Analytical estimation of cloud droplet nucleation based on an underlying aerosol population

被引:28
|
作者
Shipway, B. J. [1 ]
Abel, S. J. [1 ]
机构
[1] Met Off, Exeter, Devon, England
关键词
Cloud; Droplet; Aerosol; Nucleation; ICE NUCLEATION; PARAMETERIZATION; ACTIVATION; MODEL;
D O I
10.1016/j.atmosres.2009.10.005
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In this paper, we describe an analytical approach to the approximation of the nucleation rate of cloud condensation nuclei (CCN) in an updraught. This approach is developed as a subgrid parametrization for numerical models whose vertical grid structure prohibits the resolution of supersaturation and thence CCN activation. The method used is a simple extension to the upper bound approximation of Twomey (1959), and follows a similar procedure to that adopted by Cohard et al. (1998). However, unlike these approaches to the problem, we incorporate a dependence upon the physicochemical properties of an underlying dry aerosol population which is not constrained to be chosen a priori. The parametrization outlined here is also able to respond to a multimodal representation of the underlying dry aerosol spectrum. Each mode of this spectrum can further have different chemical characteristics and as such could be suitable for use in a coupled cloud-chemistry model whereby each mode of the aerosol distribution is free to evolve independently. The results of the parametrization calculated using a range of properties of the dry aerosol are validated against those from a more detailed parcel model. Crown Copyright (c) 2009 Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:344 / 355
页数:12
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