Atmos. Chem. Phys., 16, 21–33, 2016 www.atmos-chem-phys.net/16/21/2016/ doi:10.5194/acp-16-21-2016 © Author(s) 2016. CC Attribution 3.0 License. Observational estimates of detrainment and entrainment in non-precipitating shallow cumulus M. S. Norgren1, J. D. Small2, H. H. Jonsson3, and P. Y. Chuang4 1Dept. of Physics, University of California Santa Cruz, Santa Cruz, CA, USA 2Dept. of Meteorology, University of Hawaii at Manoa, Honolulu, HI, USA 3Center for Interdisciplinary Remotely-Piloted Aircraft Studies, Naval Postgraduate School, Monterey, CA, USA 4Earth and Planetary Sciences, University of California Santa Cruz, Santa Cruz, CA, USA Correspondence to: P. Y. Chuang (
[email protected]) Received: 4 July 2014 – Published in Atmos. Chem. Phys. Discuss.: 26 August 2014 Revised: 27 November 2015 – Accepted: 3 December 2015 – Published: 14 January 2016 Abstract. Vertical transport associated with cumulus clouds method could be readily used with data from other previous is important to the redistribution of gases, particles, and en- aircraft campaigns to expand our understanding of detrain- ergy, with subsequent consequences for many aspects of the ment for a variety of cloud systems. climate system. Previous studies have suggested that detrain- ment from clouds can be comparable to the updraft mass flux, and thus represents an important contribution to ver- 1 Introduction tical transport. In this study, we describe a new method to deduce the amounts of gross detrainment and entrainment One of the important ways cumulus clouds affect the at- experienced by non-precipitating cumulus clouds using air- mosphere is through vertical transport. The redistribution craft observations.