Gr11 Atmosphere Terminology, Quiz 1 Flashcards

1
Q

Adiabatic cooling

A

The process of decreasing heat through a change in air pressure caused by an air mass expanding.

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2
Q

Adiabatic heating

A

The process of increasing heat through a change in air pressure caused by an air mass compressing.

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3
Q

Albedo

A

Albedo is the fraction of insolation reflected from the Earth’s surface back into space. (1= high albedo vs 0= low albedo)

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4
Q

Convergence

A

The horizontal inflow of two different air masses towards a low pressure zone.

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5
Q

Coriolis force/effect

A

A force which causes a body that moves freely with respect to the rotating Earth to veer to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.

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6
Q

Equatorial low pressure belt

A

This area is in the earth’s equatorial region and is composed of warm, light ascending and converging air.

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7
Q

Equinox

A

Time of year when the sun crosses the equator, making daytime and night equal in length.

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8
Q

Ferrel’s Law

A

A law stating that due to the Coriolis force, winds are deflected to their right in the northern hemisphere and to their left in the southern hemisphere.

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9
Q

Insolation

A

Solar radiation falling on a unit area of the Earth’s surface.

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10
Q

Insolation angle of incidence

A

The angle at which the sun’s rays strike the Earth’s surface.

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11
Q

Polar high pressure belt

A

An area of high pressure located at 90• N/S. The air in this belt is extremely cold and dry.

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12
Q

Pressure gradient force

A

The force producing air flow from regions of high pressure to regions of low pressure.

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13
Q

Radiation budget

A

The balance of energy gain (from insolation) and energy loss (terrestrial radiation).

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14
Q

Solstice

A

Time of year when the sun is at its greatest distance from the equator.

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15
Q

Subtropical high pressure belt (Horse latitudes)

A

This is a zone of hot, dry air that forms as the warm air descending from the tropics heats adiabatically.

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16
Q

Subpolar low pressure belt

A

A zone of cool, wet weather caused by the meeting of cold air masses from higher latitudes and warm air masses from lower latitudes.