Physics Department: Clouds - LACIS

Overview

Atmospheric clouds are complex systems the influence of which is global concerning the formation of precipitation and the energy budget. Via the emission of gases and particulate matter (the products of combustive processes are especially important in this context), human activity alters the formation and characteristics of clouds and exerts an influence on the spatial distribution and intensity of precipitation and on climate in general.

Given their complexity and their irregular appearance in inaccessible locations, atmospheric clouds are difficult to investigate. As a consequence, many of the processes associated with cloud formation and precipitation are still inadequately understood, and are not yet quantifiable with sufficient exactitude. They must, hence, be investigated in appropriate experiments. Key processes in this connection are the formation of condensation droplets on the natural and anthropogenic particulate matter available in the atmosphere, as well as the freezing of cloud droplets.

In order to investigate these key processes under clearly defined and controllable conditions, the "Leipzig Aerosol Cloud Interaction Simulator" (LACIS) was built at the Leibniz Institute for Tropospheric Research in Leipzig. In the form of an 8 m long vertically oriented flow tube, LACIS was configured such that atmospheric conditions for particle and droplet growth in relation to water vapour saturation and to time can be imitated as closely to reality as possible. For further information on setup, measurement principle, and experiments at LACIS click here.

LACIS-Versuchsaufbau

The LACIS flow tube (colored in pink - middle picture) with several thermostats for the regulation of temperatures inside LACIS (left picture) and with a setup to generate aerosol particles (right picture).

Experiments that have been or will be conducted at LACIS cover:
  • the influence of the chemical composition of aerosol particles onto their hygroscopic growth and activation (examined were pure substances as well as mixtures of soluble, slightly soluble, and insoluble ones)
  • the influence of atmospheric trace gases (e.g., HCl, HNO3) on the growth of particles and droplets
  • the influence of the chemical composition of the aerosol particles and of their shape onto the freezing of cloud droplets
Last modification: 2007-04-20