Buoyancy reversal and cloud‐top entrainment instability

In 1980, Randall suggested that cloud top entrainment instability, a runaway positive feedback between mixing, evaporative cooling and entrainment, may cause the transition from the subtropical stratocumulus layers, frequently observed over the cold water of the eastern oceans, to tradewind cumulus....

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Veröffentlicht in:	Quarterly journal of the Royal Meteorological Society 1990-04, Vol.116 (493), p.705-739
Hauptverfasser:	Siems, Steven T., Bretherton, Christopher S., Baker, Marcia B., Shy, Shenqyang, Breidenthal, Robert E.
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth, ocean, space Exact sciences and technology External geophysics Meteorology Other topics in atmospheric geophysics
Online-Zugang:	Volltext
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