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. Author manuscript; available in PMC: 2019 Dec 6.
Published in final edited form as: Atmos Chem Phys. 2018 Dec 6;18(23):17325–17354. doi: 10.5194/acp-18-17325-2018

Figure 2:

Figure 2:

Dependence of N/IWC (g−1) on the effective absorption optical depth ratio βeff as predicted from the method of Parol et al. (1991), based on PSDs from SPARTICUS synoptic cirrus (blue squares) and anvils (black squares), and TC4 aged (red diamonds) and fresh (black diamonds) anvils, where the first size-bin is included. The larger (smaller) symbols denote PSDs measured at a temperature colder (warmer) than −38°C. The curve-fit equations are for SPARTICUS synoptic cirrus (blue) and for TC4 aged and fresh anvils (red).