Multiyear turbulence measurements from oceanographic moorings in equatorial Atlantic and
Pacific cold tongues reveal similarities in deep cycle turbulence (DCT) beneath the mixed …

Microstructure observations in the Pacific cold tongue reveal that turbulence often
penetrates into the thermocline, producing hundreds of watts per square meter of downward …

The equatorial Pacific cold tongue is a site of large heat absorption by the ocean. This heat
uptake is enhanced by a daily cycle of shear turbulence beneath the mixed layer—“deep …

Given the increasing attention in forecasting weather and climate on the subseasonal time
scale in recent years, National Oceanic and Atmospheric Administration (NOAA) announced …

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 …

In the tropical Pacific, weak ventilation and intense microbial respiration at depth give rise to
a low dissolved oxygen (O2) environment that is thought to be ventilated primarily by the …

Deficiencies in upper ocean vertical mixing parameterizations contribute to tropical upper
ocean biases in global coupled general circulation models, affecting their simulated ocean …

We use a version of the NOAA Climate Forecast System with enhanced (up to 1‐m) ocean
model vertical resolution to investigate the mean diurnal cycles of upper ocean temperature …

The impacts of rainy days (> 24 mm) on the physics of the surface atmosphere and upper
ocean are characterized in the central Pacific Ocean (140°–170° W) on the equator, where …

Computational models of the oceanic and atmospheric circulation are critical tools for un-30
derstanding and projecting changes in the Earth's climate. These models have errors that …