1. Earth’s Oceans

3. Modern Oceanography
investigated ocean currents, water temperature and chemical composition, seafloor sediments and topography, and marine life. Technology included:
Nets
Bottom dredges
Sonar

4. Modern Oceanography
Sonar- (sound navigation and ranging)- determines ocean depth, uses the return time of an echo and the known velocity of sound in water
Velocity of sound in water= 1500 m/s
Advanced Technology
Satellites (Topex/Poseidon)- monitor ocean’s surface temperatures, currents, and wave conditions
Submersiles (underwater vessels) investigate the deepest trenches

5. Ocean Water: Salinity - Key Points
Salinity is the amount of dissolved solids/ salts in the oceans
Salinity, temperature, and density fluctuate within the ocean
Increased salinity and decreased temperature result in more dense water
Where do you think these salts come from?

6. Ocean Water: Salinity
The main source of these salts in seawater is chemical weathering of rocks on the continents
They reach the ocean through runoff
The other major source is the earth’s interior

7. Ocean Water: Salinity
In general, when the amount of water in the oceans changes, the salinity changes
Anything that increases the amount of water will decrease salinity (make the water more dilute)
Anything that decreases the amount of water will increase salinity
Brainstorm: what are some processes that could increase the water in oceans? Decrease the amount of water?

8. Ocean Water: Salinity Salinity and Density
Recap: What is density? What is its formula?
The two main factors that affect density are salinity and temperature
The higher the salinity, the more dense the water
Demo here

9. Ocean Water: Temperature and Density
At the surface of the ocean, temperature differences are mostly due to the amount of energy received from the sun
Areas at lower latitudes (closer to the equator) receive more direct, and intense sunlight and are therefore warmer

10. Ocean Movement

11. Why is Ocean Circulation Important?
Transport ~ 20% of latitudinal heat from the equator to the poles
Transports nutrients and organisms in important upwelling areas
Influences weather and climate
Influences commerce (economy)

12. Types of Currents Two main types of currents:
(1) surface currents – driven by wind
(2) deep water currents – driven by density and gravity
Let’s take a closer look.

13. -17 major surface currents that move quickly
How fast? A few miles/hr (Gulf Stream off of Miami = 4.5 mph)
How much? Total water in ocean surface circulation = about 100 Amazon Rivers (20 million m3/s).

14. Surface Currents Map
What do you notice about the current pattern in the northern hemisphere?
What do you notice about the current pattern in the southern hemisphere?

15. Surface Currents
Because of the earth’s rotation, currents are deflected to the RIGHT in the Northern Hemisphere and circulate clockwise. Surface currents are deflected to the LEFT in the Southern Hemisphere and circulate counterclockwise.
This is known as the Coriolis effect.
BOTTOM LINE: The Coriolis effect causes surface ocean currents to be deflected.

16. Gyres Gyres are closed systems of circulating water
The winds blowing from the east are called the Trade Winds. The winds blowing from the west are called Westerly Winds. These opposing wind systems contribute to the formation of  gyres.
Video showing ocean currents.

17. Global Conveyor Belt
The surface and deep water currents work together to transfer solar radiation from the equator to the poles and helps moderate Earth’s climate
Deep water currents are colder and higher in salinity, which keeps the currents in deep water
Surface water currents are warmed by the sun and are less dense because they contain lower levels of salinity
The surface and deep water currents work together to create the “Global Conveyor Belt”

18. Upwelling Winds push surface water offshore
Deeper water moves upward to replace the displaced surface water
Deeper water brings nutrients (phosphorus and nitrogen) up keeping the ocean ecosystem in balance and to create plankton (microorganisms) blooms

20. Surface Currents
The importance of upwelling.

21. Specific Heat
Specific heat capacity is amount of heat required to change a substances temperature by 1`C.
Not all things heat up at the same rate. It takes different amounts of energy to heat up different objects.
For example, aluminum foil heats up very quickly, however cools very quickly as well.
How long does it take to boil a pot of water?

22. Specific Heat
Water has a higher specific heat capacity than air. (Water is more resistant to changing temperature.)
Land heats and cools more rapidly than water. Land also reaches higher and lower temperatures than water
The temperature of the land and water influences the temperature of the air above it
This explains why inland areas experience greater temperature variations than cities near large bodies of water.

23. Climate
Climate- pattern of temperature and precipitation typical of an area over a long period of time.
Solar energy drives convection currents in the ocean. Surface currents warm or cool the air above it, influencing the climate of the land near the coast.

24. Land/Sea Breezes
Another process that occurs as a result of differences in density along coastlines are land and sea breezes.
Water has a higher specific heat capacity than sand, meaning it takes more energy to heat 1g of water than it would 1g of sand.
As a result, water also retains heat energy a lot longer as well.
Specific heats: Salt water: J/g Sand: .83 J/g
When you might first go to the beach during spring break, say in April when the air starts to warm up, what is the relative temperature of the water?

25. Land/Sea Breezes
SEA BREEZE: during the day, when the land heats up, the air rises
the beach will be warmer than the ocean, causing wind to move from the beach to the ocean, creating a sea breeze.
Due to a concentration
difference, this causes the
wind from the ocean to
travel toward the land.

26. Land/Sea Breezes
LAND BREEZE: during the night, ocean is warmer than the sand, causing wind to move from the ocean to the beach
The difference in density of these air masses has a very direct effect on the weather experienced along a coastline.