Original Articles
Vol. 85 (2026)
The impact of climate change on the dynamics of the water level of Lake Skadar
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All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.
Published: 5 February 2026
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Lake Skadar is the largest freshwater body on the Balkan Peninsula. It is recognized as a wetland of international importance under the Ramsar Convention and holds the status of a national park in Montenegro. The results presented in this study indicate a significant downward trend in monthly water levels during the period 1948-2021, ranging from -14.9 cm in September to -24.0 cm per decade in May. Water levels show significant variation both seasonally and annually (cm per decade): from -16.8 (autumn) to -21.7 (spring), i.e., -19.3 (year). Standardized deviations suggest that the most pronounced decline began in 1981, a pattern further confirmed by the Rescaled Adjusted Partial Sums. Total precipitation in Lake Skadar's drainage basin has shown little to no change. However, there has been a significant increase in air temperature, and thus increased evaporation. According to ERA5-Land data, the annual total evaporation trend in the lake basin reaches up to 10.0 mm per decade. The substantial increase in evaporation has probably resulted in a significant reduction in runoff (Y) derived from precipitation contributing to stream flow. The trend of the mean annual runoff (Y) from 1 m2 is -45 mm per decade, and the flow of the Morača River, the main tributary of the lake, -2.5% per decade. Notably, over the past 14 years, Lake Skadar recorded both its highest water level (2010) and its lowest (2017). We appreciate that the long-term trend of falling water levels is influenced by significant warming of the atmosphere, which has led to increased water evaporation. Short-term fluctuations in lake water levels are primarily driven by variations in precipitation within the catchment area, which are likely linked to atmospheric oscillation patterns. In addition, human impact is evident near the confluence of the Morača River and Lake Skadar, particularly due to the intensive extraction of gravel and sand. To preserve the ecology and economy of Lake Skadar, its natural and cultural heritage, urgent measures are necessary by the countries (Montenegro and Albania) within whose territories this natural gem is located.
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Citations
Aladin NV, Plotnikov IS, Micklin P, Ballatore T, 2009. Aral Sea: Water level, salinity and long–term changes in biological communities of an endangered ecosystem–past, present and future. Natural Resources and Environmental Issues 15:177-183.
Blauhut V, Stoelzle M, Ahopelto L, Brunner MI, Teutschbein C, Wendt DE, et al., 2022. Lessons from the 2018–2019 European droughts: a collective need for unifying drought risk management. Nat Hazards Earth Syst Sci 22:2201-2217. DOI: https://doi.org/10.5194/egusphere-egu22-6146
Burić D, 2024. Detected and projected temperature changes in the area of mediterranean Montenegro. Geogr J 190:e12580. DOI: https://doi.org/10.1111/geoj.12580
Burić D, Doderović M, 2022. Trend of percentile climate indices in Montenegro in the period 1961-2020. Sustainability 14:12519. DOI: https://doi.org/10.3390/su141912519
Burić D, Doderović M, Dragojlović J, Penjišević I, 2021. Extreme weather and climate events in Montenegro – case study, November 2019. Weather 76:383-388. DOI: https://doi.org/10.1002/wea.3885
Burić D, Doderović M, Mihajlović J, Marčev A, Penjišević I, 2025. Changes in river flow in Mediterranean Montenegro and interaction with variations in atmospheric and oceanic oscillations. Pure Appl Geophys 182:2351-2371. DOI: https://doi.org/10.1007/s00024-025-03720-3
