Development of aerosol activation in the double-moment Unified Model and evaluation with CLARIFY measurements

被引:11
|
作者
Gordon, Hamish [1 ,2 ]
Field, Paul R. [1 ,3 ]
Abel, Steven J. [3 ]
Barrett, Paul [3 ]
Bower, Keith [4 ]
Crawford, Ian [4 ]
Cui, Zhiqiang [1 ]
Grosvenor, Daniel P. [1 ]
Hill, Adrian A. [3 ]
Taylor, Jonathan [4 ]
Wilkinson, Jonathan [3 ]
Wu, Huihui [4 ]
Carslaw, Ken S. [1 ]
机构
[1] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England
[2] Carnegie Mellon Univ, Engn Res Accelerator, Forbes Ave, Pittsburgh, PA 15213 USA
[3] Met Off, Fitzroy Rd, Exeter EX1 3PB, Devon, England
[4] Univ Manchester, Dept Earth & Environm Sci, Manchester M13 9PL, Lancs, England
关键词
SOUTH-EAST ATLANTIC; PART I; CLOUD DROPLETS; SPECTRUM FORMATION; CONVECTIVE CLOUDS; CLIMATE MODELS; GLOMAP-MODE; MICROPHYSICS; PARAMETERIZATION; CONDENSATION;
D O I
10.5194/acp-20-10997-2020
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Representing the number and mass of cloud and aerosol particles independently in a climate, weather prediction or air quality model is important in order to simulate aerosol direct and indirect effects on radiation balance. Here we introduce the first configuration of the UK Met Office Unified Model in which both cloud and aerosol particles have "double-moment" representations with prognostic number and mass. The GLObal Model of Aerosol Processes (GLOMAP) aerosol microphysics scheme, already used in the Hadley Centre Global Environmental Model version 3 (HadGEM3) climate configuration, is coupled to the Cloud AeroSol Interacting Microphysics (CASIM) cloud microphysics scheme. We demonstrate the performance of the new configuration in high-resolution simulations of a case study defined from the CLARIFY aircraft campaign in 2017 near Ascension Island in the tropical southern Atlantic. We improve the physical basis of the activation scheme by representing the effect of existing cloud droplets on the activation of new aerosol, and we also discuss the effect of unresolved vertical velocities. We show that neglect of these two competing effects in previous studies led to compensating errors but realistic droplet concentrations. While these changes lead only to a modest improvement in model performance, they reinforce our confidence in the ability of the model microphysics code to simulate the aerosol-cloud microphysical interactions it was designed to represent. Capturing these interactions accurately is critical to simulating aerosol effects on climate.
引用
收藏
页码:10997 / 11024
页数:28
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