Climatic Change

, Volume 36, Issue 3, pp 327–344

20th-CENTURY CHANGES OF TEMPERATURE IN THE MOUNTAIN REGIONS OF CENTRAL EUROPE

Authors

  • RUDOLF O. WEBER
    • Paul Scherrer Institute
  • PETER TALKNER
    • Paul Scherrer Institute
  • INGEBORG AUER
    • Central Institute for Meteorology and Geodynamics
  • REINHARD BÖHM
    • Central Institute for Meteorology and Geodynamics
  • MARJANA GAJIĆ-ČAPKA
    • Meteorological and Hydrological ServiceCentre for Meteorological Research
  • KSENIJA ZANINOVIĆ
    • Meteorological and Hydrological ServiceCentre for Meteorological Research
  • RUDOLF BRÁZDIL
    • Department of GeographyMasaryk University
  • PAVEL FAŠKO
    • Slovak Hydrometeorological Institute
Article

DOI: 10.1023/A:1005378702066

Cite this article as:
WEBER, R.O., TALKNER, P., AUER, I. et al. Climatic Change (1997) 36: 327. doi:10.1023/A:1005378702066

Abstract

Daily maximum and minimum temperatures from 29 low-lying and mountain stations of 7 countries in Central Europe were analyzed. The analysis of the annual variation of diurnal temperature range helps to distinguish unique climatic characteristics of high and low altitude stations. A comparison of the time series of extreme daily temperatures as well as mean temperature shows a good agreement between the low-lying stations and the mountain stations. Many of the pronounced warm and cold periods are present in all time series and are therefore representative for the whole region. A linear trend analysis of the station data for the period 1901–1990 (19 stations) and 1951–1990 (all 29 stations) shows spatial patterns of similar changes in maximum and minimum daily temperatures and diurnal temperature range. Mountain stations show only small changes of the diurnal temperature range over the 1901–1990 period, whereas the low-lying stations in the western part of the Alps show a significant decrease of diurnal temperature range, caused by strong increase of the minimum temperature. For the shorter period 1951–1990, the diurnal temperature range decreases at the western low-lying stations, mainly in spring, whereas it remains roughly constant at the mountain stations. The decrease of diurnal temperature range is stronger in the western part than in the eastern part of the Alps.

Copyright information

© Kluwer Academic Publishers 1997