activity
20132023
most citedCrawling scallop: Friction-based locomotion with one degree of freedom

44 citations · 107 across the 8 of their papers we have counts for

collaborators

8 papers

physics.flu-dyn2023

Transition to turbulence in wind-drift layers

Gregory LeClaire Wagner, Nick Pizzo, Luc Lenain +1

A light breeze rising over calm water initiates an intricate chain of events that culminates in a centimeters-deep turbulent shear layer capped by gravity-capillary ripples. At fir…

physics.ao-ph2023★ 3 cited

Formulation and calibration of CATKE, a one-equation parameterization for microscale ocean mixing

Gregory LeClaire Wagner, Adeline Hillier, Navid C. Constantinou +7

We describe CATKE, a parameterization for fluxes associated with small-scale or "microscale" ocean turbulent mixing on scales between 1 and 100 meters. CATKE uses a downgradient fo…

physics.ao-ph2022★ 4 cited

Stokes drift should not be added to ocean general circulation model velocities

Gregory LeClaire Wagner, Navid C. Constantinou, Brandon G. Reichl

Studies of ocean surface transport often invoke the "Eulerian-mean hypothesis": that wave-agnostic general circulation models neglecting explicit surface waves effects simulate the…

stat.AP2021★ 23 cited

Epidemic Management and Control Through Risk-Dependent Individual Contact Interventions

Tapio Schneider, Oliver R. A. Dunbar, Jinlong Wu +8

Testing, contact tracing, and isolation (TTI) is an epidemic management and control approach that is difficult to implement at scale because it relies on manual tracing of contacts…

physics.ao-ph2020★ 17 cited

Capturing missing physics in climate model parameterizations using neural differential equations

Ali Ramadhan, John Marshall, Andre Souza +8

We explore how neural differential equations (NDEs) may be trained on highly resolved fluid-dynamical models of unresolved scales providing an ideal framework for data-driven param…

physics.flu-dyn2016★ 16 cited

An asymptotic model for the propagation of oceanic internal tides through quasi-geostrophic flow

Gregory L. Wagner, Gwenael Ferrando, William R. Young

Starting from the hydrostatic Boussinesq equations, we derive a time-averaged `hydrostatic wave equation' that describes the propagation of inertia-gravity internal waves through q…