{"id":1874,"date":"2025-01-14T14:20:28","date_gmt":"2025-01-14T11:20:28","guid":{"rendered":"https:\/\/hydro-chemistry-ecology.knu.ua\/?page_id=1874"},"modified":"2025-01-14T14:22:19","modified_gmt":"2025-01-14T11:22:19","slug":"%d0%b3%d0%be%d0%bf%d1%86%d1%96%d0%b9-%d0%bc-%d0%b2-%d0%b1%d0%be%d0%bd%d0%b4%d0%b0%d1%80%d0%b5%d0%bd%d0%ba%d0%be-%d0%b0-%d1%94-%d0%bc%d1%96%d0%b6%d1%80%d1%96%d1%87%d0%bd%d0%b0-%d0%bc%d1%96%d0%bd","status":"publish","type":"page","link":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/%d0%b3%d0%be%d0%bf%d1%86%d1%96%d0%b9-%d0%bc-%d0%b2-%d0%b1%d0%be%d0%bd%d0%b4%d0%b0%d1%80%d0%b5%d0%bd%d0%ba%d0%be-%d0%b0-%d1%94-%d0%bc%d1%96%d0%b6%d1%80%d1%96%d1%87%d0%bd%d0%b0-%d0%bc%d1%96%d0%bd\/","title":{"rendered":"GOPTSIY M.V., BONDARENKO A.YE. INTERANNUAL VARIABILITY OF FLOOD RUNOFF IN THE TETERIV RIVER BASIN OVER A MULTI-YEAR PERIOD"},"content":{"rendered":"\n<p><strong>DOI: <a href=\"https:\/\/doi.org\/10.17721\/2306-5680.2024.3.4\">https:\/\/doi.org\/10.17721\/2306-5680.2024.3.4<\/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-3\/\" data-type=\"link\" data-id=\"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-3\/\">Hydrology, Hydrochemistry and Hydroecology. 2024. \u2116 3 (73)<\/a><br><strong>Publication language: <\/strong>Ukrainian<br><strong>Authors:<br><\/strong>Goptsiy M.V., Odesa Mechnikov National University, Taras Shevchenko National University of Kyiv<br>Bondarenko A.Ye., Odesa Mechnikov National University<\/p>\n\n\n\n<p><em>The article analyzes the interannual variability of flood runoff in the Teteriv River basin over a long period of observation. The rivers of the studied basin are characterized as flat with a pronounced spring flood. The river is of important water management importance for the Zhytomyr and Kyiv regions and is a source of drinking water for a number of settlements, including the cities of Zhytomyr and Korostyshiv. Its waters are also used for industrial needs, in particular by enterprises operating along its banks. The nature of the river&#8217;s water regime is largely determined by the characteristics of the spring flood, its duration and the percentage ratio in the annual runoff, which is determined by the type of feeding. The highest average monthly water flows are observed in March-April. The duration of the spring flood is 1.5-2 months. The volume of spring runoff of the rivers of the studied region constitutes the main part of the total runoff in most of the years considered.<\/em><br><em>Generalizations of the studied characteristics of spring runoff are presented, which are based on data for a multi-year period up to 2020, inclusive, based on the hydrological-genetic method of analysis of runoff series.<\/em><br><em>According to the constructed difference-integral curves of the time series of maximum spring flood water discharges in recent decades (starting from 1980), a long low-water phase is noted, and before that, a long high-water phase was noted from the beginning of observations. While for the runoff layers, we have a slightly different course of change in water content phases, where over the past 40 years we have a low-water phase from 1981-82 to 1994-95, and then a high-water phase to 2005-2006, and again a low-water phase.<\/em><br><em>In the series of the largest water flows of the spring flood, a significant downward trend in the values of the runoff is noted in all considered series, except for the Teteriv River &#8211; Ivankiv Township. While in the series of the layers of the spring flood runoff, we have an insignificant trend in the series: the Teteriv River &#8211; Troscha, the Teteriv River &#8211; Ivankiv and the Irsha River &#8211; Volodarsk-Volynskyi; in all other series, a negative trend in the value of the runoff is noted.