Ocean Features
Ocean Water Properties
Ocean Circulation & Currents
Atmosphere Layers
Heat Transfer
100

A broad, flat area of the deep ocean floor.

abyssal plain

100

The amount of dissolved salt in ocean water.

salinity

100

A horizontal movement of ocean water caused mostly by wind.

surface current

100

The lowest layer of the atmosphere where weather occurs.

troposphere

100

The amount of water vapor in the air.

humidity

200

A long underwater mountain range where new seafloor forms.

mid-ocean ridge

200

A measure of how much mass is in a certain volume of water.

denisty

200

A current driven mostly by density differences in ocean water.

deep current

200

The layer above the troposphere that contains the ozone layer.

stratosphere

200

The temperature at which air becomes saturated and condensation begins.

dew point

300

A deep, narrow depression in the ocean floor formed by subduction.

trench

300

A water mass is usually identified using these two main characteristics.

temperature and salinity

300

Global circulation caused by differences in temperature and salinity.

thermohaline circulation

300

The coldest atmospheric layer.

mesosphere

300

When air contains the maximum amount of water vapor possible at that temperature.

saturation

400

An underwater volcanic mountain that does not reach the ocean surface.

seamount

400

The property that increases when salinity increases (assuming temperature stays constant).

density

400

The effect that causes moving water and air to curve due to Earth’s rotation.

coriolis effect

400

The layer where auroras occur and temperatures increase due to absorbing radiation.

thermosphere

400

When warm air is trapped above cooler air near the surface.

temperature inversion

500

A flat-topped seamount, usually caused by erosion when it was above sea level.

guyot

500

The name for a large section of ocean water that forms based on its density and tends to stay grouped together as it moves.

water mass

500

In thermohaline circulation, water sinks because it becomes colder and/or _______.

saltier water

500

The outermost layer where atmospheric particles can escape into space.

exosphere

500

When air is forced upward over a mountain range, cooling and forming clouds.

orographic lifting

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