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https://doi.org/10.21861/HGG.2015.77.01.01

Contemporary changes of mean annual and seasonal river discharges in Croatia

Ivan Čanjevac orcid id orcid.org/0000-0002-1536-4128 ; Sveučilište u Zagrebu, Prirodoslovno-matematički fakultet, Geografski odsjek, Zagreb, Hrvatska
Danijel Orešić orcid id orcid.org/0000-0002-5809-085X ; Sveučilište u Zagrebu, Prirodoslovno-matematički fakultet, Geografski odsjek, Zagreb, Hrvatska


Puni tekst: engleski pdf 1.070 Kb

str. 7-27

preuzimanja: 1.132

citiraj


Sažetak

This paper presents the first comprehensive nationwide trend detection of mean discharges in Croatia. Over the last 30 years, global climate change has manifested itself largely in the rise of the average annual temperature, which has resulted in the changes of evapotranspiration and precipitation patterns. The consequences of those changes have been varied spatial impacts on river discharge (flow). We analysed the changes in mean river discharges in Croatia at 53 gauging hydrological stations over the most recent period from 1990 to 2009. To assess the trend, the Kendall-Theil (Sen) non parametric trend test was carried out for the yearly and seasonal mean discharge values. We found evidence of redistribution of discharge throughout the year, an increase in autumn and winter discharges (especially on the rivers dominantly fed by snowmelt) and a decrease in summer discharge values. Furthermore, we detected a change in the month of the appearance of mean discharge maxima and minima. In most cases the changes can be explained by the changes in the regime of climate elements (temperature, precipitation, evapotranspiration) although that information should be treated with care because of the shortness of the time-series. The results are consistent with the ones from the upstream countries, i.e. Slovenia and Austria.

Ključne riječi

discharge; trends; Croatia; rivers; hydrology; geography

Hrčak ID:

142678

URI

https://hrcak.srce.hr/142678

Datum izdavanja:

29.7.2015.

Podaci na drugim jezicima: hrvatski

Posjeta: 2.766 *