4.7 Article

Characteristics of raindrop spectra as normalized gamma distribution from a Joss-Waldvogel disdrometer

Journal

ATMOSPHERIC RESEARCH
Volume 108, Issue -, Pages 57-73

Publisher

ELSEVIER SCIENCE INC
DOI: 10.1016/j.atmosres.2012.01.013

Keywords

Drop size distribution (DSD); Microphysics of precipitation; Precipitation particle measurement; Meteorological radar; Reflectivity; Stratiform and convective clouds; Microphysical parameterization schemes; Variability; Rainfall algorithms; RSD model parameters

Funding

  1. Colorado State University
  2. Natural Environment Research Council [cfaarr010001] Funding Source: researchfish
  3. NERC [cfaarr010001] Funding Source: UKRI

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The raindrop spectra observed in a precipitation system is a complex phenomenon that can help to explain the underlying physical processes of rainfall. This paper explores the characteristics of raindrop spectra in terms of drop size distributions (DSD) using seven years of Joss-Waldvogel disdrometer data within the mid-latitude UK region climatology. A total of 162,415 one-minute filtered raindrop spectra obtained from the disdrometer are fitted into a normalized gamma DSD model describing DSDs by the concentration parameter (N-w), the drop diameter (Do, and Do), and the shape parameter (mu). The results show that the rain rates retrieved from the normalized gamma DSD model are in good agreement with the disdrometer measured rain rates, implying the appropriateness of the raindrop spectra as normalized gamma distributions. The DSD characteristics are studied in different seasonal (cold and warm), atmospheric (dry and wet) as well as rain type (stratiform and convective) contexts in a long-term perspective. It has been revealed that the normalized gamma DSD parameters are very sensitive to the rain intensities. The mass weighted mean drop diameter D-m clearly increases exponentially with respect to the rain intensities. Variation of the DSDs in different contexts is also exposed reflecting seasonal, atmospheric and rain type consequence on raindrop spectra. Particularly, the scatterplot between the concentration parameter log(10)N(w) and the median drop diameter D-0 exhibits clear separation index between stratiform and convective DSDs. There is a large difference in averaged mass weighted mean drop diameters among stratiform and convective segments (stratiform =0.988 mm versus convective =1.99 mm). The DSD inconsistency in different contexts have been further examined in terms of the Z-R relationships (Z=aR(b)) variability. Additionally, 10 selected events taken place during the study period are also investigated, in which each of the events has shown unique DSD characteristics. (C) 2012 Elsevier B.V. All rights reserved.

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