Airborne and ground-based holographic measurement of hydrometeors in liquid-phase, mixed-phase and ice clouds

A new cloud particle spectrometer has been developed in this work with the purpose of obtaining in-situ measurements on different research aircraft. It is based on the principle of digital in-line holography and delivers six images per second of the recorded interference pattern from the laser backg...

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Bibliographic Details
Main Author: Schlenczek, O.
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: 2018
Subjects:
Online Access:http://hdl.handle.net/21.11116/0000-0007-8860-3
Description
Summary:A new cloud particle spectrometer has been developed in this work with the purpose of obtaining in-situ measurements on different research aircraft. It is based on the principle of digital in-line holography and delivers six images per second of the recorded interference pattern from the laser background and particles suspended in the approx. 35 cubic centimeter large sample volume. Particle position and two-dimensional in-focus images of particles are determined via numerical reconstruction based on Fraunhofer diffraction pattern analysis. Particle properties such as diameter, area and mass are calculated from the reconstructed images. This new instrument, called "HALOHolo", has been calibrated in the laboratory w.r.t. particle detectability and sizing accuracy. An instrument intercomparison with other cloud particle spectrometers confirmed the determined instrument characteristics in general. Measurements in liquid-phase, mixed-phase and ice clouds have been obtained from three airborne field campaigns where HALOHolo was operated on two different aircraft. The liquid-phase clouds measured were Arctic stratocumulus clouds, where the connection between variability of particle number concentration and mean volume diameter was investigated. The measured data were indicative of inhomogeneous mixing between the cloud and the surrounding air. A developing tropical rain shower was sampled in the process of glaciation and its microphysical evolution has been characterized. The local environment of ice crystals surrounded by supercooled liquid water droplets was studied and the spatial distribution of ice crystals and droplets was found to be a uniform random distribution for the majority of measurements in the rapid glaciation zone of the cloud. In addition, the simultaneous occurrence of small columnar ice crystals among larger rimed particles (graupels) has been documented in a variety of cases, which were most likely to be found in strong updrafts. Finally, the spatial structure of cirrus clouds has been ...