<\/em><br><em>Analysis of the interannual variability of the spring flood volumes showed that on average, according to modern data, 32-44% is formed with an average flood duration of 39-60 days, and not 45-60%, as noted in many scientific works that summarized shorter observation data that did not cover the long low-water phase on the rivers of the region in recent years.<\/em><\/p>\n\n\n\n<p><strong><em>Key words:<\/em><\/strong><em> spring runoff, Teteriv River, runoff variability, flood, statistical characteristics.<\/em><em><\/em><\/p>\n\n\n\n<p><strong>References<\/strong>:<br>1. Ovcharuk V.A. Maksymalnyi stik vesnianoho vodopillia rivnynnykh richok Ukrainy [Maximum spring runoff of lowland rivers of Ukraine] : monohrafiia. Odesa: Vydavnychyi dim \u00abHelvetyka\u00bb, 2020. 300s.<br>2. Ekstremalni hidrolohichni yavyshcha: pavodky i posukhy na terytorii hirskykh rehioniv Ukrainy [Extreme hydrological phenomena: floods and droughts in the mountainous regions of Ukraine] \/ za red. Hopchenka Ye.D.: monohrafiia. Odesa: TES,&nbsp; 2018. 324 s.<br>3. Hopchenko Ye.D., Ovcharuk V.A., Goptsiy M.V., Todorova O.I. Statystychni parametry chasovykh riadiv maksymalnoho stoku vesnianoho vodopillia v baseini Dnipra v umovakh minlyvosti klimatu [Statistical parameters of time series of maximum spring flood discharge in the Dnieper basin under conditions of climate variability]. Hidrolohiia, hidrokhimiia i hidroekolohiia, 2018. T. 4(51). S. 47-55.<br>4. Horbachova L.O., Barandich S.L. Prostorovo-chasova minlyvist maksymalnoho stoku vody vesnianoho vodopillia ta pavodkiv zmishanoho pokhodzhennia richok Ukrainy [Spatio-temporal variability of maximum spring flood discharge and mixed origin floods of rivers of Ukraine]. Nauk. pratsi UkrNDHMI. 2016. Vyp. 269. S. 107- 114.<br>5. Zvit pro NDR \u00abNaukovo-metodychna baza dlia vstanovlennia rozrakhunkovykh kharakterystyk vesnianoho vodopillia v baseini Dnipra v umovakh minlyvosti klimatu (ostatochnyi)\u00bb [Scientific and methodological basis for establishing estimated characteristics of spring flood discharge in the Dnieper basin under conditions of climate variability] DR \u2116 0117U002424, nauk., keriv. Hopchenko, Ye.D., 2019. ODEKU, Odesa. 755 s.<br>6. Shakirzanova Zh.R., Boiko V.M., Goptsiy M.V., Todorova O.I., Dokus A.O., Serbova Z.F., Shvets N.M. Metod prohnostychnoi otsinky kharakterystyk maksymalnoho stoku richok baseinu Dnipra u vesnianyi period roku. [Method for predictive assessment of characteristics of maximum river discharge of the Dnieper basin in the spring period of the year] Ukrainskyi hidrometeorolohichnyi zhurnal. 2018. T. 22. S. 80-99.<br>7. Metodyky hidrohrafichnoho ta vodohospodarskoho raionuvannia terytorii Ukrainy vidpovidno do vymoh Vodnoi ramkovoi dyrektyvy Yevropeiskoho Soiuzu [Methods of hydrographic and water management zoning of the territory of Ukraine in accordance with the requirements of the Water Framework Directive of the European Union] \/ Hrebin V.V. ta in. Kyiv : Interpres, 2013. 55 s.<br>8. Vyshnevskyi V.I. Richky i vodoimy Ukrainy. Stan i vykorystannia [Rivers and reservoirs of Ukraine. State and use] : monohrafiia. Kyiv : Vipol, 2000. 376 s.<br>9. Horbachova L.O. Suchasnyi vnutrishnorichnyi rozpodil vodnoho stoku richok Ukrainy [Modern intra-annual distribution of water discharge of rivers of Ukraine]. Ukrainskyi heohrafichnyi zhurnal, 2015, \u2116 3 S. 16-23.<br>10. Horbachova L.O. Hidroloho-henetychnyi analiz prostorovo-chasovykh zakonomirnostei vodnoho stoku richok Ukrainy: metodolohiia, tendentsii, prohnoz [Hydrogenetic analysis of spatio-temporal patterns of water discharge of rivers of Ukraine: methodology, trends, forecast] : dys&#8230; d-ra heohr. nauk. Kyiv: 2017. 399 s.