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An unconfined aquifer is usually closer to Earth's surface where precipitation seeps down from above. The upper surface of an unconfined aquifer is called the water (table-source).
significant
table
deflection
warmer
surface
less
below
low
If the current is at, or near, the ocean surface, it's called a (deep-surface) current.
significant
table
deflection
warmer
surface
less
below
low
Confined aquifers are often found (above-below) unconfined aquifers.
significant
table
deflection
warmer
surface
less
below
low
If water cannot flow freely, an aquifer has a (low-high) permeability.
significant
table
deflection
warmer
surface
less
below
low
The Coriolis effect is the (reflection-deflection) of moving objects from a straight path because of Earth's rotation.
significant
table
deflection
warmer
surface
less
below
low
Warm water is (less-more) dense than colder water.
significant
table
deflection
warmer
surface
less
below
low
Water near the surface of the ocean around the equator is usually (warmer-colder) than water in other parts of the ocean.
significant
table
deflection
warmer
surface
less
below
low
Groundwater is a (insignificant-significant) source of drinking water.
significant
table
deflection
warmer
surface
less
below
low
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