2. Earth’s Oceans Divisions Dissolved Solids Dissolved Gases Upwelling https://www.youtube.com/watch?v=3GRA7ilM708

3. Freshwater vs. Seawater 3% of Earth’s water 3% of Earth’s water 2% in glaciers 2% in glaciers 1% lakes, rivers, & aquifers 1% lakes, rivers, & aquifers Mixture of substances not just pure H 2 O Mixture of substances not just pure H 2 O Minerals from rocks and pollutants from air get mixed in Minerals from rocks and pollutants from air get mixed in Density = 1.0g/cm 3 Density = 1.0g/cm 3 Freezes at 0 º C Freezes at 0 º C 97% of Earth’s water Mixture of substances 96.5% water and 3.5% dissolved salts NaCl is most abundant salt Dissolved gases include O, N, CO 2 Salinity varies from place to place Density = 1.02-1.03 g/cm 3 Freezes at -2 º C

4. Both Fresh and Seawater Respond to solar radiation (sunlight) Respond to solar radiation (sunlight) remember it is the sun that drives the water cycle remember it is the sun that drives the water cycle

5. Visible Light Visible light is both absorbed and reflected Visible light is both absorbed and reflected Most wavelengths are absorbed Most wavelengths are absorbed Blue light is reflected Blue light is reflected All wavelengths are absorbed by 100m depth so deep lakes and oceans are dark except for surface All wavelengths are absorbed by 100m depth so deep lakes and oceans are dark except for surface

6. Absorption of Light –Water absorbs light, which gives rise to another physical property of oceans—they are dark. –In general, light penetrates only the upper 100 m of seawater. –Light sufficient for photosynthesis exists only in the top 100 m of the ocean.

7. Infrared Rays Determine water temperature Determine water temperature Rapidly moving water does not have time to absorb infrared waves Rapidly moving water does not have time to absorb infrared waves Lakes and ponds become warm because absorb infrared rays Lakes and ponds become warm because absorb infrared rays Upper zone of ocean absorbs infrared so only surface is heated Upper zone of ocean absorbs infrared so only surface is heated Surface temperature varies with latitude Surface temperature varies with latitude Deep seawater is very cold Deep seawater is very cold

8. How Did the Oceans Form? About 4.5 billion years ago, there were no oceans. About 4.5 billion years ago, there were no oceans. Sometime before 4 billion years ago, water vapor in the atmosphere condensed and fell as rain. Sometime before 4 billion years ago, water vapor in the atmosphere condensed and fell as rain. The rain filled the deeper levels of Earth’s surface and the first oceans began to form. The rain filled the deeper levels of Earth’s surface and the first oceans began to form. https://www.youtube.com/watch?v=PoV4qSwg7nc

9.  All waterways on earth are connected to the oceans because almost all watersheds empty into the ocean.  Minerals and gases are carried along with the water and dissolve into seawater The Global Ocean

10.  Oceans produce most of the earth’s rain and oxygen (over 50%)  The ocean affects every person on Earth The Global Ocean

11. ≈ Pacific Ocean – largest (North and South) ≈ Atlantic Ocean - half the volume of Pacific (North and South) ≈ Indian Ocean - 3 rd largest ≈ Southern Ocean-Newest recognized in 2000 ≈ Arctic Ocean – smallest with most covered in ice Divisions of the Global Ocean

12. Divisions of Ocean All five of Earth’s oceans are connected to each other by the ocean currents creating 1 global ocean https://www.youtube.com/watch?v=vy6dj_ZWOos

13. Earth’s Oceans

14. Ocean water contains salt Ocean water is 96.5% water Ocean water is 96.5% water Plus, ions of dissolved salts Plus, ions of dissolved salts Evaporation removes pure water Evaporation removes pure water Leaving salt behind Leaving salt behind Low levels of nutrients (nitrogen and phosphorus) Low levels of nutrients (nitrogen and phosphorus) Oxygen is added by plants, bacteria, and atmospheric diffusion Oxygen is added by plants, bacteria, and atmospheric diffusion

15. Ocean water is vertically structured Temperature declines with depth Temperature declines with depth Heavier (colder, saltier) water sinks Heavier (colder, saltier) water sinks Light (warmer, less salty) water stays near the surface Light (warmer, less salty) water stays near the surface Temperatures are more stable than land temperatures Temperatures are more stable than land temperatures Water has high heat capacity (heat required to increase temperature by a given amount) Water has high heat capacity (heat required to increase temperature by a given amount) It takes more energy to warm water than air It takes more energy to warm water than air Oceans regulate Earth’s climate Oceans regulate Earth’s climate They absorb and release heat They absorb and release heat The ocean’s surface circulation moves heat around The ocean’s surface circulation moves heat around

16. What’s in Ocean Water? Oceans contain many dissolved solids and gases. Oceans contain many dissolved solids and gases. Dissolved solids like minerals and salts are eroded from the land as rivers travel to the sea. Dissolved solids like minerals and salts are eroded from the land as rivers travel to the sea. When the water evaporates, these minerals are left behind. This is why the ocean is salty. When the water evaporates, these minerals are left behind. This is why the ocean is salty. Some gases become dissolved in the ocean through wave action. Others come from photosynthesis and respiration of ocean organisms. Some gases become dissolved in the ocean through wave action. Others come from photosynthesis and respiration of ocean organisms.

