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Global Warming

011. Global Warming. Vernal equinox March 21 Sun vertical at equator. Northern Hemisphere Names. Winter solstice Dec. 22 Sun vertical at 23.5 o S. Winter solstice Dec. 22 Sun vertical at 23.5 o S. Summer solstice June 21 Sun vertical at 23.5 o N. Autumnal equinox Sep. 23

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Global Warming

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  1. 011 Global Warming

  2. Vernal equinox March 21 Sun vertical at equator Northern Hemisphere Names Winter solstice Dec. 22 Sun vertical at 23.5oS Winter solstice Dec. 22 Sun vertical at 23.5oS Summer solstice June 21 Sun vertical at 23.5oN Autumnal equinox Sep. 23 Sun vertical at equator

  3. Earth further from sun Earth closer to sun

  4. The radiant energy emitted by the sun. It is highest at the equator and lowest at the poles. Solar irradiance- We are interested in conditions near the Earth’s surface What are some factors that effect exposure to irradiance?

  5. Non-rotating Earth Convection cell model

  6. Add rotation and add landmasses unequal heating and cooling of the Earth

  7. Physical properties of the atmosphere: Density • Warm, low density air rises • Cool, high density air sinks • Creates circular- moving loop of air (convection cell)

  8. Physical properties of the atmosphere: Water vapor • Cool air cannot hold much water vapor, so is typically dry • Warm air can hold more water vapor, so is typically moist • Water vapor decreases the density of air

  9. Physical properties of the atmosphere: Pressure • A column of cool, dense air causes high pressure at the surface, which will lead to sinking air • A column of warm, less dense air causes low pressure at the surface, which will lead to rising air

  10. 90o High pressure, dry climate 60o Low pressure, wet climate High pressure, dry climate 30o ITCZ intertropical convergence zone= doldrums Low pressure, wet climate 0o 30o 60o 90o

  11. Idealized winds generated by pressure gradient and Coriolis Force.  • Actual wind patterns owing to land mass distribution..

  12. The Coriolis effect • The Coriolis effect • Is a result of Earth’s rotation • Causes moving objects to follow curved paths: • In Northern Hemisphere, curvature is to right • In Southern Hemisphere, curvature is to left • Changes with latitude: • No Coriolis effect at Equator • Maximum Coriolis effect at poles

  13. The Coriolis effect on Earth • As Earth rotates, different latitudes travel at different speeds • The change in speed with latitude causes the Coriolis effect

  14. North Pole Buffalo moves 783 mph Quito moves 1036 mph Buffalo 15o N equator Quito Buffalo equator 79oW Quito South Pole

  15. Current Gyres • Gyres are large circular-moving loops of water • subtropical gyres • Five main gyres (one in each ocean basin): • North Pacific • South Pacific • North Atlantic • South Atlantic • Indian • Generally 4 currents in each gyre • Centered about 30o north or south latitude

  16. Geostrophic flow and western intensification • Geostrophic flow causes a hill to form in subtropical gyres • The center of the gyre is shifted to the west because of Earth’s rotation • Western boundary currents are intensified Figure 7-7

  17. Wind-driven surface currents

  18. Global Warming

  19. The E-M Spectrum

  20. Fate of Solar Radiation Reaching the Earth reflection clouds snow and ice the earth’s surface atmospheric dust

  21. Fate of Solar Radiation Reaching the Earth absorption atmosphere oceans land plant photosynthesis

  22. Fate of Solar Radiation Reaching the Earth radiation

  23. The Greenhouse Effect

  24. Greenhouse Gases Carbon Dioxide Methane Nitrous Oxide Water Vapor Ozone

  25. Atmospheric CO2 (ppm) Temperature Change (oF) Thousands of Years Before Present

  26. Atmospheric CO2 & Surface Temperature Trends Atmospheric CO2 (ppm) Temperature Temperature Change (oF) Carbon Dioxide Year

  27. Predicted changes with increased greenhouse warming • Sea level rise • Increased plant primary productivity • Shifts in the distribution of plants and animals • Water contamination and outbreaks of water-borne diseases • Increased storm severity • Potential melting or enlargement of polar ice caps • Changes to patterns of rainfall • More severe droughts or increased precipitation • changes to ocean circulation patterns

  28. Ice Age 18,000 years ago

  29. Sea Level Changes due to Ice Ages and Ice Cap Melting

  30. Mean Sea Level Rise Changes in Mean Sea Level Year

  31. Summer Arctic Sea Ice Decline Comparison between 1979 & 2005

  32. Early Fall Arctic Sea Ice Extent Sea Ice Extent (million km2) Year

  33. Greenland Seasonal Surface Melting Surface melting

  34. Permafrost

  35. Permafrost

  36. Permafrost melting

  37. Permafrost melting

  38. Permafrost melting Drunken forest

  39. North Atlantic Tropical Storms 10-year running average Named Tropical Storms Year

  40. 1 Meter Sea Level Rise Waikiki http://www.soest.hawaii.edu/HMRG/FloodingOahu/index.php http://www.soest.hawaii.edu/coasts/sealevel/waikiki.html

  41. Sea Level Rise • Destroys coastal habitat (e.g. salt marshes, mangroves) • Destroys human property • Increases pollution • Decreases freshwater supply

  42. Effect on Marine Life • Phytoplankton bloom due to light and temperature cues • Changes will impact food web • Hypoxia may result

  43. Effect on Fisheries • Migrations are in response to temperature • May impact fisheries

  44. Effect on Corals • Coral bleaching • Leads to loss of habitat and food for reef- dependent species

  45. Currents • Oceanic conveyor belt may change ocean currents • Currents carry plankton • Bring food and oxygen • Distribute eggs and larvae • Remove wastes and pollutants

  46. Salinity • Animals have a narrow range of tolerance • Glacial melting inputs lots of freshwater

  47. Acidity • CO2 makes water acidic • Corals and other calcium carbonate species can’t make skeleton • Impact on plankton development impacts food web

  48. Temperature • Higher temperature results in less O2 • - Results in hypoxia • Ice melting leaves no resting/hunting areas for polar bears • Antarctic Krill impacts food web

  49. Invasive Species • Algae smothers coral • Invasive species out-compete natives

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