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The name for the seawater ice, that essentially doubles the size of the continent, is called sea ice.

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11y ago

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What kind of currents forms when more dense seawater moves toward less dense seawater?

A density current forms when more dense seawater moves toward less dense seawater.


What kind of currents forms when more dense seawater moves towards less dense seawater?

A density current forms when more dense seawater moves toward less dense seawater.


What kind of current forms when denser seawater sinks under less seawater?

riptide


What forms when more dense seawater sinks under less dense seawater?

Density current


What kind of current froms when more dense seawater move toward less dense seawater?

A density current forms when more dense seawater moves toward less dense seawater.


How density current forms?

Density currents - more dense seawater sinking beneath less dense seawater.


When is Antarctica smaller and bigger?

The continent of Antarctica does not change size. However, the ice sheet that covers 98% of the continent during summer merges with the sea ice that forms during the winter, effectively doubling the size of the continent.


What causes the density in the mediterranean sea?

the answer to this question is a density current forms when more dense seawater sinks beneath less dense seawater


What causes the density current in the mediterranean?

the answer to this question is a density current forms when more dense seawater sinks beneath less dense seawater


What 2 water forms in Antarctica?

Any water in Antarctica forms into ice, either sea ice or fresh-water ice.


How big is antarctica in winter?

The continent of Antarctica remains the same -- about 10% of the earth's surface. However, the ice sheet that covers 98% of the continent joins with the sea ice that freezes, and essentially doubles the size of the mass.


What kind of current forms when more dense seawater moves towards less dense seawater?

A density current forms when denser seawater moves towards less dense seawater. This movement occurs due to differences in temperature and salinity, causing the denser water to sink and flow along the seabed towards less dense seawater. This process helps distribute nutrients and maintain ocean circulation.