日本地球惑星科学連合2021年大会

講演情報

[E] 口頭発表

セッション記号 M (領域外・複数領域) » M-GI 地球科学一般・情報地球科学

[M-GI29] Data assimilation: A fundamental approach in geosciences

2021年6月3日(木) 09:00 〜 10:30 Ch.09 (Zoom会場09)

コンビーナ:中野 慎也(情報・システム研究機構 統計数理研究所)、藤井 陽介(気象庁気象研究所)、三好 建正(理化学研究所)、宮崎 真一(京都大学理学研究科)、座長:中野 慎也(情報・システム研究機構 統計数理研究所)、宮崎 真一(京都大学理学研究科)

09:30 〜 09:45

[MGI29-03] Optimizing the localization scale for a convective-scale ensemble radar data assimilation system

★Invited Papers

*James David Taylor1、Takumi Honda1、Arata Amemiya1、Takemasa Miyoshi1 (1.RIKEN Research center for computational science)

キーワード:LETKF, localization, assimilation

For any ensemble-based data assimilation system sampling errors are introduced as a consequence of limited ensemble size, generating spurious backgound errors covariances and leading to erroneous adjustments to the analysis. As a way to reduce the impact of these systematic errors, as well as improve rank deficiency, covariance localization is applied, which artifically reduces the weighting of error covariances beyond a defined physical distance between the background and observations deemed to be false.

In this study we perform sensitivity tests to find the appropriate horizontal localization scale for the SCALE-LETKF, a numerical weather prediction model that combines the SCALE numerical model with the local ensemble transform Kalman filter. The system has been in development since 2013 to provide very high resolution modelling of convective weather systems and is unique in its ability to perform near real-time NWP operation at 500-m resolution refreshed every 30 seconds with observations from Phased Array Weather Radar (PAWR). Here, we perform sensitivity tests at 500-m resolution with 30-second update cycling of PAWR data for several testcases of heavy convective rainfall over Tokyo metropolitan area from August/September 2019. Test scores showed horizontal localization scale of 2-km generally provided optimal forecast skill for lead times up to 30 minutes, although there were variations on this dependent upon lead time and case study. We show that by reducing localization scale, systematic errors leading to over-intensification of convective activity in forecasts were reduced, resulting in improved consistency with observations. This was a conseqence of generating more convectively stable, less dynamically active environment with smaller localization scale.