The contributions of autonomous underwater gliders as an observing platform in the in-situ
global ocean observing system (GOOS) are investigated. The assessment is done in two …

Double-diffusive convection (DDC) is a critical driving mechanism for diapycnal mixing in the
ocean. However, there is limited quantitative investigation on the impacts of dynamic ocean …

Using velocity and high-resolution temperature mooring data from the fore-reef slope of
Yongxing Island in the northwest South China Sea (water depth of 69 m), we examine the …

Thirty-four individual thermohaline sheets are identified at depths of 170–400 m in the
Canada Basin of the Arctic Ocean by using the hydrographical data measured with the Ice …

The internal wave climate in the deep Arctic Ocean, away from the shelves, is quiet because
the ice cover shields the ocean from wind energy input, and tidal amplitudes are small …

Motivated by a desire to understand the geothermal heating effects on ocean circulation, a
large‐scale circulation generated and sustained by thermal forcing at the surface subject to …

The ocean bottom is the Earth's least explored region, and the bottom mixed layer (BML) is
the pathway for communication between the ocean interior and the ocean floor. In this study …

Powell Lake contains a deep layer of relic seawater separated from the ocean since the last
ice age. Permanently stratified and geothermally heated from below, this deep layer is an …

Temporal variability in bottom water structures has been observed in 37‐h high‐resolution
temperature data at the ocean bottom up to 67.4 m on the continental shelf of the northern …

In this study we examined the applicability of the threshold, curvature, maximum angle, and
relative variance methods for identifying the oceanic bottom mixed layer (BML) thickness …