Freud, E.; Rosenfeld, D. (2012). "Linear relation between convective cloud drop number concentration and depth for rain initiation". Journal of Geophysical Research117 (D2). pp. n/a. Bibcode:2012JGRD..117.2207F. doi:10.1029/2011JD016457.
Laufersweiler, M. J.; Shirer, H. N. (1995). "A theoretical model of multi-regime convection in a stratocumulus-topped boundary layer". Boundary-Layer Meteorology73 (4). pp. 373–409. Bibcode:1995BoLMe..73..373L. doi:10.1007/BF00712679.
Nave, R. (2013). "Adiabatic Process". gsu.edu. Consultado o 25 de setembro do 2023.
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Freud, E.; Rosenfeld, D. (2012). "Linear relation between convective cloud drop number concentration and depth for rain initiation". Journal of Geophysical Research117 (D2). pp. n/a. Bibcode:2012JGRD..117.2207F. doi:10.1029/2011JD016457.
Laufersweiler, M. J.; Shirer, H. N. (1995). "A theoretical model of multi-regime convection in a stratocumulus-topped boundary layer". Boundary-Layer Meteorology73 (4). pp. 373–409. Bibcode:1995BoLMe..73..373L. doi:10.1007/BF00712679.