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Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12128/8770
Title: Vertical climatic belts in the Tatra Mountains in the light of current
Authors: Łupikasza, Ewa
Szypuła, Bartłomiej
Keywords: Carpathians; vertical climatic belts; DEM
Issue Date: 2018
Citation: Theoretical and Applied Climatology, Vol. 136, no. 1-2 (2018), s. 249-264
Abstract: The paper discusses temporal changes in the configuration of vertical climatic belts in the Tatra Mountains as a result of current climate change. Meteorological stations are scarce in the Tatra Mountains; therefore, we modelled decadal air temperatures using existing data from 20 meteorological stations and the relationship between air temperature and altitude. Air temperature was modelled separately for northern and southern slopes and for convex and concave landforms. Decadal air temperatures were additionally used to delineate five climatic belts previously distinguished by Hess on the basis of threshold values of annual air temperature. The spatial extent and location of the borderline isotherms of 6, 4, 2, 0, and − 2 °C for four decades, including 1951–1960, 1981–1990, 1991–2000, and 2001–2010, were compared. Significant warming in the Tatra Mountains, uniform in the vertical profile, started at the beginning of the 1980s and led to clear changes in the extent and location of the vertical climatic belts delineated on the basis of annual air temperature. The uphill shift of the borderline isotherms was more prominent on southern than on northern slopes. The highest rate of changes in the extent of the climatic belts was found above the isotherm of 0 °C (moderately cold and cold belts). The cold belt dramatically diminished in extent over the research period.
URI: http://hdl.handle.net/20.500.12128/8770
DOI: 10.1007/s00704-018-2489-2
ISSN: 0177-798X
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