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19 Cards in this Set

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Newton's First Law of Motion

Stationary objects tend to stay stationary unless an external force is applied to it.

Law of Inertia.

Newton's Second Law of Motion

Change of parcel pressure is equal to all gases in an air parcel multiplied by movement of the air parcel.

F=ma.

Newton's Third Law of Motion

For every actions there is an equal and opposite reaction.

Think collision and coalescence.

Buys Ballot's Law

Wind moves air parcels from high pressure to low pressure.


In Northern Hemisphere, wind at your back, low pressure is to your left.

Winds has upstream and downstream characteristics.

Contour Gradient Force

Initiates upper air winds between the surface and tropopause by increasing parcel pressure towards lower heights.

Change in height ÷ change in distance.

Pressure Gradient Force

Initiates surface winds by increasing parcel pressure towards lower pressure.

Change in pressure ÷ change in distance.

Coriolis Force

Deflects air parcels to the right in the Northern Hemisphere.

Opposes Contour and Pressure Gradient Force, by increasing parcel pressure to higher heights/pressure. Weaker at the Equator.

Centripetal Force

Increases parcel pressure inward to the center of a curved flow.

CeP= velocity^2 ÷ radius of rotation.

Centrifugal Force

Increases parcel pressure outward from the center of the curved flow.

CeP = mass × velocity^2 ÷ radius of rotation.

Frictional Force

Opposes motion and acts opposite of wind direction between surface Gradient Level or PBL.

Has no effect above Gradient Level.

When an air parcel sinks from the upper atmosphere...

Surface friction increases, wind speed decreases, wind directions backs with height.

Think Frictional Force.

When an air parcel rises from the surface to the upper atmosphere...

Friction decreases, speed increases, and wind directions veersl

Think Frictional Force.

Backs

Moves counter clockwise.

Veers

Moves clockwise.

Conservation of Momentum relative to wind.

Air parcels speed and direction do not change unless acted upon. Linear and Anglular Momentum.

Law of Inertia

Geostrophic Winds

Occurs when Coriolis and Gradient forces are balanced. Straight line and curved flow.

Linear and Angular Momentum.

Cyclonic

Counter clockwise motion, associated with lower heights/pressure.

CGF and CeP = CoF and CeF

Anticyclonic

Clockwise, associated with higher heights/pressure.

CGF and Cef = CoF and CeP

Gradient Wind

Occurs when atmosphere is out of balance, turmoil, curved flow. Increases velocity or mass of air parcels causing rotation.

State of turmoil.