4.4 Article

Dependence of Ice Crystal Size Distributions in High Ice Water Content Conditions on Environmental Conditions: Results from the HAIC-HIWC Cayenne Campaign

Journal

JOURNAL OF THE ATMOSPHERIC SCIENCES
Volume 79, Issue 12, Pages 3103-3134

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JAS-D-22-0008.1

Keywords

South America; Tropics; Mesoscale systems; Cirrus clouds; Cloud microphysics; Ice crystals

Funding

  1. National Science Foundation [1213311, 1842094]
  2. FAA William Hughes Technical Center and Aviation Weather Research Program
  3. NASA Aeronautics Research Mission Directorate Aviation Safety Program
  4. Boeing Co., Environment and Climate Change Canada
  5. National Research Council of Canada, and Transport Canada
  6. European Commission [ACP2-GA-2012-314314]
  7. European Safety Agency (EASA) [EASA.2013.FC27]
  8. Ice Crystal Consortium
  9. China Scholarship Council (CSC)
  10. Div Atmospheric & Geospace Sciences
  11. Directorate For Geosciences [1213311, 1842094] Funding Source: National Science Foundation

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This study introduces a new method to determine the modality of particle size distribution (PSD) and its representation using gamma functions. It investigates the influence of environmental conditions, such as temperature and ice water content, on the parameters of the gamma function. The results show that temperature and ice water content are the most important factors affecting the modality of PSD.
A new method that automatically determines the modality of an observed particle size distribution (PSD) and the representation of each mode as a gamma function was used to characterize data obtained during the High Altitude Ice Crystals and High Ice Water Content (HAIC-HIWC) project based out of Cayenne, French Guiana, in 2015. PSDs measured by a 2D stereo probe and a precipitation imaging probe for particles with maximum dimension (D-max) > 55 mu m were used to show how the gamma parameters varied with environmental conditions, including temperature (T) and convective properties such as cloud type, mesoscale convective system (MCS) age, distance away from the nearest convective peak, and underlying surface characteristics. Four kinds of modality PSDs were observed: unimodal PSDs and three types of multimodal PSDs (Bimodal1 with breakpoints 100 +/- 20 mu m between modes, Bimodal2 with breakpoints 1000 +/- 300 mu m, and Trimodal PSDs with two breakpoints). The T and ice water content (IWC) are the most important factors influencing the modality of PSDs, with the frequency of multimodal PSDs increasing with increasing T and IWC. An ellipsoid of equally plausible solutions in (N-o-lambda-mu) phase space is defined for each mode of the observed PSDs for different environmental conditions. The percentage overlap between ellipsoids was used to quantify the differences between overlapping ellipsoids for varying conditions. The volumes of the ellipsoid decrease with increasing IWC for most cases, and (N-o-lambda-mu) vary with environmental conditions related to distribution of IWC. HIWC regions are dominated by small irregular ice crystals and columns. The parameters (N-o-lambda-mu) in each mode exhibit mutual dependence.

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