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Numerical comparison study of cloud microphysical parameterization schemes for a moderate snowfall event in North China

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Summary

A moderate snowfall event in North China is simulated using the high-resolution mesoscale model MM5. A fourfold-nest experiment, with a minimum horizontal grid size of 2 km, is run. In order to study the cloud microphysics processes associated with the snowfall, two experiments were conducted in two inner domains, one using the Goddard scheme (Goddard experiment), and the other using the Reisner scheme (Reisner experiment). The analysis focused on the comparison of the cloud microphysics processes which occurred in the experiments.

It is shown that there is no implicit precipitation of cumulus parameterization in the domain of grid scale 18 km. The snowfall distribution patterns in the experiments are slightly different, but the microphysical characteristics and processes may have considerable differences between the two experiments: (1) The water substances in the cloud have cloud water, cloud ice and snow, but no rainwater and graupel in the Goddard experiment. However, the water substances in the cloud have cloud ice, snow, and graupel, but no cloud water and rainwater in the Reisner experiment. (2) The cloud ice mixing ratios in the Goddard experiment are larger than those in the Reisner experiment. (3) In the Goddard experiment, the dominant cloud microphysical processes include the growth of cloud water by the condensation of supersaturated vapor, the depositional growth of cloud ice, the initiation of cloud ice, the accretion of cloud ice by snow, the accretion of cloud water by snow, the deposition growth of snow and the Bergeron process of cloud ice. In the Reisner experiment, the dominant cloud microphysical processes include the depositional growth of cloud ice, the conversion of cloud ice to snow, the deposition of snow, and the deposition growth of graupel. (4) There is only snowfall in the Goddard experiment. Meanwhile, there is ice fall, snow fall, and graupel in the Reisner experiment. But the ice fall and graupel in the Reisner experiment is very slight and can be ignored.

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Authors and Affiliations

  1. Monsoon and Environment Research Center, Department of Atmospheric Sciences, Sun Yat-sen University, Guangzhou, China

    W. S. Lin, A. Wang, S. Fan, C. Wu, J. Li & J. Meng

  2. Institute of Hydrological Sciences, National Central University, Jhongli, Taiwan

    C.-H. Sui

  3. LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China

    C. Bueh

  4. Macau Geophysical and Meteorological Observatory, Macau, China

    S. Fong

Authors
  1. W. S. Lin
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  2. C.-H. Sui
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  3. C. Bueh
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  4. A. Wang
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  5. S. Fan
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  6. C. Wu
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  7. S. Fong
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  8. J. Li
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  9. J. Meng
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Lin, W., Sui, CH., Bueh, C. et al. Numerical comparison study of cloud microphysical parameterization schemes for a moderate snowfall event in North China. Meteorol. Atmos. Phys. 95, 195–204 (2007). https://doi.org/10.1007/s00703-006-0189-4

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  • DOI: https://doi.org/10.1007/s00703-006-0189-4

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