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Summerschool Schedule and Introduction to the Assignments

Join the 5th Earth System Modelling School in Hamburg for lectures, hands-on experiments, and discussions. Explore student experiments on atmosphere, ocean, and land dynamics, utilizing the IBM Power 6 supercomputer. Analyze experiment results and participate in roundtable discussions on climate conflicts and history.

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Summerschool Schedule and Introduction to the Assignments

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  1. 5th Earth System Modelling School Hamburg 2011 Summerschool Schedule and Introduction to the Assignments Christian Reick Max Planck Institute for Meteorology Hamburg

  2. Ocean biogeochemistry SCHEDULE Atmosphere Ocean Land Lectures Hands-on Good bye Buffet & drinks Informal get-together at Geo Evening lectures Climate conflicts Climate history

  3. STUDENT EXPERIMENTS IBM Power 6 supercomputer at German Climate Computing Center (DKRZ) Student Experiments Precomputed Control Experiment • Cloud top mass flux • Soil respiration • Ocean mixing • Ocean albedo • Flat earth (100 years)

  4. SCHEDULE Analysis Of Experiments Lectures Student Presen- tations Submit experiments Hands-on Good bye Buffet & drinks Informal get-together at Geo Evening lectures Climate conflicts Climate history

  5. An Example from ISSMES‘07 Reduction of Solar constant: 1367W/m2 1000 W/m2 What are the consequences for the Earth System?

  6. An Example from ISSMES‘07 Global air temperature 8 [°C] 4 0 - 4 800 810 820 year

  7. An Example from ISSMES‘07 Sea surface temperature [°C] 15.0 12.5 10.0 7.5 800 810 820 year

  8. An Example from ISSMES‘07 Sea ice volume [1012 m3] Northern Hemisphere Southern Hemisphere

  9. An Example from ISSMES‘07 Change in SST: year 800  807 [°C] 800 807 Sea ice border

  10. An Example from ISSMES‘07 North Atlantic deep water flux control

  11. An Example from ISSMES‘07 360 340 320 300 280 Atmospheric CO2 concentration [ppm]

  12. An Example from ISSMES‘07 Global Net Primary Productivity [mol(C)/m2 month] [mol(C)/m2 month] control year

  13. An Example from ISSMES‘07 Change in living vegetation carbon: year 800  820 [mol(C)/m2]

  14. An Example from ISSMES‘07  Temperature drop  destabilization of ocean stratification  change in ocean circulation  change in ocean heat distribution  change in sea ice extent  Temperature drop  death of northern vegetation  reduced plant CO2-uptake  increasing atmospheric CO2  increased growth of tropical vegetation Conclusion Solar input response of physical system response of biogeochemical system

  15. SCHEDULE Lectures presentation of results Hands-on collection of hypotheses roundtable discussion discussion of hypotheses Good bye Buffet & drinks Informal get-together at Geo Evening lectures Climate conflicts Climate history

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