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Beneath the Surface: Using Sound to Study the Ocean's Interior
02:17

Beneath the Surface: Using Sound to Study the Ocean's Interior

Sound is sometimes used to study the ocean's interior. For example, the speed of sound in the ocean can be used to measure the temperature between the source and the receiver.

Its in the Water: Measuring Salinity
02:59

Its in the Water: Measuring Salinity

Efforts to measure salinity have long been a fundamental part of chemical oceanography. At one time, this was done by simply weighing the salt. Then, for years, salinity was determined based on the concentration of chloride. Today, salinity is measu...

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.

The Ocean's Memory: Sediments and Past Climate
05:09

The Ocean's Memory: Sediments and Past Climate

As sediments get laid down, they carry with them a record of the kind of environment in which they were formed. Scientists can read that record and learn valuable information about past climate and temperature change.

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.