<br>11. Vyshnevskyi V. I., Kosovets O. O. Hidrolohichni kharakterystyky richok Ukrainy [Hydrological characteristics of rivers of Ukraine]. Kyiv, 2003. 324 s.<br>12. Lukianets O. I., Obodovskyi O. H., Hrebin V.V., Pochaievets O.O., Korniienko V.O. Prostorovi zakonomirnosti zminy serednoho richnoho stoku vody richok Ukrainy [Spatial patterns of changes in the average annual water flow of rivers of Ukraine]. Ukrainskyi heohrafichnyi zhurnal,&nbsp; 2021.Vyp. 1(113) S. 6-14.<br>13. Hidrolohichni rozrakhunky [Hydrological calculations] : pidruchnyk \/ za red. Ye.D. Hopchenko, N.S. Loboda, V.A. Ovcharuk. Odesa: TES, 2014. 484 s.<br>14. Bondarenko A.Ye. Formuvannia maksymalnoho stoku na richkakh baseinu r. Teteriv [Formation of maximum flow on rivers of the Teteriv River basin] \/\/ Materialy studentskoi naukovoi konferentsii Odeskoho derzhavnoho ekolohichnoho universytetu, 10-17 travnia 2023r. Odesa: ODEKU. 2023. S. 432-433.<br>15. Bondarenko A.Ye. Statystychni parametry kharakterystyk maksymalnoho stoku na richkakh baseinu r. Teteriv [Statistical parameters of the characteristics of maximum flow on rivers of the Teteriv River basi] \/\/ Materialy studentskoi naukovoi konferentsii Odeskoho derzhavnoho ekolohichnoho universytetu, 10-19 kvitnia 2024 r. Odesa : ODEKU. 2024. S. 108-109.<br>16. Goptsiy M.V., Bondarenko A.Ye. Otsinka velychyny ta minlyvosti vesnianoho stoku v baseini r. Teteriv. Materialy mizhnarodnoi naukovo-praktychnoi konferentsii [Assessment of the magnitude and variability of spring flow in the Teteriv River basin]: Pryrodnycho-heohrafichni doslidzhennia reliefu, klimatu ta poverkhnevykh vod: suchasnyi stan ta perspektyvy rozvytku (do 75-richchia kafedr KNUTSh: zemleznavstva ta heomorfolohii; meteorolohii ta klimatolohii; hidrolohii ta hidroekolohii). 2-4 zhovtnia 2024 r. Kyiv, 2024. S. 16-17.<br>17. Hrebin V. V. Suchasnyi vodnyi rezhym richok Ukrainy (landshaftno-hidrolohichnyi analiz) [Modern water regime of rivers of Ukraine (landscape and hydrological analysis)] : monohrafiia. Kyiv: Nika-Tsentr, 2010. 316 s.<\/p>\n\n\n\n<p><a href=\"https:\/\/hydro-chemistry-ecology.knu.ua\/wp-content\/uploads\/2025\/01\/4_-\u0413\u0413\u0413-\u2116373_2024.pdf\" data-type=\"link\" data-id=\"https:\/\/hydro-chemistry-ecology.knu.ua\/wp-content\/uploads\/2025\/01\/4_-\u0413\u0413\u0413-\u2116373_2024.pdf\" target=\"_blank\" rel=\"noreferrer noopener\">READ THE FULL ARTICLE<br><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>Goptsiy, M.V., Bondarenko, A.Ye. (2024). Interannual variability of flood runoff in the Teteriv River basin over a multi-year period. <em>Hidrolohiia, hidrokhimiia i hidroekolohiia<\/em> [Hydrology, Hydrochemistry and Hydroecology], 3 (73), 37-49 (in Ukrainian, abstr. in English). https:\/\/doi.org\/10.17721\/2306-5680.2024.3.4<\/p>\n","protected":false},"excerpt":{"rendered":"<p>DOI: https:\/\/doi.org\/10.17721\/2306-5680.2024.3.4 Hydrology, Hydrochemistry and Hydroecology. 2024. \u2116 3 (73)Publication language: UkrainianAuthors:Goptsiy M.V., Odesa Mechnikov National University, Taras Shevchenko National University of KyivBondarenko A.Ye., Odesa Mechnikov National University The article analyzes the interannual variability of flood runoff in the Teteriv [&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-1874","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\/1874","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=1874"}],"version-history":[{"count":2,"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/pages\/1874\/revisions"}],"predecessor-version":[{"id":1877,"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/pages\/1874\/revisions\/1877"}],"wp:attachment":[{"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/media?parent=1874"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}