Related Experiment Video
Updated: Aug 5, 2026

Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
Compensation of horizontal temperature and salinity gradients in the ocean mixed layer
Abstract:
Establishment of the temperature-salinity relationship in the ocean has concerned oceanographers for decades because of its importance for understanding ocean circulation. High-resolution measurements in the ocean mixed layer are used to show that temperature and salinity gradients on horizontal scales of 20 meters to 10 kilometers tend to compensate in their effect on density. These observations support the notion of a horizontal mixing in the mixed layer that depends on density gradient.
Related Concept Videos
Osmoregulation in Fishes
Damped Oscillations
Although friction and other non-conservative...
Magnetostatic Boundary Conditions
Fluid Pressure over Curved Plate of Constant Width
Gradient Fields
Marine Microbial Ecology

