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.
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...
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.
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.
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.
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...
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.