A climatology of midlatitude continental clouds from the ARM SGP central facility: Part I: Low-level cloud macrophysical, microphysical, and radiative properties

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Aerosol nucleation and its role for clouds and Earth's radiative forcing in the aerosol-climate model ECHAM5-HAM (2010, background): “…use the cloud droplet burden (CDB) from a long term time series (1997–2002) of low-level cloud observations at a continental site (36.6◦ N, 262.5◦ E) (Dong et al., 2005), and from a compilation of marine low-level cloud measurements at various locations (Miles et al., 2000) for evaluation of the…”
On the effect of dust particles on global cloud condensation nuclei and cloud droplet number (2011, background): “Finally, over North America, the predicted CDNC range from 201 cm−3 over Alaska (observed of 54–222 cm−3 [Dong and Mace, 2003]) to 896 cm−3 over Oklahoma (observed of 100–650 cm−3 [Dong et al., 2005, 1997, 2000; Iacobellis and Somerville, 2006]).”
Analysis of cloud layer structure in Shouxian, China using RS92 radiosonde aided by 95 GHz cloud radar (2010, background): “[24] Much research has focused on the diurnal variation of cloud layers [Wang et al., 1999;Minnis and Harrison, 1984; Blaskovic et al., 1991; Dong et al., 2006].”