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

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Presentation transcript:

Winds and Ocean Currents

Latent Heat Transport 580 cal/g Surface wind Surface wind

30 o 0o0o 60 o Northern Hemisphere

30 o 0o0o 60 o Northern Hemisphere Something is redirecting the wind Hurricanes Fronts

The Coriolis Effect Due 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 0 o latitude 1042 mi/hr 0 mi/hr

stationary 1042 mi/hr

The Coriolis Effect Velocity at 90 o latitude zero Velocity at equator 1042 mi hr Objects moving in the northern hemisphere deflect to the right of the direction of travel.

The Coriolis Effect Velocity at 90 o latitude zero Velocity at equator 1042 mi hr Objects moving in the northern hemisphere deflect to the right of the direction of travel mi/hr Stationary

30 o 0o0o 60 o Northern Hemisphere The Coriolis Effect deflects the wind to the right of the direction of travel

30 o 0o0o 60 o The Coriolis Effect deflects the wind to the right of the direction of travel

Equator 30 o 60 o Surface Winds Prevailing Westelies Tropical Easterlies

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

stationary 1042 mi/hr

The Coriolis Effect Velocity at 90 o latitude zero Velocity at equator 1042 mi hr Objects moving in the southern hemisphere deflect to the left of the direction of travel.

Equator 30 o 60 o In the Southern Hemisphere moving objects, including air, are deflected to the left of the direction of travel

Equator 30 o 60 o

Calm air descending rising

Hurricane Track 30 o 0o0o

Sailing, Sailing… 30 o Trade winds (easterlies) Westerlies

Winds and Ocean Currents

Ocean Surface Currents 1. Solar Heating (temp, density) 2. Winds 3. Coriolis Forces

Density Mass (g) Volume (cm 3 ) Solar Heating and Density Water Expands as it is heated

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

Solar Heating equator N S Heat expands water near the Equator Increasing its volume and creating a bulge Water flows away from equator Water flows toward pole

equator pole Sun’s rays General Circulation Earth Ocean

General Circulation (North) Surface Water equator 30 o 1. Solar Heating 2. Winds 3. Coriolis

Winds Guide the Direction of Surface Water Winds blow to the west between 0 o and 30 o latitude. 30 o 0o0o

General Circulation (North) Surface Water wind equator 30 o

The Coriolis force deflects objects To the right of the direction of motion.

East wind Winds plus Coriolis Force East winds blow water to the west Coriolis deflects water to the right (east). equator 30 o

East wind West wind Winds plus Coriolis Force Coriolis deflects water to the right in the direction of travel (east). Above 30 o, westerlies push water to the east. equator 30 o

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

Atlantic Gyre

Temperature/Energy Transfer cool warm cool

Unusual Example of Heat Transport

Ireland England Spain Gulf Stream

Ireland England Spain cornwall

Next: Ocean Fundamentals