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Volume 16, issue 10
Atmos. Chem. Phys., 16, 6563–6576, 2016
https://doi.org/10.5194/acp-16-6563-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: VERDI – Vertical ​Distribution of Ice ​in Arctic Clouds...

Atmos. Chem. Phys., 16, 6563–6576, 2016
https://doi.org/10.5194/acp-16-6563-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 30 May 2016

Research article | 30 May 2016

Long-resident droplets at the stratocumulus top

Alberto de Lozar and Lukas Muessle Alberto de Lozar and Lukas Muessle
  • Max Planck Institute for Meteorology, Bundestr. 53, 20146 Hamburg, Germany

Abstract. Turbulence models predict low droplet-collision rates in stratocumulus clouds, which should imply a narrow droplet size distribution and little rain. Contrary to this expectation, rain is often observed in stratocumuli. In this paper, we explore the hypothesis that some droplets can grow well above the average because small-scale turbulence allows them to reside at cloud top for a time longer than the convective-eddy time t*. Long-resident droplets can grow larger because condensation due to longwave radiative cooling, and collisions have more time to enhance droplet growth. We investigate the trajectories of 1 billion Lagrangian droplets in direct numerical simulations of a cloudy mixed-layer configuration that is based on observations from the flight 11 from the VERDI campaign. High resolution is employed to represent a well-developed turbulent state at cloud top. Only one-way coupling is considered. We observe that 70 % of the droplets spend less than 0.6t* at cloud top before leaving the cloud, while 15 % of the droplets remain at least 0.9t* at cloud top. In addition, 0.2 % of the droplets spend more than 2.5t* at cloud top and decouple from the large-scale convective eddies that brought them to the top, with the result that they become memoryless. Modeling collisions like a Poisson process leads to the conclusion that most rain droplets originate from those memoryless droplets. Furthermore, most long-resident droplets accumulate at the downdraft regions of the flow, which could be related to the closed-cell stratocumulus pattern. Finally, we see that condensation due to longwave radiative cooling considerably broadens the cloud-top droplet size distribution: 6.5 % of the droplets double their mass due to radiation in their time at cloud top. This simulated droplet size distribution matches the flight measurements, confirming that condensation due to longwave radiation can be an important mechanism for broadening the droplet size distribution in radiatively driven stratocumuli.

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We follow 1 billion cloud droplets in numerical simulations, which are based on observations of Arctic stratocumuli from the VERDI campaign. Small-scale turbulence allows some droplets to escape the large-scale convective movements, with the result that they can spend a long time at cloud top. Long-resident droplets can grow well above the average due to radiative cooling and collisions. This can have consequences for rain models that assume that all droplets spend the same time in the cloud.
We follow 1 billion cloud droplets in numerical simulations, which are based on observations of...
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