Seawater Properties & Processes
Surface Circulation
Large-Scale Circulation
Waves
Tides
100

This measure of dissolved salt content averages about 35‰ in the ocean.

salinity

100

hese large surface-current loops are driven by global wind belts and Earth’s rotation.

gyres

100

This “global conveyor belt” is driven by density differences in seawater.

thermohaline circulation

100

These waves form when wind blows across the water’s surface.

wind waves

100

The twice-daily rise and fall of sea level is primarily caused by this celestial body.

the Moon

200

The process by which cold, salty water sinks in polar regions, helping drive thermohaline circulation.

deep-water formation

200

The deflection of moving water due to Earth’s rotation is known as this effect.

What is the Coriolis effect?

200

ENSO stands for this phenomenon affecting global ocean–atmosphere systems.

El Niño–Southern Oscillation

200

The depth at which wave orbital motion becomes negligible is approximately this fraction of the wavelength.

½ the wavelength

200

This type of tide has one high and one low tide per day.

diurnal tide

300

This gas is more soluble in colder water, making high-latitude oceans important sinks for it.

CO₂

300

This western boundary current is the fastest and most well-known in the North Atlantic.

Gulf Stream

300

During La Niña, upwelling off this country strengthens significantly.

Peru

300

These long-period waves generated by seismic activity can travel across entire oceans.

tsunamis

300

When the Sun, Moon, and Earth are aligned, this type of tide occurs.

spring tides

400

The rapid change in temperature with depth creates this boundary layer.

thermocline

400

Converging Ekman transport in subtropical gyres causes the formation of this “hill” of water.

Ekman convergence / geostrophic doming

400

This mid-depth circulation cell in the southern hemisphere is critical for distributing carbon and nutrients.

Antarctic Intermediate Water (AAIW)

400

In shallow water, wave speed depends primarily on this physical parameter.

water depth

400

The difference in height between consecutive high and low tides is known as this.

tidal range

500

Light penetration in the upper ocean defines this biologically productive zone.

euphotic (photic) zone

500

The angle between surface winds and the net direction of water movement is approximately this many degrees.

90° (but 45° for the uppermost layer)?

500

he deep water mass formed in the North Atlantic is specifically called this.

North Atlantic Deep Water (NADW)

500

The bending of waves as they approach shore at an angle is called this.

wave refraction

500

The tidal bulge on the side opposite the Moon is created primarily by this force.

centrifugal force from the Earth–Moon system