The climate is a forced and dissipative nonlinear system featuring nontrivial dynamics on a
vast range of spatial and temporal scales. The understanding of the climate's structural and …

Understanding the ocean requires determining and explaining global integrals and
equivalent average values of temperature (heat), salinity (freshwater and salt content), sea …

A Description of Local and Nonlocal Eddy–Mean Flow Interaction in a Global Eddy-Permitting
State Estimate in: Journal of Physical Oceanography Volume 44 Issue 9 (2014) Jump to …

Thermodynamics sets fundamental laws for all physical processes and is central to driving
and maintaining planetary dynamics. But how do Earth system processes perform work …

Kinematic backward trajectories are used to globally quantify the contributions of
temperature advection, adiabatic compression and diabatic processes to near‐surface …

The past years have seen the success of a novel and rigorous localized multiscale
energetics formalism in a variety of ocean and engineering fluid applications. In a self …

This paper investigates the multilayer Rayleigh–Taylor instability (RTI) using statistically
stationary experiments conducted in a gas tunnel. Employing diagnostics such as particle …

Biases in Thorpe-Scale Estimates of Turbulence Dissipation. Part II: Energetics Arguments and
Turbulence Simulations in: Journal of Physical Oceanography Volume 45 Issue 10 (2015) …

Zonal-mean storm-track shifts in response to perturbations in climate occur even in idealized
simulations of dry atmospheres with axisymmetric forcing. Nonetheless, a generally …

Boussinesq salt-water laboratory experiments of Rayleigh–Taylor instability (RTI) can
achieve mixing efficiencies greater than 0.75 when the unstable interface is confined …