{"id":2125,"date":"2026-02-24T17:26:18","date_gmt":"2026-02-24T14:26:18","guid":{"rendered":"https:\/\/hydro-chemistry-ecology.knu.ua\/?page_id=2125"},"modified":"2026-02-24T17:37:22","modified_gmt":"2026-02-24T14:37:22","slug":"%d1%85%d1%96%d0%bb%d1%8c%d1%87%d0%b5%d0%b2%d1%81%d1%8c%d0%ba%d0%b8%d0%b9-%d0%b2-%d0%ba-%d0%be%d1%81%d0%be%d0%b1%d0%bb%d0%b8%d0%b2%d0%be%d1%81%d1%82%d1%96-%d0%b3%d1%96%d0%b4%d1%80%d0%be%d0%b3%d1%80-2","status":"publish","type":"page","link":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/%d1%85%d1%96%d0%bb%d1%8c%d1%87%d0%b5%d0%b2%d1%81%d1%8c%d0%ba%d0%b8%d0%b9-%d0%b2-%d0%ba-%d0%be%d1%81%d0%be%d0%b1%d0%bb%d0%b8%d0%b2%d0%be%d1%81%d1%82%d1%96-%d0%b3%d1%96%d0%b4%d1%80%d0%be%d0%b3%d1%80-2\/","title":{"rendered":"KHILCHEVSKYI V.K. FEATURES OF HYDROGRAPHY AND WATER RESOURCES OF HUNGARY"},"content":{"rendered":"\n<p><strong>DOI: <a href=\"https:\/\/doi.org\/10.17721\/2306-5680.2025.3.1\">https:\/\/doi.org\/10.17721\/2306-5680.2025.3.1<\/a><\/strong><\/p>\n\n\n\n<p><a href=\"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/issn-2306-5680-%d0%b3%d1%96%d0%b4%d1%80%d0%be%d0%bb%d0%be%d0%b3%d1%96%d1%8f-%d0%b3%d1%96%d0%b4%d1%80%d0%be%d1%85%d1%96%d0%bc%d1%96%d1%8f-%d1%96-%d0%b3%d1%96%d0%b4%d1%80%d0%be%d0%b5%d0%ba%d0%be%d0%bb-6\/\" target=\"_blank\" rel=\"noreferrer noopener\">Hydrology, Hydrochemistry and Hydroecology. 2025. \u2116 3(77)<br><\/a><strong>Publication language: <\/strong>Ukrainian<br><strong>Authors:<br><\/strong>Khilchevskyi V.K., Taras Shevchenko National University of Kyiv <\/p>\n\n\n\n<p><em>The article is devoted to the study of hydrography and water resources of the territory of Hungary. The country&#8217;s hydrographic conditions are determined by its location in the center of the Carpathian basin, therefore its entire territory belongs to the Danube basin. The river enters the territory of Hungary in transit. Danube (from Slovakia) and Tisza is the largest tributary of the Danube (from Ukraine). Another large river \u2013 the Drava (a tributary of the Danube) forms the border between Hungary and Croatia. The annual water balance shows a surplus \u2013 about 100 km<sup>3<\/sup> of water flows south from the country through rivers. Only 10% of this volume falls on precipitation, the rest is brought by rivers from the surrounding areas. There are about 9,800 rivers in the country, of which only 1,031 rivers have a catchment area exceeding 10 km<sup>2<\/sup>. According to the hydrographic zoning of the territory of Hungary, carried out in accordance with the requirements of the EU Water Framework Directive, one area of the river basin is distinguished \u2013 the Danube, which includes 4 sub-basins: the Danube itself; Tisza;&nbsp; Drava; lake Balaton.<\/em><br><em>About 3,500 lakes are included in the list of the country&#8217;s lakes. reservoir It includes natural lakes, which account for 25% of all water bodies, and man-made lakes, which account for 75% of the country&#8217;s water bodies. Balaton is the largest freshwater lake in the country and in the central part of Europe. The largest reservoir is Lake Tisza on the river Tisza. The average annual volume of total renewable water resources in Hungary is 104 km<sup>3<\/sup>\/year, of which 6% are internal (local) water resources (6 km<sup>3<\/sup>\/year), and 