日本地球惑星科学連合2021年大会

講演情報

[E] ポスター発表

セッション記号 A (大気水圏科学) » A-OS 海洋科学・海洋環境

[A-OS11] Ocean Mixing Frontiers

2021年6月5日(土) 17:15 〜 18:30 Ch.05

コンビーナ:日比谷 紀之(東京大学大学院理学系研究科地球惑星科学専攻)

17:15 〜 18:30

[AOS11-P01] Sensitivity of the ocean state estimation to the vertical distribution of tidally induced far-field mixing

*長船 哲史1、纐纈 慎也1、土居 知将1、杉浦 望実1、増田 周平1 (1.国立研究開発法人 海洋研究開発機構)

キーワード:潮汐、鉛直混合、熱塩循環

Vertical mixing plays an important role in determining the large-scale ocean circulation including the meridional overturning and the distribution of water properties. The breaking of internal tide is a major source of interior vertical mixing below the surface mixed layer. Recent numerical studies have shown the importance of incorporating tidally induced far-field mixing in addition to the near-field mixing. In our previous study under the OMIX project, we conducted a linear optimization experiment to reproduce the climatological distribution of water properties with an ocean general circulation model using tidally induced near- and far-field mixing schemes with an assumption that diffusivity is vertically constant for far-field mixing. The optimized model performed reasonably well in reproducing the deep-water properties of the Pacific Ocean. However, the reproducibility of water mass distribution is degraded in some places, especially in the sub-surface-intermediate layers, when compared with the optimized state in the earlier version of our model using semi-empirical interior mixing schemes. This shortcoming may be overcome by improving model interior mixing. Our new model uses the far-field mixing scheme only related to the wave-wave interactions, but the far-field mixing is caused through various mechanisms, on which the vertical structure of diffusivity depends. In this study, we conducted numerical experiments using our new model but with different vertical distribution function for the far-field mixing on the basis of a previous semi-empirical scheme. We show the incorporation of a vertical structure into the far-field mixing representation can possibly resolve the upper layer issues in our state estimation. It can be a clue to uncover nature of vertical mixing in the real ocean. We will discuss the effectiveness of the proposed implementation in our experiments, referring the recent vertical mixing schemes suggested in the theoretical studies.