Overview

This page is part of the Bulk Cloud Model (BCM) documentation.
It contains a listing of the references.
For an overview of all BCM-related pages, see the Bulk Cloud Model main page.

References

• Arnason G, Brown J. 1971. Growth of cloud droplets by condensation: A problem in computational stability. J. Atmos. Sci. 28: 72-77.

• Emanuel KA. 1994. Atmospheric Convection. Oxford University Press.

• Seifert A, Beheng KD. 2001. A double-moment parameterization for simulating autoconversion, accretion and selfcollection. Atmos. Res. 59: 265–281.

• Seifert A, Beheng KD. 2006. A two-moment cloud microphysics parameterization for mixed-phase clouds. Part 1: Model description. Meteorol. Atmos. Phys. 92: 45–66.

• Savic-Jovcic V, Stevens B. 2008. The structure and mesoscale organization of precipitating stratocumulus. J. Atmos. Sci. 65: 1587–1605. ​doi

• Heus T, van Heerwaarden CC, Jonker HJJ, Pier Siebesma A, Axelsen S, van den Dries K, Geoffroy O, Moene AF, Pino D, de Roode SR, Vilà-Guerau de Arellano J. 2010. Formulation of the Dutch Atmospheric Large-Eddy Simulation (DALES) and overview of its applications. Geosci. Model Dev. 3: 415–444. ​doi

• Stevens B, Seifert A. 2008. Understanding macrophysical outcomes of microphysical choices in simulations of shallow cumulus convection. J. Meteor. Soc. Jpn. 86: 143–162.

• Bougeault, P. 1981. Modeling the trade-wind cumulus boundary layer. Part I: Testing the ensemble cloud relations against numerical data. J. Atmos. Sci. 38: 2414–2428.

• Khairoutdinov M, Kogan Y. 2000. A new cloud physics parameterization in a large-eddy simulation model of marine stratocumulus. Mon. Weat. Rev. 128: 229–243.

• Sommeria G, Deardorff JW. 1977. Subgrid-scale condensation in models of nonprecipitating clouds. J. Atmos. Sci. 34: 344–355.

• Kessler E. 1969. On the Distribution and Continuity of Water Substance in Atmospheric Circulation. Meteor. Monogr: 1-84.

• Pruppacher HR, and Klett JD. 1997. Microphysics of Clouds and Precipitation. 2nd Edn. Kluwer Academic Publishers. Dordrecht.

• Morrison H. 2007. Comparison of bulk and bin warm-rain microphysics models using a kinematic framework. J. Atmos. Sci. 64: 2839-2681.

• Seifert A, Nuijens L, Stevens B. 2010. Turbulence effects on warm-rain autoconversion in precipitating shallow convection. Q. J. Roy. Meteor. Soc. 136: 1753–1762.

• Seifert A. 2008. On the parameterization of evaporation of raindrops as simulated by a one-dimensional rainshaft model. J. Atmos. Sci. 65: 3608–3619. ​doi.

• Ackerman, AS, vanZanten MC, Stevens B, Savic-Jovcic V, Bretherton CS, Chlond A, Golaz J-C, Jiang H, Khairoutdinov M, Krueger SK, Lewellen DC, Lock A, Moeng C-H, Nakamura K, Petters MD, Snider JR, Weinbrecht S, Zuluaf M. 2009. Large-eddy simulations of a drizzling, stratocumulus-topped marine boundary layer, Mon. Weather Rev., 137: 1083–1110.

• Geoffroy O, Brenguier J-L, Burnet F. 2010. Parametric representation of the cloud droplet spectra for LES warm bulk microphysical schemes. Atmos. Chem. Phys. 10: 4835–4848. ​doi.

• Rogers RR, Baumgardner D, Ethier SA, Carter DA, Ecklund WL. 1993. Comparison of raindrop size distributions measured by radar wind profiler and by airplane. J. Appl. Meteorol. 32: 694–699.

• Cuijpers JWM, Duynkerke PG. 1993. Large eddy simulation of trade wind cumulus clouds. J. Atmos. Sci. 50: 3894–3908.

• Khvorostyanov V, Curry J. 2006. Aerosol size spectra and CCN activity spectra: Reconciling the lognormal, algebraic, and power laws. J. Geophys. Res. 111.

• Dipankar A, Stevens B, Heinze R, Moseley C, Zängl G, Giorgetta M, Brdar D. 2015. Large eddy simulation using the general circulation model ICON. J. Adv. Mod. Earth Syst. 07. ​doi.

• Gronemeier T, Kanani-Sühring F, Raasch S. 2016. Do shallow cumulus clouds have the potential to trigger secondary circulations via shading? Boundary-Layer Meteorol. ​doi.

References for Input Parameter

Ackerman, A. et al (2009): Large-Eddy Simulations of a Drizzling, Stratocumulus-Topped Marine Boundary Layer, Monthly Weather Review, 137, 1083-1110, ​https://doi.org/10.1175/2008MWR2582.1.

Kessler, E.(1969): On the continuity and distribution of water substance in atmospheric circulations, Atmospheric Research, 38, 109-145, ​https://doi.org/10.1007/978-1-935704-36-2_1.

Khairoutdinov, M. and Kogan, Y. (2000): A New Cloud Physics Parameterization in a Large-Eddy Simulation Model of Marine Stratocumulus, Monthly Weather Review, 128, 229, ​https://doi.org/10.1175/1520-0493(2000)128<0229:ANCPPI>2.0.CO;2.

Khvorostyanov, V. I. and Curry, J. A. (2006): Aerosol size spectra and CCN activity spectra: Reconciling the lognormal, algebraic, and power laws. J. Geophys. Res., 111, D12, ​https://doi.org/10.1029/2005JD006532.

Morriion, H. and Grabowski, W. W. (2007): Comparison of Bulk and Bin Warm-Rain Microphysics Models Using a Kinematic Framework, Journal of the Atmosheric Sciences, 64, 2839, ​https://doi.org/10.1175/JAS3980.

Seifert, A. and Beheng, K. (2006): A two-moment cloud microphysics parameterization for mixed-phase clouds. Part 1: Model description, Meteorol. Atmos. Phys., 92, 45-66, ​https://doi.org/10.1007/s00703-005-0112-4.

Seifert, A. (2008): On the Parameterization of Evaporation of Raindrops as Simulated by a One-Dimensional Rainshaft Model, Journal of the Atmospheric Sciences, 65, 3608-3619, ​https://doi.org/10.1175/2008JAS2586.1.

Seifert, A., Nuijens, L., Stevens, B. (2010): Turbulence effects on warm‐rain autoconversion in precipitating shallow convection, Quarterly Journal of the Royal Meteorological Society, 136, 1753-1762, ​https://doi.org/10.1002/qj.684.

Stevens, B. and Seifert, A. (2008): Understanding macrophysical outcomes of microphysical choices in simulations of shallow cumulus convection, 86A, 143-162, ​https://doi.org/10.2151/jmsj.86A.143.