94% are external water resources (98 km<sup>3<\/sup>\/year). The indicator of total water resources per 1 person is 10,697 m<sup>3<\/sup>\/year, internal water resources per 1 person is 642 m<sup>3<\/sup>\/year. During 1992-2018 there was a noticeable reduction in the use of water resources in the country. Thus, the total withdrawal of surface water decreased by 1.8 times &#8211; from 7137 million m<sup>3<\/sup> (1992) to 4033 million m<sup>3<\/sup> (2018). Structure of surface water use in 2018: industry \u2013 82.2%; agriculture &#8211; 9.5%. communal water supply \u2013 6.2%; recreational water use \u2013 1.5%; ecological water use \u2013 0.6%. A modern institutional structure of water resources management has been created in the country.<\/em><\/p>\n\n\n\n<p><strong><em>Keywords:<\/em><\/strong><em> hydrography<\/em><em>;<\/em><em> water bodies<\/em><em>;<\/em><em> hydrographic zoning<\/em><em>;<\/em><em> river<\/em><em>;<\/em><em> lake<\/em><em>;<\/em><em> reservoir<\/em><em>;<\/em><em> water resources<\/em><em>;<\/em><em> management<\/em><em>;<\/em><em> Danube<\/em><em>;<\/em><em> Tisza<\/em><em>;<\/em><em> Hungary.<\/em><em><\/em><\/p>\n\n\n\n<p><strong>References<\/strong>:<br>1. Topohrafichna karta Uhorshchyny [Topographic map of Hungary] URL:&nbsp; https:\/\/ua.mozaweb.com\/Extra-3D_sceni-Topografichna_karta_Ugorshini-139724<br>2. Khilchevskyi V.K. Vodni resursy krain Yevropy: kharakterystyka na osnovi bazy danykh FAO-Aquastat [Water resources of European countries: characteristics based on the FAO-Aquastat database]. Hidrolohiia, hidrokhimiia i hidroekolohiia, 2023. \u2116 1(67). S. 6-16.<br>3. Khilchevskyi V.K. Hidrohrafiia ta vodni resursy Yevropy [Hydrography and water resources of Europe]. \u041ayiv, DIA, 2023. 308 s.<br>4. Khilchevskyi V.K., Petovka V.Iu. Vodni resursy Uhorshchyny: dosvid upravlinnia v konteksti yevropeiskoi intehratsii [Water resources of Hungary: management experience in the context of European integration]. Zbirnyk tez XIII Mizhnar. naukovo-praktychnoi konferentsii \u00abVoda dlia maibutnoho: upravlinnia, zberezhennia, innovatsii\u00bb, prysviachenoi Vsesvitnomu dniu vodnykh resursiv, 25-26 bereznia 2025 r. Kyiv.: IVPiM NAAN Ukrainy 2025. S. 68-71. URL: https:\/\/mivg.iwpim.com.ua\/files\/Water_day_tezy2025.pdf<br>5. Aquastat: FAO. Country Profile &#8211; Hungary. URL: https:\/\/www.fao.org\/aquastat\/en\/countries-and-basins\/country-profiles\/country\/HUN<br>6. Balatonyi L., Ligetv\u00e1ri K., T\u00f3th L., Berger A. Water resources management and its homeland security aspect in Hungary. Scientia et Securitas. 2022. 2(4). 519-528.<br>7. Borsos B., Sendzimir J. The Tisza River: Managing a Lowland River in the Carpathian Basin. In: Schmutz, S., Sendzimir, J. (eds) Riverine Ecosystem Management. Aquatic Ecology Series, 2018. Vol 8. Springer, Cham. https:\/\/doi.org\/10.1007\/978-3-319-73250-3_28<br>8. ClimateChangePost \u2013 Hungary. URL: https:\/\/www.climatechangepost.com\/countries\/hungary\/<br>9. Danube Facts and Figures. Hungary. URL: https:\/\/www.icpdr.org\/sites\/default\/files\/nodes\/documents\/hungary_facts__figures.pdf<br>10. Dob\u00f3 K. A hazai \u00e1rv\u00edzv\u00e9delmi strat\u00e9gia f\u0151bb ir\u00e1nyai. M\u0171szaki Katonai K\u00f6zl\u00f6ny. 2019. (29)(2). 