Changes between Version 8 and Version 9 of doc/tec/lcm


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Timestamp:
Jun 27, 2016 8:52:08 PM (9 years ago)
Author:
Giersch
Comment:

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  • doc/tec/lcm

    v8 v9  
    128128== Recent applications ==
    129129
     130The LCM was validated against traditional bulk models for the BOMEX (The Barbados Oceanographic and Meteorological EXperiment) experiment (see [#siebesma2003 Siebesma et al., 2003]) by [#riechelmann2012 Riechelmann et al. (2012)]. [#riechelmann2012 Riechelmann et al. (2012)] and [#lee2014 Lee et al. (2014)] used the LCM for studying turbulence and droplet dynamics in convective clouds; [#hoffmann2015a Hoffmann et al. (2015)] investigated cloud droplet activation. Figure 10 shows the spatial distribution of simulated droplets and their respective radius within a simulated cumulus cloud. It appears that the largest drops (in terms of radius) are located at the top and the edges of the cloud, whereas smaller droplets tend to be located at the cloud base.
     131
    130132== References ==
    131133
     
    149151
    150152* [=#ayala2008] '''Ayala O, Rosa B, Wang L-P.''' 2008. Effects of turbulence on the geometric collision rate of sedimenting droplets. Part 2. Theory and parameterization. New J. Phys. 10: 075016. [http://dx.doi.org/10.1088/1367-2630/10/7/075016 doi]
     153
     154* [=#siebesma2003] '''Siebesma AP, Bretherton CS, Brown A, Chlond A, Cuxart J, Duynkerke PG, Jiang H, Khairoutdinov M, Lewellen D, Moeng C-H, Sanchez E, Stevens B, Stevens, DE.''' 2003. A large eddy simulation intercomparison study of shallow cumulus convection. J.~Atmos.~Sci. 60: 1201–1219.
     155
     156* [=#riechelmann2012] '''Riechelmann T, Noh Y, Raasch S.''' 2012. A new method for large-eddy simulations of clouds with Lagrangian droplets including the effects of turbulent collision. New J. Phys. 14: 065008. [http://dx.doi.org/10.1088/1367-2630/14/6/065008 doi]
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     158* [=#lee2014] '''Lee JH, Noh Y, Raasch S, Riechelmann T, Wang L-P.''' 2014. Investigation of droplet dynamics in a convective cloud using a Lagrangian cloud model. Meteorol. Atmos. Phys. 124: 1–21. [http://dx.doi.org/10.1007/s00703-014-0311-y doi]
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