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Wind and Ocean Currents Global winds Ocean Currents Local winds

Wind and Ocean Currents

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Wind and Ocean Currents . Global winds Ocean Currents Local winds. Coriolis Effect. Because the Earth rotates, and consists of a mixture of land and sea, the Coriolis Effect exists The Coriolis Effect is the movement of particles (such as air) to the right in the Northern Hemisphere - PowerPoint PPT Presentation

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Page 1: Wind and Ocean Currents

Wind and Ocean Currents

Global windsOcean Currents

Local winds

Page 2: Wind and Ocean Currents

Coriolis Effect

• Because the Earth rotates, and consists of a mixture of land and sea, the Coriolis Effect exists

• The Coriolis Effect is the movement of particles (such as air) to the right in the Northern Hemisphere

• How about the South?– They move to the left

Page 3: Wind and Ocean Currents

Coriolis Effect

Page 4: Wind and Ocean Currents

Air movement • Warm air raises; Cold air sinks moving into

the void left be the warm air • Air moves from high pressure to low

pressure

Page 5: Wind and Ocean Currents

Global winds

What beltAre we in?Westerlies

Page 6: Wind and Ocean Currents

Ocean Currents

• Surface Currents – In the upper 1000 m – Driven by temperature– Also know as the global ocean currents

• Density Currents – Driven by Density – More dense water sinks and where they

circulate for 500 to 2000 years

Page 7: Wind and Ocean Currents

Surface Currents • Warm Currents

– Driven by Winds (temperature)– Flow away from the equator towards the poles

• Cold Currents – Driven by Winds (temperature)– Flow away from the poles towards the equator

• Counter Currents – Flow the opposite of the “wind” currents – They “Fill” in the gaps

Page 8: Wind and Ocean Currents

Global ocean currents

Page 9: Wind and Ocean Currents

Doldrums

• Windless zones at the equator • Air moves vertically

• And current-less zone in the middle of the major ocean basins

• Water mover around them

Page 10: Wind and Ocean Currents

Local winds • Land Breeze • Cool air over the land • Warm air over water • Cold air slides into the

void left by the warm air rising

• Happens during nighttime

• Wind blowing from the land

• Sea breeze • Warm air over land • Cool air over water • Cold air slides into the

void left by the warm air rising

• Happens during daytime

• Wind blowing from the sea

Page 12: Wind and Ocean Currents

CONVECTIONMoves air in the atmosphere!

Page 13: Wind and Ocean Currents

CONVECTIONWind over the shore changes direction

because of EARTH’S UNEVEN

WARMING & COOLING!

Page 14: Wind and Ocean Currents

What About Convection in Water?

• Water and air are both fluids. • They both move due to convection!– Just like air, when liquid water is heated, it expands,

becomes less dense, and rises. Side note: Water is different, however, because of it’s unique

structure as a solid. Ice is actually less dense than liquid water whereas other substances are most dense as solids!

Page 15: Wind and Ocean Currents

CONVECTION IN LIQUIDS!

Page 16: Wind and Ocean Currents

Land Breeze

Wind

Page 17: Wind and Ocean Currents

Land Breeze

Wind

Page 18: Wind and Ocean Currents

Sea Breeze

Wind

Page 19: Wind and Ocean Currents

Sea breeze

Wind

Page 20: Wind and Ocean Currents