Aerosol and gas-phase characteristics in relation to meteorology: Case studies in populated arid settings
[Thesis]
Ewan Colin Crosbie
Sorooshian, Armin
The University of Arizona
2015
103
Committee members: Betterton, Eric; Zeng, Xubin
Place of publication: United States, Ann Arbor; ISBN=978-1-321-81115-5
Ph.D.
Atmospheric Sciences
The University of Arizona
2015
Atmospheric aerosols and trace gases are a highly relevant component of the climate system affecting atmospheric radiative transfer and the hydrologic cycle. In arid and semi-arid regions, where cloud cover is often low and precipitation is generally scarce and sporadic, the driving processes accounting for the production, loss and transport of atmospheric constituents are often distinctly different from other climates. In arid regions, the same circulation dynamics that suppress cloud formation can be responsible for creating strong subsidence inversions, which cap atmospheric mixing and trap pollutants close to the surface, often placing populated arid regions high on global rankings of air pollution concerns. In addition, low soil moisture can encourage wind-blown dust emissions, which can be a significant fraction of the total aerosol loading in both coarse and fine modes on a mass basis.