1. Anthropocene Introduction to Meteorology, spring 2011 Observations –Trace gases –Temperature, land and ocean –Precipitation –Sea level Attribution Models and predictions Uncertainties

2. Human activities have changed the composition of the atmosphere since the pre- industrial era Watt’s steam engine Begin industrial period

3. Global mean surface temperatures have increased

5. = diurnal temperature range Reference Interval

7. Precipitation patterns have changed

8. Sea Levels have risen

9. Climate-induced increases in sea level are caused by thermal expansion of the oceans and melting of land ice and ice sheets

11. Atmospheric Window ~290 K Recall: 1)Molecules absorb different radiation wavelengths. 2) Black body radiation depends on temperature of object observed. 2) Wien’s law - Max wavelength (µm) ≈ 3000/T(K)

15. Svante Arrhenius (1859 -1927) Swedish 1884 PhD dissertation electro- chemistry – did not impress advisor, 150 pages, 85 theses. 1896 – Suggested that CO2 could warm the planet, from his work on ice ages. Emission of CO2 may prevent future ice ages. 1903 – Nobel prize in chemistry for work in his dissertation. Most of his theses would be unquestioned today

17. Intergovernmental panel on climate change (IPCC) Established by WMO and UNEP and confirmed by UN general assembly December 1988 Four reports issued so far 1990 human emissions are increasing atmospheric greenhouse gases, resulting increase 0.3 °C per decade 21st century. 1995 discernible human influence on global climate 2001 surface temperature projected to increase 1.4 - 5.8 C 1990 -2100, and sea level to rise by 0.1 - 0.9 meters 2007 (Nobel peace prize) Climate warming unequivocal. Most increase in global temperatures since mid-20th century is (>90%) due to increase in anthropogenic greenhouse gas concentrations. The fifth one is underway. 831 authors selected from 3000 nominations. 3-4 reviewers for each chapter.

19. Most of the observed warming in the past 50 years is attributable to human activities

21. More adverse than beneficial impacts on biological and socioeconomic systems are projected

22. Land areas are projected to warm more than the oceans with the greatest warming at high latitudes Annual mean temperature change, 2071 to 2100 relative to 1990: Global Average in 2085 = 3.1 o C

23. Some areas are projected to become wetter, others drier with an overall increase projected Annual mean precipitation change: 2071 to 2100 Relative to 1990

24. 2020s 2050s 2080s Initially increased agricultural productivity in some mid-latitude regions & reduction in the tropics and sub-tropics even with warming of a few degrees

25. Uncertainties Changes in atmospheric water vapor –Changes in cloudiness –Changes in albedo Carbon budgets Aerosol particles –Direct effects –Impact on clouds –Black carbon

26. There are fast and slow processes in the carbon cycle

27. Atmosphere Estimated Fossil Deposits 6.3 62.3 92.3 60 90 3.3 Plants Soil Oceans 750 500 2000 39,000 About 16,000 1.6 This is the “greenhouse” problem Driven by fossil fuel emissions …and land clearing The oceans and land vegetation are currently taking up 4.6 Gt C per year The KP seeks to reduce total emissions by about 0.2 Humans are perturbing the carbon cycle Units Gt C for stores & Gt C y -1 for fluxes