1 / 37

Extra Credit #3

Extra Credit #3. May 2 (Monday), 7:30pm Byrne Lecture Dr. Eddie Bernard, NOAA “Tsunamis” Austin Auditorium LaSells Stewart center 1-page reaction paper to your TA. Reminder:.

jterrance
Download Presentation

Extra Credit #3

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Extra Credit #3 • May 2 (Monday), 7:30pmByrne LectureDr. Eddie Bernard, NOAA“Tsunamis”Austin AuditoriumLaSells Stewart center1-page reaction paper to your TA

  2. Reminder: • Interviews with instructors must be completed by this Friday (April 29)Dr. Wright’s office hours are:MW 1:50-3pm or just before classDr. Duncan’s office hours are:MWF 3-4pm in COAS Admin Bldg

  3. Physical and Chemical Structure of the Ocean Why are the oceans blue? How do you keep your beer cool in the tropics?

  4. Light Absorption in Water

  5. Why do objects lose their color with depth? • The colors other than blue (and green) are absorbed by the water molecules in the first few meters -- only blue (and green) are reflected

  6. Sound in Sea Water • Sound is transmitted better in water than it is in air • Sound velocity in the ocean is about 1500 m/s, or about 4 times its speed in air

  7. SOFAR Sound Channel • Sound is focused into the SOFAR channel because it is a low velocity region • Sound is transmitted best through this channel -- good for whales and submarines

  8. Heard Island Experiment • Global Warming -- faster velocity??

  9. Solar Heating • Uneven heating of Earth’s surface • Release of heat asinfrared radiation • Requires flow ofheat by oceans andatmosphere

  10. Global Heat Budget • heatat the Earth's surface (342 W/m2) is supplied by absorption of ‘short-wave’ solar radiation from the sun. • heat lost from Earth is through long-wave radiation back to space.

  11. The Greenhouse Effect • The Atmosphere is transparent to sunlight (ultraviolet (UV) and visible) • Clouds absorb or reflect about half • Sunlight heats the Earth’s surface, which then radiates energy as longer wavelength energy (Infrared) • This energy is trapped by the atmospheric gases (CO2, H2O, CH4)

  12. Special Properties of Water • RECALL:Melting and boiling points are very highHighest heat capacity of common liquidsHigh heat of fusion and vaporization

  13. Sea Surface Temperaturesonly 0°-30°C world-wide Land: 50°C to -50°C

  14. Local Annual Heat Budgets • Amount of solar energy captured at one location on the Earth varies with season

  15. Temperature (vertical profile)

  16. Temperature (vertical profile) Beer goes here

  17. Temperatures with Depth • Thermocline -- sharp temperature change

  18. Evaporation - Precipitation • Over the oceans, evaporation exceeds precipitation • The balance is restored by rain over the continents, returning water via rivers

  19. Evaporation vs Precipitation

  20. Climate Belts

  21. Ocean Surface Salinity

  22. Salinity Variations

  23. Chemistry of River and Ocean Water • Can’t just concentrate river water to get seawater • How do we explain this observation?

  24. Concept of Residence Time • Each element removed from ocean in different ways • And at different rates • e.g. Cl- vs. SiO2

  25. Residence Time F has units of mass per unit time R has units of mass R/F has units of time

  26. Salinity Variations • Surface salinity follows evaporation-precipitation pattern • Atlantic Ocean is generally more salty than Pacific Ocean, in spite of river input -- why??

  27. Isthmus of Panama • Net transfer offresh waterfrom Atlanticto Pacific

  28. Density of Sea Water(Where does Oregon’s seawater plot?) o *

  29. Density of Sea Water(Where does Oregon’s seawater plot?) Oregon’s ocean o Bottom Water *

  30. Density Rules!

  31. Where does the Ocean’s Deepest Water Come From? • The densest seawater is COLD and SALTY • This is formed at high latitudes in the North and South Atlantic: North Atlantic Deep Water (NADW) Antarctic Bottom Water (AABW) • Could dense seawater form in the tropics? (evaporation!)

  32. Dissolved Gases in the Ocean

  33. Important Gases in the Ocean • Oxygen -- Respiration, Decomposition • CO2 -- Photosynthesis, CaCO3 • Nitrogen -- Nutrient for growth • Methane -- a product of decomposition

  34. Photosynthesis and Respiration • Biology interacts with the Chemistry

  35. Dissolved Oxygen

  36. Biochemical Recycling

  37. Summary: Biochemical Cycles • Nutrients enter oceans through rivers • Gases enter oceans thru air-sea boundary • Biology alters distribution of nutrients and gases • Circulation returns nutrients to surface • Interaction of physics, chemistry and biology => geological record (sediments)

More Related