深海の高速「バタフライ効果」を解明(Scientists Unravel the Fast-Moving ‘Butterfly Effect’ of the Deep Ocean)

2026-07-14 カリフォルニア大学サンディエゴ校(UCSD)

米国カリフォルニア大学サンディエゴ校(UC San Diego)スクリプス海洋研究所の研究チームは、深海で発生する小規模な乱流や渦が短時間のうちに広範囲へ影響を及ぼす「深海のバタフライ効果」を解明した。研究では、高解像度の数値シミュレーションと海洋観測データを組み合わせて解析し、海底地形や局所的な流れによって生じた微細な乱流が、エネルギーや物質を効率よく周囲へ伝達し、深層循環や海洋混合に大きく寄与することを明らかにした。従来は局所現象と考えられていた小規模な変動が、海洋全体の循環や熱・炭素・栄養塩の輸送、さらには気候システムにも影響を及ぼす可能性が示された。この成果は、深海循環の理解を深めるとともに、地球規模の気候モデルや海洋予測の精度向上に役立つ重要な知見となる。

深海の高速「バタフライ効果」を解明(Scientists Unravel the Fast-Moving ‘Butterfly Effect’ of the Deep Ocean)
The myriad paths of turbulent mixing in the ocean and the forces that influence them. Image: Cimoli et al, Nature Communications

<関連情報>

海洋内部における小規模乱流の気候的影響範囲 Climatic reach of small-scale turbulence in the ocean interior

Laura Cimoli,Ali Mashayek,Alberto C. Naveira Garabato,Colm-cille P. Caulfield,Matthew H. Alford,Lois Baker,B. B. Cael,Bieito Fernández Castro,Casimir de Lavergne,Elizabeth Ellison,Geoffrey Gebbie,Jonathan Gula,Patrick Heimbach,Joshua Lanham,Arnaud Le Boyer,Kate Oglethorpe,W. Richard Peltier,Helen R. Pillar,Alexander M. Piotrowski,Sarah G. Purkey,Nick Reynard,Emily Shuckburgh,Martin J. Siegert,Alessandro Silvano,… Bethan L. Wynne-Cattanach
Nature Communications  Published:09 July 2026
DOI:https://doi.org/10.1038/s41467-026-73809-3

Abstract

Small-scale turbulent mixing in the ocean interior is vital in governing ocean circulation and tracer distributions, and hence global climate. However, the planetary extent of this role and its dependence on the microphysics of mixing remain inadequately understood. Here, we emphasize the variety of spatio-temporal scales on which such interior turbulent mixing can shape the climate system. In addition to its well-established role in facilitating the equilibration of deep branches of ocean circulation on centennial-to-millennial timescales, interior turbulent mixing is a leading determinant of oceanic tracer budgets on timescales as short as sub-annual. We highlight the importance of the co-dependence of vertical (diapycnal) mixing and lateral (isopycnal) stirring in establishing the large-scale impacts of oceanic turbulence. We conclude with a summary of theoretical, observational and computational bottlenecks in the way of a sufficiently accurate representation of mixing in Earth System Models, and discuss emerging opportunities for making progress in these areas.

1702地球物理及び地球化学
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