Burić D, Mihajlović J, Doderović M, Mijanović I, 2024a. Comparative analysis of SPI and SPEI drought indices for Montenegro and the impact of teleconnections. J Water Clim Chang 15:5149-5168. DOI: https://doi.org/10.2166/wcc.2024.238
Burić D, Mihajlović J, Ducić V, 2023a. Climatic regionalization of Montenegro by applying different methods of cluster analysis. Geogr Pannon 27:119-131. DOI: https://doi.org/10.5937/gp27-43776
Burić D, Mihajlović J, Luković J, Jandžiković B, Dragojlović J, 2024b. Deciphering the breaking points and spectral periodicities of mean air temperatures and precipitation sums in Montenegro. Environ Earth Sci 83:370. DOI: https://doi.org/10.1007/s12665-024-11666-3
Burić D, Mijanović I, Doderović M, Mihajlović J, Trbić G, 2023a. Assessment of the environmental quality of Lake Skadar and its urban surroundings in Montenegro. Eur J Geogr 14:76-87. DOI: https://doi.org/10.48088/ejg.d.bur.14.2.076.087
Burić D, Penjišević I, 2023. Southern Hemisphere temperature trend in association with greenhouse gases, El Niño Southern Oscillation, and Antarctic Oscillation. IDOJARAS 127:23-42. DOI: https://doi.org/10.28974/idojaras.2023.1.2
Dalla Torre D, Di Marco N, Menapace A, Avesani D, Righetti M, Majone B, 2024. Suitability of ERA5-Land reanalysis dataset for hydrological modelling in the Alpine region. J Hydrol Reg Studs 52:101718. DOI: https://doi.org/10.1016/j.ejrh.2024.101718
Doderović M, Burić D, Ducić V, Mijanović I, 2020. Recent and future air temperature and precipitation changes in the mountainous north of Montenegro. J Geogr Inste "Jovan Cvijic" SASA 70:189-201. DOI: https://doi.org/10.2298/IJGI2003189D
Doderović M, Burić D, Popović Lj, 2018. [Hidrologija kopna].[Book in Serbian]. Univerzitet Crne Gore, Podgorica. ISBN 978-86-7664-155-0
Dong H, Geng Y, Sarkis J, Fujita T, Okadera T, Xue B, 2013. Regional water footprint evaluation in China: A case of Liaoning. Sci Total Environ 442:215-224. DOI: https://doi.org/10.1016/j.scitotenv.2012.10.049
Dobricic M, Marjanovic P, 2017. Interaction between water protection and spatial planning. Water Res Manage 7:3-15.
Đurin B, Raič M, Sušilović P, 2022. Application of the RAPS method of time series analysis to the assessment of Grout Curtain performance in Karst - A case study of the hydro energy power plant (HEPP) Mostar Dam in Bosnia and Herzegovina. Hydrology 9:192. DOI: https://doi.org/10.3390/hydrology9110192
FAO, 2024. The state of the world’s forests 2024: Forest-sector innovations towards a more sustainable future. Available from: https://openknowledge.fao.org/items/ec487897-97b5-43ec-bc2e-5ddfc76c8e85
Garbrecht J, Fernandez GP, 1994. Visualization of trends and fluctuations in climatic records. Water Resour Bull 30:297-306. DOI: https://doi.org/10.1111/j.1752-1688.1994.tb03292.x
Government of Montenegro, 2017. [Water Management Strategy of Montenegro]. [Report in Montenegrin]. Ministry of Agriculture and Rural Development. Available from: https://faolex.fao.org/docs/pdf/mne228018.pdf
Gronewold DA, Rood BR, 2019. Recent water level changes across Earth's largest lake system and implications for future variability. J Great Lakes Res 45:1-3. DOI: https://doi.org/10.1016/j.jglr.2018.10.012
Gnjato S, Popov T, Ivanišević M, Trbić G, 2023. Long-term streamflow trends in Bosnia and Herzegovina (BH). Environ Earth Sci 82:356. DOI: https://doi.org/10.1007/s12665-023-11040-9
Gyau–Boakye P, Tumbulto J, 2000. The Volta Lake and declining rainfall and streamflows in the Volta River Basin. Environ Dev Sustain 2:1-11. DOI: https://doi.org/10.1023/A:1010020328225