17. Characteristics of Ocean Water Dissolved solids: Sodium chloride, or table salt, is the most abundant dissolved solid in the ocean. Other solids are also found in ocean water. Dissolved solids: Sodium chloride, or table salt, is the most abundant dissolved solid in the ocean. Other solids are also found in ocean water.

19. Salinity Amount of dissolved salts present in a sample of ocean water Amount of dissolved salts present in a sample of ocean water Described in parts per thousand Described in parts per thousand ppm this is the notation for parts per thousand ppm this is the notation for parts per thousand Changes in Salinity Climate and water movement affect salinity. Costal water in cool, humid places has a low salinity. Slow-moving bodies of water have higher salinity than other parts of the ocean do. Changes in Salinity Climate and water movement affect salinity. Costal water in cool, humid places has a low salinity. Slow-moving bodies of water have higher salinity than other parts of the ocean do. Salinity in various regions all differ Salinity in various regions all differ Range from 33ppm to 40ppm Range from 33ppm to 40ppm Average Salinity is 35ppm Average Salinity is 35ppm https://www.youtube.com/watch?v=EIDSMzXXzLM

20. Characteristics of Ocean Water Dissolved Gases Nitrogen, oxygen, and carbon dioxide are the main gases dissolved in ocean water. Dissolved Gases Nitrogen, oxygen, and carbon dioxide are the main gases dissolved in ocean water. More than half of Earth’s oxygen comes from the surface layers of the ocean. More than half of Earth’s oxygen comes from the surface layers of the ocean. About 93% of the world’s carbon dioxide is dissolved in the ocean. About 93% of the world’s carbon dioxide is dissolved in the ocean.

21. CO 2 Has more than 60 times that is the atmosphere Has more than 60 times that is the atmosphere Called carbon sink can trap CO 2 for thousands of years Called carbon sink can trap CO 2 for thousands of years

23. Behavior of Gases in Water You know that warm water dissolves solids more easily than cold water. You know that warm water dissolves solids more easily than cold water. Try to dissolve sugar in cold and warm water, and you’ll see that it’s true. Try to dissolve sugar in cold and warm water, and you’ll see that it’s true. Gases behave in the opposite way. Cold water dissolves gases more easily than warm water. Gases behave in the opposite way. Cold water dissolves gases more easily than warm water. Open a warm and a cold soda. The warm one will fizz more and go flat more quickly. Open a warm and a cold soda. The warm one will fizz more and go flat more quickly. This is because the CO 2 dissolved in the soda stays dissolved easier in cold water. This is because the CO 2 dissolved in the soda stays dissolved easier in cold water.

24. Behavior of Gases in Water Pressure also plays a role in how easily gases dissolve in water. Pressure also plays a role in how easily gases dissolve in water. If the water is under high pressure, gases dissolve more easily than water under no pressure. If the water is under high pressure, gases dissolve more easily than water under no pressure. To keep CO 2 dissolved in soda, it is bottled under pressure. When you open the soda, it loses pressure. The CO 2 fizzes out and the soda eventually goes flat. To keep CO 2 dissolved in soda, it is bottled under pressure. When you open the soda, it loses pressure. The CO 2 fizzes out and the soda eventually goes flat.

25. 25°CSurface0m 23°CSurface Zone 300m 5°CThermocline 700m 1°CDeep Zoneto1200m Temperature Zones

26. ≈ Sunlight heats the top 100m of the surface zone ≈ Surface currents mix the heated water with cooler water in surface zone Temperature Zones

27. Two factors affect surface temperatures: ≈ Latitude-water along equator is warmer because it receives more direct sunlight (So temp would be lowest at the poles.) ≈ Time of year-more direct sun during summer, so surface zone is heated more Surface Temperature Changes

28. Ocean Currents Oceans don’t just sit still. Oceans don’t just sit still. Currents move ocean water from place to place, moving nutrients and organisms with it. Currents move ocean water from place to place, moving nutrients and organisms with it. One very important kind of ocean current is upwelling. One very important kind of ocean current is upwelling.

29. Upwelling Defined as the movement of deep, cold, nutrient rich water to the surface. Defined as the movement of deep, cold, nutrient rich water to the surface. Because many nutrients sink to the bottom of the ocean, upwelling brings nutrients up where surface organisms can use them. Because many nutrients sink to the bottom of the ocean, upwelling brings nutrients up where surface organisms can use them. These nutrient rich waters near the surface create productive fisheries. These nutrient rich waters near the surface create productive fisheries. Let’s watch a video to see how this occurs: Let’s watch a video to see how this occurs: http://www.classzone.com/books/earth_science/terc/content/visualizations/es2 405/es2405page01.cfm http://www.classzone.com/books/earth_science/terc/content/visualizations/es2 405/es2405page01.cfm http://www.classzone.com/books/earth_science/terc/content/visualizations/es2 405/es2405page01.cfm http://www.classzone.com/books/earth_science/terc/content/visualizations/es2 405/es2405page01.cfm http://www.youtube.com/watch?v=APMzM-xYlOs http://www.youtube.com/watch?v=APMzM-xYlOs http://www.youtube.com/watch?v=APMzM-xYlOs

30. Upwelling Wind blows away from the shore, taking surface water with it. Wind blows away from the shore, taking surface water with it. Deep water “wells up” to replace the surface water. Deep water “wells up” to replace the surface water. This brings deep, cold, This brings deep, cold, nutrient rich water up to the surface.