15 research outputs found

    ARRIVAL DATES OF MIGRATING BIRDS IN CENTRAL EUROPE AND CLIMATE VARIABILITY

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    Recently the study of plant and animal phenological observations has contributed much to understand the sensitivity of biosphere to the variability of its atmospheric environment. This study is based on time series of 3 bird phenological phases (‘first barn swallow’, ‘first cuckoo call’ and ‘all swallows have left’) from the archive of the Central Institute for Meteorology and Geodynamics in Vienna, which have been collected at 65 Austrian stations from 1951 – 1999. In contrast to many European countries the arrival times of barn swallow and the cuckoo have predominantly been moving to later dates in Austria. A preliminary analysis points towards dryer conditions in the sub - saharan winter quarters as possible cause for a later departure from the African winter quarters to Europe. About a third of the year to year variability of both spring bird phases can be explained by temperature and wind conditions on the migration route and local temperature

    EVALUATION OF THE OPERATIONAL OZONE FORECAST MODEL OF THE ZAMG WITH MEASUREMENTS OF THE AUSTRIAN AIR QUALITY NETWORK

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    Operational model forecasts of ozone concentrations are compared to the observations of about 150 air quality stations in Austria. Evaluations of the last three summers revealed that exceedances of the information threshold could be predicted quite well by the model. Investigation of a heat period in summer 2006 indicates possible sources of precursors. The Lagrangian particle model LASAT (www.janicke.de) is used additionally to the chemical model CAMx (www.camx.com) to show the dispersion of the plumes of stacks with high emissions of NOx in the vicinity of Vienna. For two months in summer 2007 sensitivity studies with different input parameters were performed. Model runs with different parameterisations for the vertical diffusion coefficient (Kv) are conducted and experiments with different values of the minimum values of Kv in the lower levels show the influence of this parameter on the nocturnal ozone decrease for different sites. Different model runs with variable boundary conditions at the top of the modelling domain as well as variable total ozone column data are performed
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