Petr Chylek

Professor of Physics and Atmospheric Science

Diploma (1967), Charles University, Prague
Ph.D. (1970), University of California, Riverside

 

Member of the Americal Meteorological Society, American Geophysical Union, Canadian Meteorological and Oceanographic Society, Fellow of the Optical Society of America

My research interests

  • Atmospheric Radiation
  • Atmospheric Aerosols
  • Cloud Physics
  • Ice Core Analysis
  • Paleoclimate
  • Climate Diagnostic
  • Global Change

My research group

  • Petr Chylek
  • I Wayan Sudiarta (Ph. D. student)
  • Xiaobo Chen (Ph. D. student)
  • Dr. Glen Lesins (Research Associate)
  • Dr. W. Kim (Postdoctoral Fellow)
  • Regina Mass (Lab Technician)
  • Nancy Ogden (Lab Technician)

Current Research Projects

 

Global Change

A common view on the current climate change (global warming) is that it is a result of fossil fuel burning and the following increase in atmospheric concentration of carbon dioxide. In reality there are several factors that produce the current climate change. Some of the most important are:

The goal of our research is to understand the relative contributions of the above listed factors to the currently observed global warming. For this purpose we are analyzing existing climate and paleoclimate data, analyzing outputs of general circulation models and creating new approximations to for the various physical processes involved in climate system.To bring together experts holding different views on the current global warming an to faciliate an intense discussion of the related scince, we are organizing The First International Conference on Global Warming and The Next Ice Age, sponsorod by the American Meteorological Society and by the Canadian Meteorological and Oceanographic Society, to take place in Halifax in August 2001.

Atmospheric Aerosols

Atmospheric aerosols (airborne particulate matter) play an important role in atmospheric energy balance and climate change. Aerosols also affect biogeochemical cycles and human health. Man-made aerosols include sulfates, nitrates, black carbon, products of biomass burning, and soil dust (produced by agricultural activities). Main types of natural aerosols are sea salt, soil dust, aerosols produced by volcanos and forest fires, and biogenic sulfates and organic aerosols. Aerosols affect climate through their direct interaction with solar and terrestrial radiation (direct aerosol effect) and through their effect on the optical properties and life cycle of clouds (indirect aerosol effect). Atmospheric aerosols can significantly modify the predicted warming of greenhouse gases. We are investigating the growth of aerosols (sulfates, nitrates, sea salt, mineral dust and black carbon) with relative humidity, their interaction with atmospheric radiation, and their effect on clouds and climate. Our work also include the parameterization of aerosol optical properties as functions of relative humidity for use in climate models.

 

Clouds

Clouds reflect a considerable portion of incoming solar radiation back to space and they modify outgoing infrared radiation. The interplay between atmospheric radiation and dynamics, cloud microphysics, aerosols, and thermodynamics is not fully understood. In many cases, predicted climate changes (connected to increasing concentration of carbon dioxide and other greenhouse gases) are dependent on the cloud parameterization used in a particular general circulation model. Our current research concerns the effect of atmospheric aerosols on cloudiness and cloud optical properties, and improvement of cloud parameterizations in radiation codes used in climate models. We are also investigating the effect of black carbon on the absorption of solar radiation by clouds.

 

Laboratory and Field Measurements

In recent years we have seen tremendous progress in computer-based modeling of various atmospheric processes. Laboratory and field measurements are needed to provide suitable checks of our modeling abilities. The discrepancy between the measured and calculated absorption of solar radiation in cloudy atmospheres demonstrates the need of a balanced approach to atmospheric research that includes modeling and measurements. In our laboratory we are currently performing the most accurate measurements of the refractive indices of water, supercooled water, ice, sulfates, and nitrates. Our graduate students have participated in several international field measurement programs like NARE (North Atlantic Regional Experiment), RACE (Radiation, Aerosols and Cloud Experiment) and FIRE.

 

Ice Core Analysis

Ice core contains a wealth of information concerning past climate. We have developed a method for determining black carbon (soot) concentrations in ice core samples and we were able to detect large forest fires that occured up to about 2000 years ago. We also observed a large increase in biosphere burning (recorded in Antarctic ice core samples) a few thousand years after the end of the last ice age. Our current investigation is directed towards recent changes (last 200 years) in black carbon deposition rates in polar regions, attributed possibly to anthropogenic activities.

 

Light Scattering and Radiative Transfer

We are using several computational techniques and approximations to calculate the scattering and absorption of radiation by nonspherical and composite atmospheric particles. Ice crystals and mineral dust aerosols are examples of nonspherical particles in the atmosphere. Hailstones, melting snow, and mineral dust or black carbon within sulfate or cloud droplets are common composite particles. The scattering and absorption characteristics of these particles are needed for remote sensing and for climate forcing calculations. Monte Carlo and other radiative transfer techniques are used to determine aerosol climate forcing, and the effect of clouds and aerosols on surface UV fluxes. We are trying to understand interactions between solar and terrestrial radiation, and clouds, aerosols, and climate. The tools used in our research include laboratory and field measurements, computational modeling, and theoretical analysis.


 

Recently Supervised Ph. D. Thesis

Recently Supervised M. Sc. Thesis


 

Recent Invited Presentations

Recent Publications (1995-2000)


2000


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Updated: 27 June 2002