Shape and size of contrails ice particles

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Abstract
A NASA DC‐8, equipped as an in‐situ sampling aircraft, flew in the exhaust wake of a Boeing 757 on May 4, 1996 over Kansas. Ice crystal samples were collected by impaction technique and replicated twice about 8 to 17 km behind the aircraft at an altitude of 11.8 km. The ice crystals in the contrail ( after about 1 minute of growing time ) had a unimodal size distribution, with an equivalent volume radius of less than 10 µm and an effective radius of about 2 µm. The crystal habits at the observed temperature of −61C were predominantly hexagonal plates (75%), columns (20%) and few triagonal plates (<5%). The habit was already well defined for crystals about 0.5 µm in radius.

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