Modeling the Phase Transition Associated with Melting Snow in a 1D Kinematic Framework: Sensitivity to the Microphysics
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- handle: 10670/1.3mb10n
- Milbrandt, J. A.; Thériault, Julie M. et Mo, R. (2014). « Modeling the Phase Transition Associated with Melting Snow in a 1D Kinematic Framework: Sensitivity to the Microphysics ». Pure and Applied Geophysics, 171(1-2), pp. 303-322.
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http://archipel.uqam.ca/7954/
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http://dx.doi.org/10.1007/s00024-012-0552-y
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doi:10.1007/s00024-012-0552-y
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Kinematics numerical model parameterization phase transition precipitation assessment radar snowmeltCiter ce document
J. A. Milbrandt et al., « Modeling the Phase Transition Associated with Melting Snow in a 1D Kinematic Framework: Sensitivity to the Microphysics », UQAM Archipel : articles scientifiques, ID : 10670/1.3mb10n
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Résumé
A simple 1D kinematic cloud model coupled to a two-moment bulk microphysics scheme is used to perform quasi-idealized simulations of snow, with a prescribed upper boundary snow field based on observed radar reflectivity and temperature, falling into a low-level melting layer. The model realistically simulates the formation of a nearly isothermal layer below the melting level, the surface precipitation rate, and the phase transition from liquid to solid, consistent with observations for this case. A series of test runs is performed to examine the sensitivity of modeling the timing and duration of the phase transition period to details of specific parameterization aspects related to snow in the microphysics scheme. The sensitivity tests include varying the number of prognostic moments, the mass–diameter relation, the fall velocity–diameter relation, the treatment of aggregation, and the lower limit for the slope of the size distribution. It is shown that the simulated transition period, for such a case with the initial melting level being close to the surface, can be quite sensitive to model parameters specified within realistic ranges and/or ranges within our physical understanding.