日本地球惑星科学連合2025年大会

講演情報

[E] 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-CG41] 衛星による地球環境観測

2025年5月29日(木) 15:30 〜 17:00 展示場特設会場 (5) (幕張メッセ国際展示場 7・8ホール)

コンビーナ:沖 理子(宇宙航空研究開発機構)、本多 嘉明(千葉大学環境リモートセンシング研究センター)、松永 恒雄(国立環境研究所地球環境研究センター/衛星観測センター)、高橋 暢宏(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)、沖 理子(宇宙航空研究開発機構)

16:15 〜 16:30

[ACG41-28] Development of GSMaP precipitation estimation algorithm considering regional characteristics

*山本 宗尚1久保田 拓志1 (1.国立研究開発法人宇宙航空研究開発機構地球観測研究センター)

キーワード:降水、マイクロ波放射計、赤外放射計

The Global Satellite Mapping of Precipitation (GSMaP) is one of the global distributions of precipitation products using multiple microwave radiometers (PMWs) on board low Earth orbit and infrared (IR) imagers from geostationary meteorological satellites with 1-hour and 0.1 degrees resolution. Since PMWs observation cannot be observed globally for less than 3 hours, precipitation estimates from IR observations fill the gaps using the relationship between PMWs estimated rain rate and IR brightness temperature, called the PMW-IR combined algorithm.
Completed the 25-year record of previous data for the latest version, evaluation studies are conducted such as the differences between PMWs only and PMW-IR, comparing other satellite precipitation products, and so on. Their results showed that PMW-IR estimates are relatively degraded, for example, severe underestimation in the western coast of the Indian subcontinent and overestimation in the southern Thailand. This study reports on possible improvement methods that are currently being implemented in preparation for the next major algorithm upgrade scheduled for April 2026.
The PMW-IR combined algorithm is implemented using the Kalman filter approach and noise tables are generated for each 10 degrees of latitude over land and ocean. This band is common to Africa, Asia, and the Amazon region, where the different precipitation types of precipitation dominate. Therefore, we reconsidered the noise tables to precipitation regimes which is an a priori classification from 3-dimensional rainfall precipitation profiles and reanalysis data. In this presentation, we will show the relationship between precipitation and infrared brightness temperatures and the differences in precipitation distributions.