PIPages
Labs

Andrey Shcherbina

University of Washington, WA·Earth & Environmental Science

The top layer of the ocean is constantly churned by wind, waves and currents. This turbulent layer, the ocean surface boundary layer (OSBL), controls how heat, gases and momentum move between the air and the deep ocean.

Fields

Earth & Environmental Science

Physics

Engineering

Topics

ocean turbulence

ocean surface boundary layer

anisotropy

Grants
1 known grant, through Mar 2027

What they work on

  1. Measure how anisotropic (direction-dependent) and inhomogeneous ocean surface boundary layer turbulence is, using two drifting Lagrangian floats each carrying customized ADCPs with 10 acoustic beams.
  2. Estimate how turbulent energy and energy flux are split across scales and directions from multi-directional velocity statistics, in a tidal channel and at Ocean Climate Station P in the North Pacific.
  3. Determine the extent of the isotropic inertial subrange and whether anisotropy can be predicted and parameterized for use in ocean and climate models.
  4. Assess how anisotropy biases existing turbulence measurement techniques, and build a dataset for benchmarking simulations and turbulence closures.

More about the research

Climate and ocean models cannot resolve its small eddies, so they rely on simplified rules. These rules usually assume that turbulence looks the same in every direction (isotropy) and in every place (homogeneity). Real ocean turbulence likely departs from this ideal because of shear, density layering and waves. Such departures may explain errors and disagreements among models.

Why it matters

Weather and climate forecasts depend on how well models represent mixing in the upper ocean. By measuring how real turbulence departs from idealized assumptions, this work could improve the rules that models use for ocean mixing. It could also lead to corrections for existing turbulence observations and better measurement practices, helping forecasts from local to global climate scales.

Known grants

From NIH and NSF research grants. Labs often have other funding we can't see.

Exploration of Anisotropy and Inhomogeneity of Ocean Boundary Layer Turbulence

NSF · Apr 2024 – Mar 2027

Closest labs

Amrapalli Garanaik

Oregon State University, OR·Earth & Environmental Science

Develop a new second-moment model of the upper ocean boundary layer that represents both local and nonlocal turbulent transport, tuned to observations and Large-Eddy Simulation results.

Brodie Pearson

Oregon State University, OR·Earth & Environmental Science

Develop statistical methods that use the anisotropy of turbulence to distinguish 3-D upper ocean mixing regimes driven by heating or cooling, wind shear and wave-wind interactions.

Tomas Chor

University of Maryland, MD·Earth & Environmental Science

Examine how symmetric instabilities, an overturning motion that grows at ocean fronts, modify the forward cascade of energy toward smaller scales at submesoscale fronts in the presence of mesoscale strain.

The school

University of Washington: 81 labs on PI Pages, $1.7B a year on research, 694 research doctorates a year.

More about University of Washington

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