Global Environmental Change Section Early-Career & Mid-Career Award Lecture - II

Global Environmental Change Section Early-Career & Mid-Career Award Lecture - II

AGU via YouTube Direct link

Observations and modeling indicate polluted continental aerosols contain a fraction of INPS

22 of 37

22 of 37

Observations and modeling indicate polluted continental aerosols contain a fraction of INPS

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Global Environmental Change Section Early-Career & Mid-Career Award Lecture - II

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  1. 1 Intro
  2. 2 Small aerosols, big health impact!
  3. 3 New-particle formation (NPF) is the most important source of aerosols
  4. 4 Complicated formation chemistry of secondary organic aerosol (SOA)
  5. 5 Aerosols have potentially important but highly uncertain impact on climate
  6. 6 How to represent organic NPF in models?
  7. 7 Development of NPF schemes within regional and global models
  8. 8 The new WRF-Chem model improves particle number simulations over the Amazon
  9. 9 NPF mechanisms over the Amazon
  10. 10 Global modeling using our new E3SM model show similar results over the Amazon
  11. 11 Contribution of NPF to CCN over the Amazon
  12. 12 The new E3SM model improves simulations of particle size distribution in eastern China
  13. 13 Amine+H,SO, is the dominant NPF mechanism near the surface of eastern China
  14. 14 NPF mechanisms all over the world
  15. 15 SOA model scheme based on the 2D-VBS
  16. 16 Novel organic emission inventory (EI) covering the entire volatility range
  17. 17 The new model and inventory improve the Simulations of OA and SOA
  18. 18 IVOC is the largest source of SOA in China
  19. 19 VCPs, domestic combustion, and biomass open burning are top SOA contributors
  20. 20 Ice crystal size (R.)-aerosol relations modulated by convective strength
  21. 21 WRF-spectral-bin simulations show the key role of ice nucleating particles (INPS)
  22. 22 Observations and modeling indicate polluted continental aerosols contain a fraction of INPS
  23. 23 Response of the optical depth of different cloud types to aerosols
  24. 24 Response of deep convective precipitation to different aerosol types
  25. 25 How do we start to understand soil carbon turnover?
  26. 26 Trees, too, have the property that most of the carbon is in the oldest pools, particularly in tropical forests
  27. 27 Because most of the carbon on Earth is in the tails, we need to focus on what governs the dynamics there
  28. 28 Land carbon cycle feedbacks are a crucial and poorly quantified determinant of the Earth system response to CO, emissions
  29. 29 Isolate temperature from moisture effects by ignoring gridcells that are either too wet or too dry
  30. 30 A simple scaling theory for why temperature Sensitivity is high in cold climates
  31. 31 Vertical mixing by cryoturbation modeled as diffusive transport
  32. 32 Prajected sail Cemissions follow the retreating permafrost boundary and persist long after permafrast has thawed
  33. 33 What happens to trees if they grow taster because of elevated CO? And how sensitive is the answer to whether the causes of large-tree mortality have more to do with size versus age?
  34. 34 Basal area and aboveground biomass both Increase in response to elevated productivity but change is 50% smaller with size-driven large-tree mortality
  35. 35 10% reduction in woody biomass carbon turnover time in size- dependent mortality case
  36. 36 And observations show that mortality rates are already increasing alongside productivity in the Amazon
  37. 37 Conclusions

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