Crisp, Stephen

See Stephen Crisp (trans. and ed.), Abraham von Franckenberg A Warning against the Deceit of setting up Man s Reason as Judge in Spiritual Matters (1646) (London 1677), 3-7. 

Wiscombe and Welch, 1986). Cloud absorption is related to droplet size in a complex way (Stephens and Tsay, 1990) so that errors in droplet size measurements can alter the model-predicted absorption by a cloud. The treatment of absorption due to water vapor is another possibility. As discussed by Crisp (1997), the treatment of water vapor in models is simplified and may not properly reflect, for example, continuum absorptions between major bands in the near-IR. Model calculations suggest that the presence of a thin, saturated layer of water vapor above the clouds, for example, leads to increased absorption by 2-6% (Davies et al., 1984 Podgorny et al., 1998). However, the Crisp calculations indicate that this cannot account for all of the observed excess absorption. 

---