日本地球惑星科学連合2022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-CG 大気海洋・環境科学複合領域・一般

[A-CG33] 中緯度大気海洋相互作用

2022年6月3日(金) 11:00 〜 13:00 オンラインポスターZoom会場 (10) (Ch.10)

コンビーナ:木戸 晶一郎(海洋開発研究機構 付加価値創生部門 アプリケーションラボ)、コンビーナ:関澤 偲温(東京大学先端科学技術研究センター)、桂 将太(カリフォルニア大学サンディエゴ校スクリプス海洋研究所)、コンビーナ:安藤 雄太(新潟大学理学部)、座長:木戸 晶一郎(海洋開発研究機構 付加価値創生部門 アプリケーションラボ)、関澤 偲温(東京大学先端科学技術研究センター)、桂 将太(カリフォルニア大学サンディエゴ校スクリプス海洋研究所)、安藤 雄太(新潟大学理学部)

11:00 〜 13:00

[ACG33-P02] 豪雪地帯と非豪雪地帯における降雪量の風向依存性の違い

*山本 諒1立花 義裕1安藤 雄太2 (1.三重大学、2.新潟大学)


キーワード:風向、マッピング、降雪

In this study, we compared the climatological wind direction, the most frequent wind direction on snowfall days, and the most likely wind direction for snowfall in heavy snowfall areas and non-heavy snowfall areas. The data used in this study are daily snowfall data from 99 meteorological stations in Japan. The analysis period is from December to March of the following year, 1961/62 to 2020/21. The wind direction data were obtained from the daily wind speed data on the 925-hPa surface of the JRA-55 long-term reanalysis data of the Japan Meteorological Agency (JMA), and the data of the grid points at the shortest distances in the second quadrant were used as the wind over that point.
In this study, the top five points (Iwamizawa, Kutchan, Aomori, Shinjo, and Takada) in terms of average daily snowfall are defined as heavy snowfall areas. The results showed that the climatological wind direction, the most frequent wind direction on snowfall days, and the most likely wind direction for snowfall matched the climatological wind direction in heavy snowfall areas except for a few points. On the other hand, in non-snowfall areas, the climatological wind direction and the most likely wind direction for snowfall matched in few points. These results suggest the difference on the amount of snowfall of wind direction in heavy snowfall areas and non-heavy snowfall areas.