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) 10:45 〜 12:15 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:村上 浩(宇宙航空研究開発機構地球観測研究センター)、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)

11:30 〜 11:45

[ACG41-16] Quantification of Constrained Scales in the Ocean with an Ensemble Analysis

*Kenneth Andrew Peterson1、Gregory C. Smith1、Kamel Chikhar2、Andrea Storto3 (1.RPN-EM, ECCC、2.MSC, ECCC、3.CNR)

キーワード:Ensemble Prediction, Constrained Scales , Data Assimilation, Altimeter Observations

Numerical models used in operational ocean prediction systems typically resolve finer scales than can be constrained through the assimilation of conventional satellite measurements. This results in unconstrained variability contributing to larger model error. An ensemble of ocean analyses, if correctly constructed, could provide a means to remove uncertainty associated with features having length scales that cannot be constrained by observations.

Here we use an eddy-permitting ocean prediction system to demonstrate that the ensemble mean can be used as a filter to remove unconstrained variability and reduce forecast error. It is demonstrated that the limits separating length scales of constrained and unconstrained variability can vary over the global domain, and that these separation scales are a product of the analysis system, not imposed by lengthscales associated with the ensemble perturbations. A further demonstration is made of how the removal of the unconstrained scales reduce errors in surface currents when compared to drifting buoys.

These findings support the use of ensembles as a means to account for errors due to unconstrained variability found in deterministic ocean predictions.