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. 2015 Aug 18;120(16):8332–8344. doi: 10.1002/2014JD022785

Figure 3.

Figure 3

Sample vertical profiles of 5 m averaged cloud droplet effective radius (r e) (a) from the vertical cloud penetration used for POST research flight of 30 July 2008 21:20:30–21:24:00 UTC and (b) from the vertical cloud penetration used for POST research flight of 15 August 2008 20:33:00–20:38:00 UTC. Figure 3a is from a drizzle case, while Figure 3b has little drizzle.