日本地球惑星科学連合2025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-AS 大気科学・気象学・大気環境

[A-AS09] 応用気象学

2025年5月27日(火) 10:45 〜 12:15 展示場特設会場 (4) (幕張メッセ国際展示場 7・8ホール)

コンビーナ:稲津 將(北海道大学大学院理学研究院)、竹見 哲也(京都大学防災研究所)、日下 博幸(筑波大学)、座長:丹治 星河(京都大学)

11:45 〜 12:00

[AAS09-05] Spatial interpolation method for estimation of charge distribution in thunderstorm

*山下 由美子1、長尾 篤1、池田 高志1、佐藤 陽祐2、佐藤 光輝2稲津 將2 (1.日本電信電話株式会社宇宙環境エネルギー研究所、2.北海道大学大学院理学研究院)

キーワード:地球統計学、クリギング、電荷分布推定、雷雲

Accurate interpolation is essential for improving estimation of charge distribution in a thunderstorm[Mansell et al., 2005]. Ordinary Kriging[Cressie, 1988] is widely used due to its ability to incorporate spatial correlations, result in high-accuracy interpolations when observation data are dense and well-distributed.
However, its performance heavily depends on the density of the observed data, leading to significant error when data points are sparse. To address this issue, we propose a novel interpolation method based on Ordinary Kriging. Our approach is to see the observed variable as the sum of two random variables: a physical model term and an observation error term. By assuming their probability distribution, we can analytically derive the error variance function to minimize and determine optimal interpolation weights.
To evaluate the effectiveness, we calculated the performance of proposed method to apply interpolation of electric field on one-dimensional space whose observation data was given by simulation by two ways, confirming the superiority of the proposed method when data points are sparse:(1) Comparison of root mean square error between Ordinary Kriging and the proposed method and (2) Estimation of charge distribution in a given domain using observed and interpolated electric field data to quantify the resolution improvement.
Finally, we applied the proposed method to actual observed electric field data and estimate charge distribution in a real thunderstorm. The results demonstrated that our approach enables higher resolution for estimation, even when observation point are limited to only six with in an approximately 10 square kilometers area. The proposed method shows significant advantages in cases with limited observation data, where Ordinary Kriging struggles due to high dependency on variogram fitting.