Articles | Volume 18, issue 4
Atmos. Chem. Phys., 18, 2525–2546, 2018
https://doi.org/10.5194/acp-18-2525-2018
Atmos. Chem. Phys., 18, 2525–2546, 2018
https://doi.org/10.5194/acp-18-2525-2018
Research article
20 Feb 2018
Research article | 20 Feb 2018

Towards a bulk approach to local interactions of hydrometeors

Manuel Baumgartner and Peter Spichtinger

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Cited articles

Baumgartner, M. and Spichtinger, P.: Local Interactions by Diffusion between Mixed-Phase Hydrometeors: Insights from Model Simulations, Mathematics of Climate and Weather Forecasting, 3, 64–89, https://doi.org/10.1515/mcwf-2017-0004, 2017. a, b, c, d, e, f, g
Baumgartner, M. and Spichtinger, P.: Diffusional growth of cloud particles: existence and uniqueness of solutions, Theor. Comp. Fluid Dyn., 32, 47–62, https://doi.org/10.1007/s00162-017-0437-x, 2018. a
Beals, M. J., Fugal, J. P., Shaw, R. A., Lu, J., Spuler, S. M., and Stith, J. L.: Holographic measurements of inhomogeneous cloud mixing at the centimeter scale, Science, 350, 87–90, 2015. a
Bergeron, T.: The Problem of Artificial Control of Rainfall on the Globe, Tellus, 1, 32–43, 1949. a
Castellano, N. E. and Avila, E. E.: Vapour density field of a population of cloud droplets, J. Atmos. Sol.-Terr. Phy., 73, 2423–2428, 2011. a
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Short summary
Ice crystals are surrounded by liquid cloud droplets in mixed-phase clouds. The coexistence of ice and water is thermodynamically not stable and the particles will influence their respective growth by condensation. This effect is known as the Wegener–Bergeron–Findeisen process. In current models, the local interactions of the particles are neglected and they can only interact indirectly. This work proposes an approach to include local interactions and discusses some implications.
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