエンコーダによる急潮の分類

*青木 邦弘1中野 英之1広瀬 成章1坂本 圭1碓氷 典久1豊田 隆寛1浦川 昇吾1川上 雄真1 (1.気象庁 気象研究所)

キーワード:クラスタリング、深層生成モデル、急潮、黒潮

Kyucho is well known as a coastal oceanic abrupt event causing a strong surface current that often destroys fishing set-nets. The prediction of Kyucho requires specifying its precursor, but, in the case where Kyucho has multiple flow patterns, their triggers can be different from each other, and, this applies to Muroto, a southern coastal area of Shikoku, Japan. However, since the flow patterns of Muroto-Kyucho have been classified by "human eyes" from limited oceanic data, the whole picture of the rigorous flow patterns has still been unclear. In this study, we identify the flow patterns accompanied by Muroto-Kyucho in a statistical manner, leveraging the variational autoencoder, a deep generative model. The method can reconstruct the spatial structure of the oceanic flow from the so-called latent space which stores compressed information of the high dimensional oceanic flow data. We apply the method to the surface current data in 1960-2007 of FORA-60JPN, a reanalysis dataset supplied by Meteorological Research Institute, Japan Meteorological Agency. The latent space shows at least three modes, whose corresponding reconstructions indicate the different flow patterns that include the strong coastal current expressing Muroto-Kyucho: 1) Coastal jet like structure successive from Kii peninsula to Muroto, 2) Cyclonic eddy-like structure just southeast of Muroto, 3) Intrusion of Kuroshio current from southwest of Muroto. Pattern-1 is consistent with the typical structure in the coastal surface density flow or coastal trapped waves, but Pattern-2 and 3 suggest a presence of different dynamics. We will discuss potential precursors of each classified Muroto-Kyucho at the meeting.