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Are We Getting Warmer?

This article explores the debate around global warming and its causes, discussing natural factors and human activities. It explains how temperature measurements are taken and factors that can affect them. The article also highlights regional temperature patterns, historical temperature proxies, and evidence for rapid temperature changes. It concludes by discussing global warming indicators and the anthropogenic nature of warming.

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Are We Getting Warmer?

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Presentation Transcript


  1. Are We Getting Warmer?

  2. Is the Earth getting warmer? • Yes • No

  3. Is change in the Earth’s climate mostly caused by natural causes or by humans? • Natural causes • Humans

  4. How do you measure a planets temperature? • If you have them, then thermometers spread around the earth can tell us the average temperature. • These record go back to the mid 19th century. • Earlier records not standardized so they have more uncertainty.

  5. What affects individual temperature measurements? • Geographic variations • Local microclimates • Land use/heat islands • Technique • Land or sea • All of the above

  6. Records must account for sea surface temperature, heat islands around cities, land use changes, measurement techniques. • Thermometers may differ in calibration. • Look for trends in temperature rather than absolute temperatures. • Usually want to determine anomalies rather than absolute values. • Anomalies are deviations from average temperature.

  7. Regional Patterns • Warming is greater on land than in oceans (specific heat) • Warming is larger in northern hemisphere (more land and more GHG) • Arctic has warmed at twice the global rate • Ice-albedo feedback, • lower evaporation; more energy directly to the surface

  8. Regional Temperature Anomlies

  9. Zonal Mean Temperature Anomolies

  10. Is the temperature rise unusual? • Before 1850 we have very little direct thermometric data so we use “proxies” for measuring the temperature from long ago. • Examples: tree rings, lake sediments, bleaching of coral reefs, isotope ratios

  11. Temperature for 1000 years.

  12. Greenland Ice Cores

  13. CO2 and Temperature are strongly correlated. • Probably not cause and effect.

  14. Correlation • Chronological relationship between two factors • Expressed as a number between -1 and 1 • Does not prove causal relationship • Rising of Sirius  flooding of the Nile • Coming to physics class  falling asleep

  15. CO2 and Temperature are strongly correlated. • Probably not cause and effect. • Small chances in temperature are caused by small orbital changes. • Small increase in sea surface temperature causes some CO2 to come out of solution. • Increase in land surface temperature increases microbial action  more CO2 • More CO2 in the air cause further warming.

  16. Using Isotope ratios we can go back millions to billions of years to find temperatures. • 16O vs. 18O • 1H vs. 2H • Compare ratios in different layers of ice. • Arctic yields clearer results.

  17. Evidence for Rapid Temperature Changes in Greenland Ice Core

  18. Younger Dryas • The Big Freeze • Approximately 15,000 years ago; 1300 year duration • Caused by collapse of North American ice sheets(?) • Believed to be nonlinear effects due to changes in ocean circulation when there was a large influx of fresh water from glacial melting

  19. Ocean Currents

  20. Caution: The rapid fluctuation in the Younger Dryas are Arctic temperatures which exaggerate global climate changes. • Fluctuation not so obvious in proxies from other regions of the world. • The rapid changes that we are experiencing now are global. They are also more exaggerated in the polar regions.

  21. Reduction in Sea Ice1979-2005

  22. Decline in Sea Ice

  23. Not only is there less area of sea ice, it is also thinner.

  24. Melting Glaciers

  25. Global Warming Indicators • Global temperature • Ice sheets (Greenland, Antarctic) • Arctic sea ice • Glaciers • Ocean surface temperature • Sea level

  26. Is the Warming Anthropogenic?

  27. Chicago Tribune 31 March 2006

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