Weather today or tomorrow, short-term climate fluctuations, or its radical changes – all of these processes are strongly affected by the physical phenomena taking place in the atmosphere. The biggest source of uncertainty in weather and climate models are clouds and aerosols. This is why we study them in particular detail. We conduct our research using both theoretical (mainly numerical) and experimental methods, in the field and in our laboratories. We are particularly interested in cloud microphysics, i.e. the physical processes in the small spatial scale, responsible for the formation of rain and cloud disappearance.
We look especially closely at the physics of the phenomena occurring at the interface of clouds and clear air, where the processes of condensation, evaporation, turbulence, and radiative energy transfer play an important role. We conduct our research in a cloud chamber as well as in natural conditions, during international measurement campaigns using planes. One of our means of collecting data is the UltraFast Thermometer (UFT) developed in our Institute. While a plane flies through a cloud, it measures the changes in air temperature inside the cloud with even a centimeter resolution.
Modern cloud research would be impossible without numerical methods and the tools they provide. The numerical approach is used to solve equations describing the physical processes occurring in the scales ranging from millimeters (activation, growth by condensation and by collision-coalescence) to hundreds of kilometers (global circulation, wave and disturbance propagation). Our Institute has been using and developing numerical tools for many years now. In collaboration with the National Center for Atmospheric Research in Boulder, USA, and the European Centre for Medium-Range Weather Forecasts (ECMWF) in the United Kingdom, we use and refine, among others, the EULAG model (Eulerian/semi-Lagrangian fluid solver), known to many scientists, as well as the Langrangian Cloud Model. The latter combines the cloud-scale flow calculated through large eddy simulation (LES) with a Lagrangian description of cloud particles.
Our scientists also conduct research on the influence of atmospheric aerosol on the climate system. We study how the solar radiant flux on the surface changes depending on the physical properties of aerosol, and how it impacts the weather and climate in Europe and in the Arctic. We conduct research using in-situ methods as well as remote sensing instruments localized in the Radiative Transfer Laboratory and the Remote Sensing Laboratory. Our equipment includes a unique, multichannel PollyXT lidar, which is part of the EARLINET observational network. It performs aerosol measurements both in near range and in far range. We conduct research on aerosol in Poland as part of the Poland-AOD network. Our focus is studying the optical properties of aerosol during smog episodes and influxes of long-range pollution emitted in biomass burning and sandstorms.
We have a broad range of interests. In one of our project, we modeled the clear sky turbulence using data collected by commercial transport planes. In collaboration with the Poznań University of Life Sciences, we also study the connection between atmospheric aerosol and the productivity of peat bogs.
We are the only teaching unit in Poland educating the second cycle degree students in accordance with the World Meteorological Organization guidelines. Graduates of our programs are specialists skilled in numerical modeling of atmospheric processes (with applications in numerical weather forecasting and climate change projections), able to reliably interpret and process measurement data acquired through remote sensing and in-situ methods, as well as acquainted with databases and specialized software for meteorological data analysis and processing