日本地球惑星科学連合2014年大会

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インターナショナルセッション(口頭発表)

セッション記号 A (大気海洋・環境科学) » A-CG 大気海洋・環境科学複合領域・一般

[A-CG06_29PM2] Satellite Earth Environment Observation

2014年4月29日(火) 16:15 〜 18:00 315 (3F)

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)、奈佐原 顕郎(筑波大学生命環境系)、中島 孝(東海大学情報デザイン工学部情報システム学科)、沖 大幹(東京大学生産技術研究所)、横田 達也(国立環境研究所 地球環境研究センター)、高薮 縁(東京大学大気海洋研究所)、村上 浩(宇宙航空研究開発機構地球観測研究センター)、岡本 創(九州大学 応用力学研究所)、座長:村上 浩(宇宙航空研究開発機構地球観測研究センター)、奈佐原 顕郎(筑波大学生命環境系)

16:15 〜 16:30

[ACG06-28] Synergistic use of the geostationary and the polar orbit satellites for surveying the cloud evolution process: plan

*中島 孝1永尾 隆1Letu Husi1 (1.東海大学)

キーワード:雲物理, 衛星観測, 大気放射

The use of spaceborne radar and imager aboard the CloudSat, Aqua, EarthCARE, GCOM-C1, and the 3rd generation geostationary satellites for investigating cloud evolution process, is suggested. These satellites have been in orbit or will be launched in the middle of 2010-era and contribute for observing aerosols, clouds on the earth system. Since aerosols and clouds exert an important influence on the planet’s water and energy balances, more understanding of their lifecycle is required. Optical thickness and particle size of clouds are primal information for estimating the cloud evolution process. These parameters are retrieved from multi-spectral imageries obtained from space-borne satellite sensors. Recently, active sensors, such as the CloudSat cloud profiling radar (CPR) and the CALIPSO Lidar present a new epoch of aerosol and cloud observation with the purpose of revealing transition of particles, from cloud condensation nuclei to rain droplets via cloud and drizzle particles. They observe vertical cross section of the cloud system along the satellite footprint. As follow on the CloudSat / CALIPSO, the EarthCARE that has both active and passive sensors is planed by JAXA, NICT, and ESA collaboration. Doppler capability of the EarthCARE CPR will reveals vertical motion of cloud particles. Moreover, the 3rd generation geostationary weather satellite will appear in 2015 and observe aerosol and cloud system in every 10 or 2.5 minutes. Therefore, it is expected that the combined use of polar orbital passive/active sensors and geostationary satellites reveal details of cloud evolution process, statistically and dynamically. In this presentation, we introduce recent progresses of aerosol and cloud observations from satellites, showing the multi-sensor views of cloud growth process obtained from an active radar (CPR) and a passive imager (MODIS).