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Milankovic climate-dalj-pandzic-2009

doxikus
15 de Apr de 2010
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Milankovic climate-dalj-pandzic-2009

  1. Climate Changes and Impacts: Possible Scenario up to 2100 Krešo Pandžić Meteorological and Hydrological Service, CROATIA
  2. Content 1 Climate and climate system 2 Paleoclimate 3 Recent global warming 4 Precipitation amount trend 5 Snow and ice cover 6 Processes in the oceans 7 Climate extreme 8 Global climate scenario 9 Conclusion
  3.  
  4. Lithosphere and Biosphere Hydrosphere
  5. CRIOSPHERE
  6. GREENHOUSE EFFECT
  7. - Carbon Dioxide (CO 2 ) - the burning of the fossil fuels - Kyoto Protocol - UN Climate Convention - EU Directives - IPCC Recommendations
  8. RADIATIVE FORCING
  9. 2. Paleoclimate
  10. Earth's Orbital Changes
  11. Paleoclimate cycles
  12. The Last Interglacial and the Arctic
  13. The Last 1000 Years
  14. 3. Recent Global Warming
  15. Recent Global Warming
  16.  
  17.  
  18.  
  19. 3. Precipitation Amount Trend
  20.  
  21.  
  22. Palmer’s Drought Severity Index
  23. 5. Snow and Ice Cover
  24. March-April NH Snow Covering Area
  25. CHANGE IN SEA ICE EXTENT Arctic Antarctic
  26. ARCTIC Summer 1983 Summer 2003
  27. 6. Processes in the Oceans
  28. PROCESSES IN THE OCEAN
  29. Global sea surface anomalies - El Nino
  30.  
  31. 7. Climate Extremes
  32. Cold Extreme Decrease
  33. Warm Extreme Increase
  34. Extreme Hot Summer 2003 in Central Europe
  35. Extreme Warm Summer 2003 in Croatia
  36. Extreme Warm Winter 2006/2007 in Croatia
  37. Number of Very Wet Day Increase
  38. Sahel Recent Drought
  39.  
  40. 8. Global Climate Scenario
  41. Comprehensive Climate Models
  42. CO 2 Temperature
  43. GLOBAL WARMING PROJECTION
  44. Decade Temperature Projection
  45. REGIONAL TEMPERATURE PRPJECTION
  46. European Temperature Projection
  47. EUROPEAN PRECIPITATION PROJECTION
  48. Frost Days Heat Waves Growing Season
  49.  
  50. Precipitation Intensity Dry Days
  51. MORE HOT WEATHER
  52. Sea Level Rise
  53. Sea Level Rise
  54. CO 2 Concentration Scenarios
  55. 8. Conclusion - Climate has been changed in the past in long time-scale (1000 years) - Recent global warming on a very short i.e. decade scale (10 to 100 years) - very probably (90 %) caused by man - some measure to limit CO 2 emission - Kyoto Protocol, UN Climate Convention, - IPCC - Political decisions are very important - Role of National Meteorological Service - Agencies for Environmental Protection - education of young people
  56. THANK YOU
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