JpGU-AGU Joint Meeting 2020

講演情報

[E] 口頭発表

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-OS24] Exploring new frontiers of oceanic mixing research in the next decade

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)、安田 一郎(東京大学大気海洋研究所)、Lakshmi Kantha(Aerospace Engineering Sciences, University of Colorado, Boulder, Colorado, USA)

[AOS24-03] CTD・グライダ・フロート等に取り付けた高速水温計を用いた効率的自動微細構造観測手法の開発

*安田 一郎1李 根淙1長澤 真樹1ザイ ソウ1佐々木 雄亮1柳本 大吾1藤尾 伸三1田中 衛1後藤 恭敬2中野 俊也2笹野 大輔2田中 雄大4纐纈 慎也3 (1.東京大学大気海洋研究所、2.気象庁、3.海洋研究開発機構、4.水産研究教育機構東北区水産研究所)

キーワード:乱流、観測

A new efficient microstructure measurement with fast-response thermistors attached to CTD, underwater glider and deep float has been elaborated. The CTD-attached thermistor measurements were confirmed to be valid in the weak turbulent energy dissipation down to 10-11W/kg by comparing with the one by free-fall instrument with the best accuracy, and revealed cross-Pacific top-bottom turbulence distribution. Vertical distribution of turbulent energy dissipationis found to be proportional withlocal squared buoyancy frequency N2(representing density vertical gradient) and local internal tide energy generation and dissipation, indicating that energy dissipation of tide-induced turbulence occurs in the main thermocline. Thermistor measurements attached to gliders and deep floats were also confirmed to be useful to measure weak turbulence area as in the deep water as well as the water where double-diffusive convections work. These contribute to revising models of tide-induced three-dimensional distribution used in ocean/climate models, which will contribute to reproducing ocean meridional overturning circulation and oceanic heat/material circulation.