Aerosol Climatology

Covers climatology of atmospheric variation in size distributions, aerosol composition (except carbon), contributors to temporal/spatial variability, thermodynamics of inorganic secondary aerosol formation, and other natural aerosols including sea spray dust, and primary biological aerosol particles.

Slides and Lecture Notes

Slide Deck: link

Reading

Reading: Seinfeld and Pandis, Chapters 8 and 14.

Homework

⌨ Assignment
  1. Formation of ammonium nitrate aerosol is strongly temperature-dependent. Assume that:

  • the sulfate aerosol concentration (SO42SO_4^{2-}) is 1 ppb

  • the total nitrate (gas-phase HNO3HNO_3 plus aerosol NO3NO_3^-) is 4 ppb

  • total ammonia (gas-phase NH3NH_3 plus aerosol NH4+NH_4^+) is 7 ppb

  • the temperature is T=10CT = 10^\circ C.

Estimate the total concentration of inorganic aerosol using the approximations derived in class.

  1. Use thethermodynamic model AIM to verify your result. Assume RH=10%RH = 10\% ("Fixed relative humidity" = 0.1). The model assumed a volume of 1  m31\; m^3, so you need to convert the ppb values to mol/m3mol/m^3 and convert the output back to ppb.

  • Upload a screenshot of your model inputs and model outputs

  • On paper show the appropriate unit conversions.

  • Compare the model output to your result from 1.

CC BY-NC 4.0 Markus Petters.