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Communicating (Paleo)climate Science

Communicating (Paleo)climate Science. Kim Cobb EAS, Georgia Inst. of Technology Acknowledgements Lab members: Intan Suci Nurhati Julien Emile-Geay Laura Zaunbrecher James Herrin Hussein Sayani EAS undergrads. with special thanks to: Norwegian Cruise Lines Palmyra Research Consortium

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Communicating (Paleo)climate Science

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  1. Communicating (Paleo)climate Science Kim Cobb EAS, Georgia Inst. of Technology Acknowledgements Lab members: Intan Suci Nurhati Julien Emile-Geay Laura Zaunbrecher James Herrin Hussein Sayani EAS undergrads with special thanks to: Norwegian Cruise Lines Palmyra Research Consortium Sarawak Department of Forestry, Malaysia NOAA, NSF

  2. Which of the following are scientific statements? • Reducing CO2 emissions would hurt the economy. • 2) Improved technology is the best way to slow global • warming. • 3) A warming of 1ºC over the next 50yrs is “dangerous”. • 4) Global temperatures were 5ºC colder during the Last • Glacial Maximum. • 5) Hurricane Katrina was caused by global warming.

  3. Which of the following are scientific statements? • Reducing CO2 emissions would hurt the economy. • 2) Improved technology is the best way to slow global • warming. • 3) A warming of 1ºC over the next 50yrs is “dangerous”. • 4) Global temperatures were 5ºC colder during the Last • Glacial Maximum. • 5) Hurricane Katrina was caused by global warming.

  4. Why do 99.999% of climate scientists believe that CO2 is warming the planet? • Theory predicts that increasing atmospheric CO2 should warm the planet. • Geologic evidence links CO2 and temperature in the past. • The warming is unprecedented in the most recent centuries (dwarfs natural variability). • 4. Climate models show that rising CO2 is necessary to simulate • 20th century temperature trends (solar and volcanic minor players).

  5. Ice core climate and CO2 records tiny gas bubbles in the ice trap ancient air samples

  6. #2 Atmospheric CO2 and temperature over the past 650 thousand years CO2 and temperature are closely linked on geologic timescales

  7. To understand how climate has changed in the past, we need to use records of climate preserved in ice cores, ancient tree rings, coral bands, and other “paleoclimatic” sources: key is to CALIBRATE to temperature records

  8. #3 The “Hockey Stick” Key Points: error bars increase as you go back in time natural variability accounts for <0.5ºC over the last millennium late 20th century temperature trend is unprecedentedin 1,000 years

  9. #4 anthropogenic only Solar and volcanic only Intergovernmental Panel on Climate Change (IPCC) 2001 natural & anthropogenic

  10. The uncertain climate future Range of scenarios: Strict international agreements  CO2 at 600ppm by 2100 *390ppm today Mid-ground  850ppm by 2100 280ppm 1800 Business as usual  1200ppm by 2100 IPCC AR4, 2007

  11. but we need to know about regional climate changes, and specifically about regional precipitation changes white = models disagree color = models mostly agree stippled = models agree IPCC AR4, 2007

  12. Research Goal:constrain tropical Pacific response to anthropogenic global warming Approach: reconstruct tropical Pacific climate at high-resolution for the last millennium El Niño Temperature WHY? “El Niño-Southern Oscillation” (ENSO) ENSO is a climate pattern in the tropical Pacific which arises from coupled interactions between the atmosphere and ocean ENSO impacts global climate every 2-7 years (huge impact on rainfall) El Niño Precipitation Dai and Wigley, 2000

  13. Research Questions How has the tropical Pacific climate system responded to CO2 forcing? What aspects of present tropical Pacific climate are unprecedented? compare last several decades to recent centuries Palmyra 1997-? Fanning 2005-? Christmas 1998-?

  14. Corals: The geologic record of El Niño Living Porites corals provide records for the last 200 years CORALS from the tropical Pacific record El Niño’s in the geochemistry of their skeletons Fossil Porites corals enable us to extend the record back many centuries

  15. Palmyra coral oxygen isotopes vs. tropical Pacific SST

  16. Overlapping fossil corals: ancient El Niño events Good reproducibility between coral geochemical records increases confidence in coral climate reconstructions.

  17. A millennium-long reconstruction of tropical Pacific temperature Key climate observations: 1) late 20th century warming is unprecedented in the last millennium 2) no cooling during the Northern Hemisphere’s “Little Ice Age” 3) significant cooling implied during the NH’s “Medieval Warm Period”

  18. THIS IS THE END OF MY SCIENCE PRESENTATION

  19. Reflections of a (Paleo)climatologist

  20. Paleoclimate data have strong visual, intuitive appeal. Their dismissal by a large fraction of the climate science community hasn’t helped cement their contributions, nor utilize their full potential. But this is changing …

  21. The Pyramid of Climate Consensus Is anthropogenic CO2 warming the planet? yes or no?

  22. The Pyramid of Climate Consensus What are the impacts of AGW? (what? how much? by when?) Is anthropogenic CO2 warming the planet? yes or no?

  23. The Pyramid of Climate Consensus What should be done about it? What are the impacts of AGW? (what? how much? by when?) Is anthropogenic CO2 warming the planet? yes or no?

  24. How climate scientists can help • Appreciate the differences between climate science and • climate policy. climate scientist policy advocate ??

  25. How climate scientists can help • Appreciate the differences between climate science and • climate policy. • Denounce sloppy science from both extremes of the • climate science debate. (climate skeptics, IPCC WG2) climate scientist policy advocate ??

  26. How climate scientists can help • Appreciate the differences between climate science and • climate policy. • Denounce sloppy science from both extremes of the • climate science debate. (climate skeptics, IPCC WG2) • Publish data in data repositories with new standards for • climate metadata. climate scientist policy advocate ??

  27. How climate scientists can help • Appreciate the differences between climate science and • climate policy. • Denounce sloppy science from both extremes of the • climate science debate. (climate skeptics, IPCC WG2) • Publish data in data repositories with new standards for • climate metadata. • 4) Engage public, policymakers, skeptics in science of climate • change, with the pyramid of consensus always in mind. climate scientist policy advocate ??

  28. How climate scientists can help • Appreciate the differences between climate science and • climate policy. • Denounce sloppy science from both extremes of the • climate science debate. (climate skeptics, IPCC WG2) • Publish data in data repositories with new standards for • climate metadata. • 4) Engage public, policymakers, skeptics in science of climate • change, with the pyramid of consensus always in mind. • 5) Remove existing structural impediments to outreach, consider • creating new structures to aid outreach. (Beyond RC?) climate scientist policy advocate ??

  29. Some thoughts on the IPCC from Judy Curry As the IPCC turns 22, needs to address the question: “What do I want to be when I grow up?”

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