133-144. DOI: 10.32562\/mkk.2019.2.11<br>11. Duna k\u00f6zvetlen r\u00e9szv\u00edzgy\u0171jt\u0151. V\u00edz Keretir\u00e1nyelv, v\u00edzgy\u0171jt\u0151-gazd\u00e1lkod\u00e1si tervez\u00e9s. URL: https:\/\/www.gwpszotar.hu\/kifejezes\/1531?kulcsszo=Duna<br>12. General Directorate of Water Management. URL: https:\/\/www.ovf.hu\/en\/about-us<br>13. Goda L., Kalocsa B., Tam\u00e1s E.A. Riverbed erosion on the Hungarian section of the Danube. Journal of Environmental Science for Sustainable Society. 2007. 1. 47-54. DOI: 10.3107\/jesss.1.47<br>14. Hungarian Hydrological Forecasting Service. URL: https:\/\/www.hydroinfo.hu\/en\/index.html<br>15. Hungary. ICPDR &#8211; International Commission for the Protection of the Danube. URL: https:\/\/www.icpdr.org\/danube-basin\/countries\/hungary#:~:text=Hungary<br>16. Hungary topographic map. URL: https:\/\/commons.wikimedia.org\/wiki\/File:Hungary_topographic_map.jpg<br>17. Honnan \u201eered\u201d a csapv\u00edz Magyarorsz\u00e1gon? URL:&nbsp; https:\/\/www.maviz.org\/fogyasztoi_informaciok\/honnan_ered_a_csapviz_magyarorszagon<br>18. Institute of Aquatic Ecology &#8211; Centre for Ecological Research. URL:&nbsp; https:\/\/ecolres.hun-ren.hu\/en\/intezetek\/institute-of-aquatic-ecology\/<br>19. Kiss T., Blanka V. River channel response to climate- and human-induced hydrological changes: Case study on the meandering Hern\u00e1d River, Hungary. Geomorphology. 2012. Vol. 175-176. 115-125.<br>20. Konecsny K; Nagy Z. Similarities and differences of the hydrological extremes on the Duna\/Danube and Tisza\/Tisa Rivers (1921-2012). Aerul si Apa. Componente ale Mediului. 2014. 134-141. URL: https:\/\/www.proquest.com\/docview\/1611002560<br>21. L\u00e1szl\u00f3 E. Magyarorsz\u00e1g v\u00edz\u00fcgyi igazgat\u00e1s\u00e1nak fejl\u0151d\u00e9st\u00f6rt\u00e9neti \u00e1ttekint\u00e9se a kiegyez\u00e9st\u0151l napjainkig. Pro Publico Bono &#8211; Magyar K\u00f6zigazgat\u00e1s. 2019. 4, 80\u2013105. DOI: 10.32575\/ppb.2019.4.4<br>22. Magyar Hidrol\u00f3giai T\u00e1rsas\u00e1g. URL: https:\/\/www.hidrologia.hu\/bemutatkozas\/<br>23. Magyarorsz\u00e1g v\u00edzgy\u0171jt\u0151-gazd\u00e1lkod\u00e1si terve \u2013 2021. I. Vitaanyag a tervet. Orsz\u00e1gos V\u00edz\u00fcgyi F\u0151igazgat\u00f3s\u00e1g. URL:&nbsp; https:\/\/vizeink.hu\/wp-content\/uploads\/2020\/12\/VGT_Vitaanyag_1222.pdf<br>24. Mez\u0151si G. Physical geography of Hungary. Springer. 2017. 325 p.<br>25. Nov\u00e1ky B., B\u00e1lint G. Shifts and Modification of the Hydrological Regime Under Climate Change in Hungary. In book: Climate Change &#8211; Realities, Impacts Over Ice Cap, Sea Level and Risks. Ed. by B. R. Singh. 2013. DOI: 10.5772\/54768<br>26. Tam\u00e1s E.A. The hydrological regime of the middle Danube reach and implications on the lateral connectivity offloodplains. Floodplain Conference. June 08 2022, Baja, Hungary. URL: https:\/\/vtk.uni-nke.hu\/document\/vtk-uni-nke-u\/Tam%C3%A1s%20Enik%C5%91%20Anna_220608.pdf<br>27. VGT1: 2010. m\u00e1jus 5-\u00e9n a Magyar Korm\u00e1ny elfogadta Magyarorsz\u00e1g els\u0151 V\u00edzgy\u0171jt\u0151-gazd\u00e1lkod\u00e1si Terv\u00e9t. 2010. URL: https:\/\/vizeink.hu\/korabbi-vizgyujto-gazdalkodasi-tervek\/vizgyujto-gazdalkodasi-terv\/<br>28. Worldometer. Hungary Water. URL: https:\/\/www.worldometers.info\/water\/hungary-water\/<\/p>\n\n\n\n<p><a