RAINFALL AND RUNOFF REGIME TRENDS IN MOUNTAIN CATCH MENTS (CASE STUDY AREA: THE UPPER HRON RIVER BASIN, SLOVA KIA)
Abstract
This paper presents an analysis of trends and causes of changes of selected hydroclimatic variables influencing the runoff regime in the upper Hron River basin (Slovakia), complemented by assessment of floods. Different methods for identifying trends in data series are evaluated and include: simple mass curve analysis, linear regression, frequency analysis of flood events, use of the Indicators of Hydrological Alteration software, and the Mann-Kendall test.
Analyses are performed for data from 1931 to 2010. The changes in runoff are significant, especially in terms of lower QMax and 75 percentile values.
This fact is also confirmed by the lower frequency and extremity of flood events. The 1980s are considered a turning point in the development of all hydroclimatic variables.
The Mann-Kendall test shows a significant decrease in runoff in the winter period. The main causes of runoff decline are: the considerable increase in air temperature, the decrease in snow cover depth and changes in seasonal distribution of precipitation amounts.