HYDROLOGICAL DROUGHT ASSESSMENT OF THE TISZA RIVER
Drought is a natural phenomenon that occurs when the availability of water is significantly below the normal levels during a shorter or longer period of time and cannot meet the necessary demand. This study focused on hydrological drought assessment of the Tisza River on four gauging stations: Vásár...
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Geographical Institute "Jovan Cvijić" SASA
2020-10-01
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doaj-5dbcf5c857a44b97b244fceecdde2c382021-03-07T22:46:00ZengGeographical Institute "Jovan Cvijić" SASAZbornik Radova: Geografski institut "Jovan Cvijić"0350-75991821-28082020-10-0170210.2298/IJGI2002089L141HYDROLOGICAL DROUGHT ASSESSMENT OF THE TISZA RIVERIgor Leščešen0Dragan Dolinaj1Milana Pantelić2Tamás Telbisz3György Varga4University of Novi Sad, Climatological and Hydrological Research Center, Novi SadUniversity of Novi Sad, Climatological and Hydrological Research Center, Novi SadUniversity of Novi Sad, Climatological and Hydrological Research Center, Novi SadEötvös Loránd University, Institute of Geography and Earth Sciences, Department of Physical Geography, BudapestEötvös Loránd University, Institute of Geography and Earth Sciences, Department of Physical Geography, BudapestDrought is a natural phenomenon that occurs when the availability of water is significantly below the normal levels during a shorter or longer period of time and cannot meet the necessary demand. This study focused on hydrological drought assessment of the Tisza River on four gauging stations: Vásárosnamény, Szolnok, Szeged, and Senta for the period 1964–2018. An effective Streamflow Drought Index (SDI) has been recently proposed and widely used for determining hydrological droughts. Both long- and short-term droughts have very severe impacts on the investigated locations. Two drought periods can be singled out: the first period was from 1983 to 1993, with the exceptions in 1985 and 1987. This period is characterized by higher absolute SDI values on Vásárosnamény (–0.84) and Szolnok (–0.87) than on Szeged (–0.29) and Senta (–0.40) stations. The second period was more severe and lasted from 2011 to 2015, with an average SDI value of –1.32 on Vásárosnamény, –1.08 on Szolnok, –0.53 on Szeged, and –0.57 on Senta station. The Mann-Kendall test results indicate that there is no trend indicating transition from humid towards more arid condition over the investigated period. http://ojs.gi.sanu.ac.rs/index.php/zbornik/article/view/160droughtStreamflow Drought IndexTisza RiverSerbiaHungary |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Igor Leščešen Dragan Dolinaj Milana Pantelić Tamás Telbisz György Varga |
spellingShingle |
Igor Leščešen Dragan Dolinaj Milana Pantelić Tamás Telbisz György Varga HYDROLOGICAL DROUGHT ASSESSMENT OF THE TISZA RIVER Zbornik Radova: Geografski institut "Jovan Cvijić" drought Streamflow Drought Index Tisza River Serbia Hungary |
author_facet |
Igor Leščešen Dragan Dolinaj Milana Pantelić Tamás Telbisz György Varga |
author_sort |
Igor Leščešen |
title |
HYDROLOGICAL DROUGHT ASSESSMENT OF THE TISZA RIVER |
title_short |
HYDROLOGICAL DROUGHT ASSESSMENT OF THE TISZA RIVER |
title_full |
HYDROLOGICAL DROUGHT ASSESSMENT OF THE TISZA RIVER |
title_fullStr |
HYDROLOGICAL DROUGHT ASSESSMENT OF THE TISZA RIVER |
title_full_unstemmed |
HYDROLOGICAL DROUGHT ASSESSMENT OF THE TISZA RIVER |
title_sort |
hydrological drought assessment of the tisza river |
publisher |
Geographical Institute "Jovan Cvijić" SASA |
series |
Zbornik Radova: Geografski institut "Jovan Cvijić" |
issn |
0350-7599 1821-2808 |
publishDate |
2020-10-01 |
description |
Drought is a natural phenomenon that occurs when the availability of water is significantly below the normal levels during a shorter or longer period of time and cannot meet the necessary demand. This study focused on hydrological drought assessment of the Tisza River on four gauging stations: Vásárosnamény, Szolnok, Szeged, and Senta for the period 1964–2018. An effective Streamflow Drought Index (SDI) has been recently proposed and widely used for determining hydrological droughts. Both long- and short-term droughts have very severe impacts on the investigated locations. Two drought periods can be singled out: the first period was from 1983 to 1993, with the exceptions in 1985 and 1987. This period is characterized by higher absolute SDI values on Vásárosnamény (–0.84) and Szolnok (–0.87) than on Szeged (–0.29) and Senta (–0.40) stations. The second period was more severe and lasted from 2011 to 2015, with an average SDI value of –1.32 on Vásárosnamény, –1.08 on Szolnok, –0.53 on Szeged, and –0.57 on Senta station. The Mann-Kendall test results indicate that there is no trend indicating transition from humid towards more arid condition over the investigated period.
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topic |
drought Streamflow Drought Index Tisza River Serbia Hungary |
url |
http://ojs.gi.sanu.ac.rs/index.php/zbornik/article/view/160 |
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