Seeding of Supercooled Low Stratus Clouds with a UAV to Study Microphysical Ice Processes: An Introduction to the CLOUDLAB Project

Author:

Henneberger Jan1,Ramelli Fabiola1,Spirig Robert1,Omanovic Nadja1,Miller Anna J.1,Fuchs Christopher1,Zhang Huiying1,Bühl Johannes2,Hervo Maxime3,Kanji Zamin A.1,Ohneiser Kevin2,Radenz Martin2,Rösch Michael1,Seifert Patric2,Lohmann Ulrike1

Affiliation:

1. Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland;

2. Leibniz Institute for Tropospheric Research (TROPOS), Leipzig, Germany;

3. Federal Office of Meteorology and Climatology MeteoSwiss, Payerne, Switzerland

Abstract

Abstract Ice formation and growth processes play a crucial role in the evolution of cloud systems and the formation of precipitation. However, the initial formation and growth of ice crystals are challenging to study in the real atmosphere resulting in uncertainties in weather forecasts and climate projections. The CLOUDLAB project tackles this problem by using supercooled stratus clouds as a natural laboratory for targeted glaciogenic cloud seeding to advance the understanding of ice processes: Ice nucleating particles are injected from an uncrewed aerial vehicle (UAV) into supercooled stratus clouds to induce ice crystal formation and subsequent growth processes. Microphysical changes induced by seeding are measured 3–15 min downstream of the seeding location using in situ and ground-based remote sensing instrumentation. The novel application of seeding with a multirotor UAV combined with the persistent nature of stratus clouds enables repeated seeding experiments under similar and well-constrained initial conditions. This article describes the scientific goals, experimental design, and first results of CLOUDLAB. First, the seeding plume is characterized by using measurements of a UAV equipped with an optical particle counter. Second, the seeding-induced microphysical changes observed by cloud radars and a tethered balloon system are presented. The seeding signatures were detected by regions of increased radar reflectivity (>−20 dBZ), which were 10–20 dBZ higher than the natural background. Simultaneously, high concentrations of seeding particles and ice crystals (up to 2,000 L−1) were observed. A cloud seeding case was simulated with the numerical weather model ICON to contextualize the findings.

Publisher

American Meteorological Society

Subject

Atmospheric Science

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