Aerosol Properties and Processes: A Path from Field and Laboratory Measurements to Global Climate Models

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Toward a Minimal Representation of Aerosols in Climate Models: Comparative Decomposition of Aerosol Direct, Semidirect, and Indirect Radiative Forcing (2012, background): “Many choices about the representation of each of these processes must be made (Ghan and Schwartz 2007), and those choices should be consistent with the representation of the aerosol.”
The magnitude and causes of uncertainty in global model simulations of cloud condensation nuclei (2013, background): “…this development in model sophistication should improve model fidelity, but the increased complexity has led to an increase in the number of uncertain model parameters, many of which have very weak observational constraints and an incomplete scientific understanding (Ghan and Schwartz, 2007).”
Bounding Global Aerosol Radiative Forcing of Climate Change (2020, methodology): “…trajectory of the climate system, involving field measurements, laboratory studies, and150 modeling from microphysical to global scales (e.g. S. J. Ghan & Schwartz, 2007; Kul-151 mala et al., 2011; Seinfeld et al., 2016).152 –3– [INSERT TABLE 1 HERE]153 In spring 2018, under the auspices of the…”
Understanding atmospheric organic aerosols via factor analysis of aerosol mass spectrometry: a review (2011, unknown): “, indirect climate forcing effect) [1, 2].”