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Updated: Jan 29, 2026

Using Generative Art to Convey Past and Future Climate Transitions
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Ocean mesoscale mixing linked to climate variability.

Julius J M Busecke1, Ryan P Abernathey2

  • 1Princeton University, Princeton, NJ, USA.

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Ocean mixing varies year-to-year globally, influenced by large-scale currents, not just local eddies. This finding impacts climate models and understanding of ocean heat, salt, and carbon transport.

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Area of Science:

  • Oceanography
  • Climate Science
  • Geophysics

Background:

  • Mesoscale turbulence is crucial for ocean circulation, water mass formation, and tracer transport.
  • Understanding how ocean mixing varies over climate timescales remains a significant knowledge gap.

Purpose of the Study:

  • To present the first time-resolved global dataset of lateral mesoscale eddy diffusivities at the ocean surface.
  • To investigate the drivers of variability in ocean mixing on interannual timescales.

Main Methods:

  • Application of the suppressed mixing length theory.
  • Analysis of satellite-observed ocean velocities.
  • Correlation of mixing variability with climate indices (ENSO, NAO, DMI, PDO).

Main Results:

  • Global interannual variability in lateral mesoscale eddy diffusivities was identified.
  • Variability in mixing length, driven by large-scale flow, was found to be a dominant factor, exceeding local eddy kinetic energy effects.
  • Regional correlations with major climate indices were observed.

Conclusions:

  • The study reveals a novel mechanism for ocean mixing variability driven by large-scale flow dynamics.
  • This mechanism, currently absent in global climate models, may significantly influence global heat, salt, and carbon distribution.
  • Findings have implications for ocean ecosystems and regional climate dynamics, including ENSO variance.