href=\"https:\/\/hydro-chemistry-ecology.knu.ua\/wp-content\/uploads\/2026\/02\/1-\u2116-377_2025.pdf\" target=\"_blank\" rel=\"noreferrer noopener\">READ THE FULL ARTICLE<\/a><br><a href=\"https:\/\/hydro-chemistry-ecology.knu.ua\/wp-content\/uploads\/2026\/02\/1-\u2116-377_2025.pdf\" target=\"_blank\" rel=\"noreferrer noopener\"><img loading=\"lazy\" decoding=\"async\" width=\"150\" height=\"44\" class=\"wp-image-853\" style=\"width: 150px;\" src=\"https:\/\/hydro-chemistry-ecology.knu.ua\/wp-content\/uploads\/2021\/07\/downloadable-pdf-button-png-hd-image-png-all-download-pdf-png-5256_1535.png\" alt=\"\" srcset=\"https:\/\/hydro-chemistry-ecology.knu.ua\/wp-content\/uploads\/2021\/07\/downloadable-pdf-button-png-hd-image-png-all-download-pdf-png-5256_1535.png 5256w, https:\/\/hydro-chemistry-ecology.knu.ua\/wp-content\/uploads\/2021\/07\/downloadable-pdf-button-png-hd-image-png-all-download-pdf-png-5256_1535-300x88.png 300w, https:\/\/hydro-chemistry-ecology.knu.ua\/wp-content\/uploads\/2021\/07\/downloadable-pdf-button-png-hd-image-png-all-download-pdf-png-5256_1535-1024x299.png 1024w, https:\/\/hydro-chemistry-ecology.knu.ua\/wp-content\/uploads\/2021\/07\/downloadable-pdf-button-png-hd-image-png-all-download-pdf-png-5256_1535-768x224.png 768w, https:\/\/hydro-chemistry-ecology.knu.ua\/wp-content\/uploads\/2021\/07\/downloadable-pdf-button-png-hd-image-png-all-download-pdf-png-5256_1535-1536x449.png 1536w, https:\/\/hydro-chemistry-ecology.knu.ua\/wp-content\/uploads\/2021\/07\/downloadable-pdf-button-png-hd-image-png-all-download-pdf-png-5256_1535-2048x598.png 2048w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/><\/a><\/p>\n\n\n\n<p>HOW TO CITE<\/p>\n\n\n\n<p>Khilchevskyi, V.K. (2025). Features of hydrography and water resources of Hungary. <em>Hidrolohiia, hidrokhimiia i hidroekolohiia<\/em> [Hydrology, Hydrochemistry and Hydroecology], 3(77), 6-18 (in Ukrainian, abstr. in English). https:\/\/doi.org\/10.17721\/2306-5680.2025.3.1<\/p>\n\n\n\n<p><\/p>\n","protected":false},"excerpt":{"rendered":"<p>DOI: https:\/\/doi.org\/10.17721\/2306-5680.2025.3.1 Hydrology, Hydrochemistry and Hydroecology. 2025. \u2116 3(77)Publication language: UkrainianAuthors:Khilchevskyi V.K., Taras Shevchenko National University of Kyiv The article is devoted to the study of hydrography and water resources of the territory of Hungary. The country&#8217;s hydrographic conditions are [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-2125","page","type-page","status-publish","hentry"],"translation":{"provider":"WPGlobus","version":"3.0.0","language":"en","enabled_languages":["uk","en"],"languages":{"uk":{"title":true,"content":true,"excerpt":false},"en":{"title":true,"content":true,"excerpt":false}}},"_links":{"self":[{"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/pages\/2125","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/comments?post=2125"}],"version-history":[{"count":2,"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/pages\/2125\/revisions"}],"predecessor-version":[{"id":2131,"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/pages\/2125\/revisions\/2131"}],"wp:attachment":[{"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/media?parent=2125"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}