Top Banner
IB Oceans and their Coastal Margins B1 – Introduction to Oceans
17
Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: L1 introduction to oceans

IB Oceans and their Coastal Margins

B1 – Introduction to Oceans

Page 2: L1 introduction to oceans

World’s Oceans

Page 3: L1 introduction to oceans

Distribution of Oceans• The world’s oceans are referred to collectively

as the “world ocean”.• Boundaries that separate the oceans are

arbitrary and blurred.• Size of oceans varied from largest to smallest:– Pacific– Atlantic– Indian– Southern– Arctic

Page 4: L1 introduction to oceans

Water in the Oceans

• Volume – 1.185 billion cubic kilometres• 97.3% of all water on the planet.• Chemical composition of water in each of the

oceans is very similar from place to place -> varies little from year to year.

• Inputs to Ocean Water– Water (from rivers, glaciers, rain)– Chemicals (dissolved mineral

Page 5: L1 introduction to oceans

Ocean Currents

Two types of ocean currents:• Surface Ocean Currents• Deep Ocean Currents

What do currents do?• Regulate the world’s climate.• Important for marine life.

Page 6: L1 introduction to oceans

• Ocean currents occur because there is very little friction between the ocean waters and the solid earth.

• As the earth rotates the water moves differently to the solid crust and the lighter atmosphere.

• Surface currents move at 9km per hour, deep currents move at 1km per hour.

Page 7: L1 introduction to oceans
Page 8: L1 introduction to oceans

Deep Ocean Currents

Page 9: L1 introduction to oceans

Deep Ocean Currents

• Deep Ocean Currents occur between the ocean bottom and 400m below the surface.

• Created by difference in water density.• Cold or salty water is more dense than warm

or less salty water.• One cycle of the ocean conveyor belt can take

1,000 years to complete.

Page 10: L1 introduction to oceans

Surface Currents

Page 11: L1 introduction to oceans

Surface Currents• Surface currents are driven by the wind.• World’s prevailing winds create giant circular

currents in the major ocean basins.• Subtropical high pressure areas at 30 degrees

latitude. • Combination of friction and coriolis force water does

not create exactly parallel to the wind direction.• Coriolis Force – created by the rotation of the earth. – Water pulls to the right in the northern hemisphere– Water pulls to the left in the southern hemisphere.

Page 12: L1 introduction to oceans

Major Ocean Currents

Page 13: L1 introduction to oceans

Ocean Gyres

Gyre – any large system of rotating ocean current.

Gyres are caused by the Coriolis effect – planetary motion along with friction.

There is a major Gyre for each ocean system.

Page 14: L1 introduction to oceans

Ocean Currents Affect Temperature

• Warm Currents carry water Polewards and raise the air temperature of the maritime environments where they flow.

• Cold currents carry water towards the equator and so lower the temperature of coastal areas.

• Main ocean currents follow a circular pattern.

Page 15: L1 introduction to oceans

What is this image showing? Why?

Page 16: L1 introduction to oceans

Questions

1. Why does the chemical composition of the oceans remain fairly constant over time? (hint: think inputs / outputs)

2. Outline the impact of ocean currents on the climatic differences between the eastern and western sides of continents.

Page 17: L1 introduction to oceans

www.oceanmotion.org