Sea ice is a heterogeneous, evolving mosaic of individual floes, varying in spatial scales
from meters to tens of kilometers. Both the internal dynamics of the floe mosaic (floe‐floe …

Tropical cyclones are among the most destructive natural disasters. However, lack of
detailed observations and the simplifications inherent in operational ocean models, lead to …

Upper-ocean turbulence results from a complex set of interactions between submesoscale
turbulence and local boundary layer processes. The interaction between larger-scale …

We report novel observations of the onset and growth of Langmuir circulations (LCs) from
simultaneous airborne and subsurface in situ measurements. Under weak, fetch-limited …

Freshwater achieves its maximum density at a pressure-dependent temperature which is
above the freezing point, close to 4° C at ambient pressure for pure water. If the temperature …

This work evaluates the fidelity of various upper-ocean turbulence parameterizations subject
to realistic monsoon forcing and presents a finite-time ensemble vector (EV) method to better …

Abstract Observations in the Pacific Equatorial Undercurrents (EUC) show that the nighttime
deep-cycle turbulence (DCT) in the marginal-instability (MI) layer of the EUC exhibits …

Diurnal warm layers (DWLs) form near the surface of the ocean on days with strong solar
radiation, weak to moderate winds, and small surface-wave effects. Here, we use idealized …

Temperature and salinity profiles in the upper ocean are predicted using non-intrusive
reduced-order modeling with deep learning. The data from Large Eddy Simulations …

Temperature and salinity profiles in the upper ocean are predicted using non-intrusive
reduced-order modeling with deep learning. The data from Large Eddy Simulations …