Abstract
In this chapter, interaction between water and ice clouds is examined through the analysis of tendency of a cloud ratio. The cloud ratio is defined as the ratio of ice water path to liquid water path. The tendency equation of the cloud ratio is derived from prognostic equations of mixing ratios of five cloud hydrometeors. The tendency of the cloud ratio is associated with conversion between the ice and liquid water paths, condensation and depositions, the evaporation of raindrops and rainfall. The cloud ratio is also used to develop a new rainfall separation method for studying structures of precipitation systems. The new rainfall partitioning method is compared to previous separation technique with the magnitude of rain rate through the analysis of cloud microphysical budgets associated with convective and stratiform rainfall.
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References
Churchill DD, Houze RA Jr (1984) Development and structure of winter monsoon cloud clusters on 10 December 1978. J Atmos Sci 41:933–960
Cui X, Zhu Y, Li X (2007) Cloud microphysical properties in tropical convective and stratiform regions. Meteorol Atmos Phys 98:1–11
Houze RA Jr (1973) A climatological study of vertical transports by cumulus-scale convection. J Atmos Sci 30:1112–1123
Houze RA Jr (1997) Stratiform precipitation in region of convection: a meteorological paradox? Bull Am Meteorol Soc 78:2179–2196
Lang S, Tao WK, Simpson J, Ferrier B (2003) Modeling of convective-stratiform precipitation processes: sensitivity to partition methods. J Appl Meteorol 42:505–527
Li X, Sui CH, Lau KM (2002) Dominant cloud microphysical processes in a tropical oceanic convective system: a 2-D cloud resolving modeling study. Mon Weather Rev 130:2481–2491
Steiner M, Houze RA Jr (1993) Three-dimensional validation at TRMM ground truth sites: some early results from Darwin, Australia. In: 26th International conference on radar meteorology, Norman, OK, American Meteorological Society, 417–420
Steiner M, Houze RA Jr, Yuter SE (1995) Climatological characterization of three-dimensional storm structure from operational radar and rain gauge data. J Appl Meteorol 34:1978–2007
Sui CH, Li X (2005) A tendency of cloud ratio associated with the development of tropical water and ice clouds. Terr Atmos Ocean Sci 16:419–434, (c) Chinese Geoscience Union. Reprinted with permission
Sui CH, Lau KM, Tao WK, Simpson J (1994) The tropical water and energy cycles in a cumulus ensemble model. Part I: equilibrium climate. J Atmos Sci 51:711–728
Sui CH, Tsay CT, Li X (2007) Convective-stratiform rainfall separation by cloud content. J Geophys Res. doi:10.1029/2006JD008082, (c) American Geophysical Union. Reprinted with permission
Tao WK, Simpson J, Sui CH, Ferrier B, Lang S, Scala J, Chou MD, Pickering K (1993) Heating, moisture, and water budgets of tropical and midlatitude squall lines: comparisons and sensitivity to longwave radiation. J Atmos Sci 50:673–690
Xu KM (1995) Partitioning mass, heat, and moisture budgets of explicit simulated cumulus ensembles into convective and stratiform components. J Atmos Sci 52:1–23
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Li, X., Gao, S. (2016). Structures of Precipitation Systems I: Cloud-Content Analysis. In: Cloud-Resolving Modeling of Convective Processes. Springer Atmospheric Sciences. Springer, Cham. https://doi.org/10.1007/978-3-319-26360-1_5
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DOI: https://doi.org/10.1007/978-3-319-26360-1_5
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