air motions geology 390 wsuv dr. robert m mackay

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Air Motions Geology 390 WSUV Dr. Robert M MacKay

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Page 1: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Air Motions

Geology 390WSUV

Dr. Robert M MacKay

Page 2: Air Motions Geology 390 WSUV Dr. Robert M MacKay

1st Law (Law of Inertia)

Every object continues in its state of rest, or of uniform motion in a straight line, unless it is compelled to change that state by forces impressed upon it.

acceleration = 0.0 unless the objected is acted on by an unbalanced force

Page 3: Air Motions Geology 390 WSUV Dr. Robert M MacKay
Page 4: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Forces that influence the wind

1. Pressure Gradient Force

2. Coriolis Force

3. Friction

On average Gravity nearly balances the vertical Pressure gradient(hydrostatic balance)

Page 5: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Fig. 8-16, p. 203

Page 6: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Pressure Gradient=∆P/dist

Page 7: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Pressure Gradient

Page 8: Air Motions Geology 390 WSUV Dr. Robert M MacKay
Page 9: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Centrifugal force an (Apparent Force)

Page 10: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Centrifugal force an (Apparent Force)

Page 11: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Coriolis Force (apparent force due to Earth’s rotation)

Page 12: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Coriolis Force

Deflects air to right in NH& Left in SH

Is always zero at the equator

Increases with latitude

Increases with wind speed

Increases as planet rotation speed increase

Page 13: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Coriolis Force

Page 14: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Coriolis Force

Page 15: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Geostrophic Winds

Page 16: Air Motions Geology 390 WSUV Dr. Robert M MacKay

Geostrophic Winds

Page 17: Air Motions Geology 390 WSUV Dr. Robert M MacKay
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