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_29AM1] Satellite Earth Environment Observation

2014年4月29日(火) 09:00 〜 10:45 315 (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:高薮 縁(東京大学 大気海洋研究所)

09:45 〜 10:00

[ACG06-10] 降水科学における全球降水観測計画(GPM)への期待

*高薮 縁1沖 理子2井口 俊夫3青梨 和正4可知 美佐子2久保田 拓志2濱田 篤1高橋 暢宏3中村 建治5 (1.東京大学大気海洋研究所、2.宇宙航空研究開発機構、3.独立行政法人 情報通信研究機構、4.気象庁気象研究所、5.獨協大学)

キーワード:全球降雨観測計画, 二周波降雨レーダー, 降水科学, 熱帯降雨観測計画, 降雨特性, コンステレーション

Three dimensional precipitation data observed with Ku (13.8GHz) band Precipitation Radar (PR) on board the Tropical Rainfall Measurement Mission (TRMM) satellite have enabled us to discover various precipitation characteristics over the tropics and subtropics between 36N and 36S. Precipitation system regimes are estimated with precipitation characteristics. The multiple instrument observations of TRMM have also made us quantify the discrepancies between TRMM Microwave Imager (TMI) vs. PR estimated rainfall, and provided us with opportunities to investigate various approaches to improve the rainfall retrieval algorithms. With the launch of the GPM/DPR, scheduled in February 2014, dual band measurements from space with Ku (13.6GHz) and Ka (35.5GHz) band frequencies will be started. Increasing information of the drop size distributions with DPR should improve the accuracy of precipitation profile structures, which are essential to study precipitation characteristics. GPM/DPR will provide excellent cross calibrations for constellation microwave observations to construct better mapping of precipitation from 65N to 65S, which covers 91% of the earth surface. Weak rainfall measurements will enable us better energy budget calculations after all, as well as more precise examinations of rainfall system lifecycles. We can also expect reexamination and further improvements of TRMM PR rainfall products by comparing Ku-band retrievals with DPR retrievals. Three dimensional satellite measurement of precipitation at mid-to-high latitudes is a completely new scientific experiment. Since the precipitation systems there are very different from those in the tropics and subtropics, we can certainly expect further scientific discoveries to improve our knowledge of precipitation characteristics with thorough observations from the satellite. Using this outcomes, we also expect to provide useful knowledge to improve the numerical models for weather predictions and climate projections.