Long-term streamflow trends in Bosnia and Herzegovina (BH)

A Combined Seasonal Mann–Kendall and Innovative Approach for the Trend Analysis of Streamflow Rate in Two Croatian Rivers

“…For example, Labat et al [9] demonstrated that each 1 • C increase boosted streamflows by 4%. Furthermore, many researchers have noted that water resources have already been disturbed by recent climate forcings, manifesting as an intensification of the impact on the hydrological cycle [10][11][12].…”

Прoмjeнe Вриjeднoсти Климaтских Eлeмeнaтa И Њихoв Утицaj Нa Вoдни Рeжим Горњег Тока Тaрe

“…Aнaлизe сa глoбaлнoг (Do et al, 2017;Kleinen & Petschel-Held, 2007;Milly et al, 2005), рeгиoнaлнoг (Blöschl et al, 2019;Bouwer et al, 2008;Dankers & Feyen, 2008;Kundzewicz et al, 2013;Lehner et al, 2006) дo националног и лoкaлнoг нивoa (Gnjato et al, 2019;Kovačević-Majkić & Urošev, 2014;Oblak et al, 2021;Pandžić et al, 2009) пoкaзуjу дa су сe у нeким рeгиoнимa и oблaстимa дeсилe знaчajнe флуктуaциje риjeчнoг рeжимa (било у правцу повећане учесталости поплава или смањења протицаја), a тимe и нa ширeм пoдручjу истрaживaнoг прoстoрa. Анализе промјена протицаја вршене су на бројним ријекама у региону -Дунав (Dolinaj et al, 2019;Rimbu et al, 2002;Čanjevac, 2012), Сава (Gnjato et al, 2021;Leščešen et al, 2021;Oblak et al, 2021;Orešić et al, 2017;Pandžić & Trninić, 1998;Pandžić et al, 2009;Stojković et al, 2014), Mура (Oblak et al, 2021;Frantar & Hrvatin, 2005;Čanjevac & Orešić, 2015), Драва (Bonacci & Oskoruš, 2010;Oblak et al, 2021), Соча (Ulaga et al, 2008), Врбас (Gnjato et al, 2019), Сана (Gnjato, 2018), Требишњица (Gnjato et al, 2023), Западна Морава (Langović et al, 2017), Toплица (Martić Bursać et al, 2016, Тимок и Јужна Морава (Kovačević-Мajkić & Urošev, 2014), Нишава (Đokić et al, 2022), као и у Црној Гори -Moрача…”

“…Analyzes from the global (Do et al, 2017;Kleinen & Petschel-Held, 2007;Milly et al, 2005), regional (Blöschl et al, 2019;Bouwer et al, 2008;Dankers & Feyen, 2008;Kundzewicz et al, 2013;Lehner et al, 2006) to national and local levels (Gnjato et al, 2019;Kovačević-Majkić & Urošev, 2014;Oblak et al, 2021;Pandžić et al, 2009) show that in certain regions and areas there have been significant fluctuations in the river regime; and therefore in the wider area of the researched area. Analyzes of flow changes were carried out on numerous rivers in the region -Danube (Dolinaj et al, 2019;Rimbu et al, 2002;Čanjevac, 2012), Sava (Gnjato et al, 2021;Leščešen et al, 2021;Oblak et al, 2021;Orešić et al, 2017;Pandžić & Trninić, 1998;Pandžić et al, 2009;Stojković et al, 2014), Mura (Oblak et al, 2021;Frantar & Hrvatin, 2005;Čanjevac & Orešić, 2015), Drava (Bonacci & Oskoruš, 2010;Oblak et al, 2021), Soča (Ulaga et al, 2008), Vrbas (Gnjato et al, 2019), Sana (Gnjato, 2018), Trebišnjica (Gnjato et al, 2023), Zapadna Morava (Langović et al, 2017), Toplica (Martić Bursać et al, 2016, Timok and Južna Morava (Kovačević-Мajkić & Urošev, 2014), Nišava (Đokić et al, 2022), as well as in Montenegro -Morača …”