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Sökning: id:"swepub:oai:DiVA.org:kth-246566" > Effect of turbulenc...

Effect of turbulence on collisional growth of cloud droplets

Li, Xiang-Yung (författare)
KTH,Nordic Institute for Theoretical Physics NORDITA
Brandenburg, Axel (författare)
Stockholms universitet,KTH,Nordic Institute for Theoretical Physics NORDITA,Nordiska institutet för teoretisk fysik (Nordita),Institutionen för astronomi,University of Colorado, USA
Svensson, Gunilla (författare)
Stockholms universitet,Meteorologiska institutionen (MISU),Swedish e-Science Research Centre, Sweden; Global & Climate Dynamics, National Center for Atmospheric Research, USA
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Haugen, N. E. L. (författare)
Mehlig, B. (författare)
Rogachevskii, lgor (författare)
KTH,Nordic Institute for Theoretical Physics NORDITA
Li, Xiang-Yu (författare)
Stockholms universitet,Meteorologiska institutionen (MISU),Nordiska institutet för teoretisk fysik (Nordita),Swedish e-Science Research Centre, Sweden; University of Colorado, USA
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 (creator_code:org_t)
American Meteorological Society, 2018
2018
Engelska.
Ingår i: Journal of the Atmospheric Sciences. - : American Meteorological Society. - 0022-4928 .- 1520-0469. ; 75:10, s. 3469-3487
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Weinvestigate the effect of turbulence on the collisional growth of micrometer-sized droplets through highresolution numerical simulations with well-resolved Kolmogorov scales, assuming a collision and coalescence efficiency of unity. The droplet dynamics and collisions are approximated using a superparticle approach. In the absence of gravity, we show that the time evolution of the shape of the droplet-size distribution due to turbulence-induced collisions depends strongly on the turbulent energy-dissipation rate ε, but only weakly on the Reynolds number. This can be explained through the « dependence of the mean collision rate described by the Saffman-Turner collision model. Consistent with the Saffman-Turner collision model and its extensions, the collision rate increases as ε1/2 even when coalescence is invoked. The size distribution exhibits power-law behavior with a slope of 23.7 from a maximum at approximately 10 up to about 40 mm. When gravity is invoked, turbulence is found to dominate the time evolution of an initially monodisperse droplet distribution at early times. At later times, however, gravity takes over and dominates the collisional growth. We find that the formation of large droplets is very sensitive to the turbulent energy dissipation rate. This is because turbulence enhances the collisional growth between similar-sized droplets at the early stage of raindrop formation. The mean collision rate grows exponentially, which is consistent with the theoretical prediction of the continuous collisional growth even when turbulence-generated collisions are invoked. This consistency only reflects the mean effect of turbulence on collisional growth. 

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)

Nyckelord

Clouds
Turbulence
Coalescence
Drops
Energy dissipation
Reynolds number
Size distribution
Collision and coalescence
Droplet dynamics
Droplet size distributions
High-resolution numerical simulation
Kolmogorov scale
Monodisperse droplets
Power-law behavior
Turbulent energy dissipation rate
cloud droplet
cloud microphysics
computer simulation
numerical model
power law
atmosfärvetenskap och oceanografi

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