winds and ocean currents. latent heat transport 580 cal/g surface wind surface wind

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Winds and Ocean Currents

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Page 1: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Winds and Ocean Currents

Page 2: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Latent Heat Transport

580 cal/g

580 cal/g

Surface wind

Surface wind

Page 3: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

30o

0o

60o

Northern Hemisphere

Page 4: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

30o

0o

60o

Northern Hemisphere

Something is redirecting the wind

Hurricanes

Fronts

Page 5: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

The Coriolis EffectDue to the rotation of a spherical earth

What is the circumference of the Earth? ~ 25,000 miles

How long does it take for the earth to make one rotation? 24 hours

25,000 mi at 0o latitude

1042 mi/hr

0 mi/hr

Page 6: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

stationary

1042 mi/hr

Page 7: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

The Coriolis Effect

Velocity at 90o latitude

zero

Velocity at equator

1042 mi hr

Objects moving in the northern hemisphere deflect to the right of the direction of travel.

Page 8: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

The Coriolis Effect

Velocity at 90o latitude

zero

Velocity at equator

1042 mi hr

Objects moving in the northern hemisphere deflect to the right of the direction of travel.

1042 mi/hr

Stationary

Page 9: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

30o

0o

60o

Northern Hemisphere

The Coriolis Effect deflects the wind to the right of the direction of travel

Page 10: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

30o

0o

60o

The Coriolis Effect deflects the wind to the right of the direction of travel

Page 11: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Equator

30o

30o

60o

60o

Surface Winds

PrevailingWestelies

Tropical Easterlies

Page 12: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

In the Northern Hemisphere moving objects, including air,are deflected to the right of the direction of travel

In the Southern Hemisphere moving objects, including air,are deflected to the left of the direction of travel

Page 13: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

stationary

1042 mi/hr

Page 14: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

The Coriolis Effect

Velocity at 90o latitudezero

Velocity at equator

1042 mi hr

Objects moving in the southern hemisphere deflect to the left of the direction of travel.

Page 15: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Equator

30o

30o

60o

60o

In the Southern Hemisphere moving objects, including air,are deflected to the left of the direction of travel

Page 16: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Equator

30o

30o

60o

60o

Page 17: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Calm air

Calm air

descending

descending

rising

Page 18: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Hurricane Track

30o

0o

Page 19: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

30o

Page 20: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Sailing, Sailing…

30o

Trade winds(easterlies)

Westerlies

Page 21: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Winds and Ocean Currents

Page 22: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Ocean Surface Currents

1. Solar Heating (temp, density)2. Winds3. Coriolis

Forces

Page 23: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Density

Mass (g)Volume (cm3)

Solar Heating and Density

Water Expands as it is heated

Page 24: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Solar Heating

Heat expands water near the Equator,increasing its volume and creating a bulge

Equator

Page 25: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Solar Heating

equator

N

S

Heat expands water near the EquatorIncreasing its volume and creating a bulge

Water flows away from equator

Water flows toward pole

Water flows toward pole

Page 26: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

equator

pole

Sun’s

rays

General Circulation

EarthOcean

Page 27: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

General Circulation (North)

Surface Water

equator

30o

1. Solar Heating2. Winds3. Coriolis

Page 28: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Winds Guide the Direction of Surface Water

Winds blow to the west between0o and 30o latitude.

30o

0o

Page 29: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

General Circulation (North)

Surface Water

wind

equator

30o

Page 30: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

The Coriolis force deflects objectsTo the right of the direction of motion.

Page 31: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

East wind

Winds plus Coriolis Force

East winds blow water to the west

Coriolis deflects water to the right (east).

equator

30o

Page 32: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

East wind

West wind

Winds plus Coriolis Force

Coriolis deflects water to the right in the direction of travel (east).

Above 30o, westerlies push water to the east.

equator

30o

Page 33: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

East wind

West wind

Water encounters land and is deflected north and south.The bulk is deflected to the south, and Coriolis deflects it to the right

Below 30o, moving water encounters east wind and is moved to the west

Page 34: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Atlantic Gyre

Page 35: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Temperature/Energy Transfer

cool

warm

cool

Page 36: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Unusual Example of Heat Transport

Page 37: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Ireland EnglandSpain

Gulf Stream

Page 38: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Ireland EnglandSpain

cornwall

Page 39: Winds and Ocean Currents. Latent Heat Transport 580 cal/g Surface wind Surface wind

Next: Ocean Fundamentals