日本地球惑星科学連合2023年大会

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[J] 口頭発表

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-CG47] 有人・無人航空機による気候・地球システム科学研究の推進

2023年5月26日(金) 09:00 〜 10:15 202 (幕張メッセ国際会議場)

コンビーナ:高橋 暢宏(名古屋大学 宇宙地球環境研究所)、小池 真(東京大学大学院 理学系研究科 地球惑星科学専攻)、町田 敏暢(国立環境研究所)、篠田 太郎(名古屋大学宇宙地球環境研究所)、座長:高橋 暢宏(名古屋大学 宇宙地球環境研究所)、小池 真(東京大学大学院 理学系研究科 地球惑星科学専攻)

09:45 〜 10:00

[ACG47-04] ACARS/AMDARを用いた台風構造解析

*伊藤 耕介1、山本 蓮1 (1.琉球大学)

キーワード:台風、航空機観測

Meteorological variables are often reported by commercial aircraft flying around tropical cyclones (TCs). They are archived in Aircraft Communications, Addressing, and Reporting System/Aircraft Meteorological Data Relay (ACARS/AMDAR). Therefore, they are potentially useful for constructing a composite mean structure of TCs based on in-situ measurements. The number of temperature and wind observations are 4.0 × 106 and 1.0 × 104 within the radius of 1,200 km and 100 km from the TC center during 2010–2020, respectively. The warm-core potential temperature anomaly with respect to the climatology is 6.4 K, 9.1 K, and 14.4 K maximized around 300 hPa for weak, moderate, and strong TCs, respectively. The composite of the potential temperature anomaly potentially extends more than 1,000 km from the TC center in the upper troposphere, cautioning the typical definition of the environment. The region of significant upper-level positive potential temperature anomalies extends broadly with increasing TC intensity. Moreover, large TCs tend to have a broad and deep upper-level warm core for a given intensity. In addition, we ensured that a single observation of potential temperature around 300 hPa could be used as a proxy for minimum sea level pressure. Low-level inflow and upper-level outflow were detected in the ACARS/
AMDAR data.