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Life Goes On: Fishes: Survival in a Challenging Environment
03:05

Life Goes On: Fishes: Survival in a Challenging Environment

Two features of water, viscosity and density, present challenges for fishes that are very different from what animals who live on land or in the air must face. Fishes have been able to meet these challenges through a number of physiological adaptati...

Its in the Water: Thermohaline Circulation
01:11

Its in the Water: Thermohaline Circulation

Thermohaline circulation is driven by differences in temperature and salinity, as opposed to circulation driven by wind. Understanding patterns of water movement may be crucial to better understanding global climate and climate change.

Its in the Water: Salinity, Density, and Temperature
03:51

Its in the Water: Salinity, Density, and Temperature

Obtaining accurate salinity measurements is vitally important because salt, along with temperature, has a significant impact on the density of seawater. And this, in turn, greatly affects ocean structure and circulation.

World in Motion: Heat, Convection and Plate Tectonics
05:54

World in Motion: Heat, Convection and Plate Tectonics

Most scientists believe heat and convection probably play a major role in plate tectonics. And, yet, many questions remain.

Deep Connections: Tracers
07:03

Deep Connections: Tracers

A tracer is a property or substance that can be used to track the movement of individual water masses. While the utility of specific tracers varies according to the locale and circumstance, tracers as a group provide a rich source of information ab...

Deep Connections: Water Masses
04:06

Deep Connections: Water Masses

Water masses are layers of water distinguished by a particular temperature and salinity. Understanding how water masses form and move around is critical in understanding global climate.

Deep Connections: Thermohaline Circulation
01:43

Deep Connections: Thermohaline Circulation

The movement of water due to differences in density is called thermohaline circulation. This process is responsible for not only the vertical movement of ocean water, but for the circulation of the global ocean as a whole.