Helsel DR, Hirsch RM, Ryberg KR, Archfield SA, Gilroy EJ, 2020. Statistical methods in water resources: U.S. Geological Survey Techniques and Methods. Reston, United States Geological Survey. DOI: https://doi.org/10.3133/tm4A3
Hering JG, 2019. Water: The environmental, technological, and societal complexity of a simple substance. In: P. A. Maurice (Ed.), Encyclopedia of water: science, technology, and society. Hoboken, J. Wiley & Sons. DOI: https://doi.org/10.1002/9781119300762.wsts0038
Hinegk L, Adami L, Piccolroaz S, Amadori M, Moretti M, Tubino M, Toffolon M, 2023. Multidecadal analysis of Lake Garda water balance. J Limnol 82:2144. DOI: https://doi.org/10.4081/jlimnol.2023.2144
Kaissi O, Belaqziz S, Kharrou M H, Erraki S, El Hachimi C, Amazirh A, Chehbouni A, 2024. Advanced learning models for estimating the spatio-temporal variability of reference evapotranspiration using in-situ and ERA5-Land reanalysis data. Model Earth Syst Environ 10:1915-1939. DOI: https://doi.org/10.1007/s40808-023-01872-6
Kayastha M B, Ye X, Huang C, Xue P, 2022. Future rise of the Great Lakes water levels under climate change. J Hydrol 612:128205. DOI: https://doi.org/10.1016/j.jhydrol.2022.128205
Kovačević-Majkić J, Urošev M, 2014. Trends of mean annual and seasonal discharges of rivers in Serbia. J Geogr Inst "Jovan Cvijic" SASA 64:143-160. DOI: https://doi.org/10.2298/IJGI1402143K
Kolokytha E, de Oliveira Galvão C, Teegavarapu RSV, 2017. Climate change impacts and water resource management and planning, pp. 283-295. In: E. Kolokytha, S. Oishi and R. Teegavarapu (eds.), Sustainable water resources planning and management under climate change. Springer. DOI: https://doi.org/10.1007/978-981-10-2051-3_11
Kraemer BM, Seimon A, Adrian R, McIntyre PB, 2020. Worldwide lake level trends and responses to background climate variation. Hydrol Earth Syst Sci 24:2593-2608. DOI: https://doi.org/10.5194/hess-24-2593-2020
Li L, Ni W, Li T, Zhou B, Qu Y, Yuan K, 2020. Influences of anthropogenic factors on lakes area in the Golmud Basin, China, from 1980 to 2015. Environ Earth Sci 79:20. DOI: https://doi.org/10.1007/s12665-019-8770-6
Luković J, Burić D, Mihajlović J, Pejović M, 2024. Spatial and temporal variations of aridity-humidity indices in Montenegro. Theor Appl Climatol 155:4553-4566. DOI: https://doi.org/10.1007/s00704-024-04893-y
Malamataris D, Kolokytha E, Loukas A, 2020. Integrated hydrological modelling of surface water and groundwater under climate change: the case of the Mygdonia basin in Greece. J Water Clim Chang 11:1429-1454. DOI: https://doi.org/10.2166/wcc.2019.011
Muñoz Sabater J, 2019. ERA5-Land monthly averaged data from 1950 to present. Accessed on: 24.04.2024. Avaial from: https://cds.climate.copernicus.eu/datasets/reanalysis-era5-land-monthly-means?tab=overview
Muñoz-Sabater J, Dutra E, Agustí-Panareda A, Albergel C, Arduini G, Balsamo G, et al., 2021. ERA5-Land: a state-of-the-art global reanalysis dataset for land applications. Earth Syst Sci Data 13:4349-4383 DOI: https://doi.org/10.5194/essd-13-4349-2021
Pešić V, Kostianoy AG, Soloviev DM, 2020. The impact of wildfires on the Lake Skadar/Shkodra environment. Ecol Montenegrina 37:57-65. DOI: https://doi.org/10.37828/em.2020.37.7
Institute for Hydrometeorology and Seismology of Montenegro, 2024. Database (1948-2021). Available from: http://www.meteo.co.me/
Radišić M, Rubinić J, Ružić I, Brozinčević A, 2021. Hydrological system of the Plitvice Lakes-Trends and changes in water levels, inflows, and losses. Hydrology 8:174. DOI: https://doi.org/10.3390/hydrology8040174
Ranzi R, Michailidi EM, Tomirotti M, Crespi A, Brunetti M, Maugeri M, 2021. A multi‐century meteo‐hydrological analysis for the Adda river basin (Central Alps). Part II: Daily runoff (1845-2016) at different scales. Int J Climatol 41:181-199. DOI: https://doi.org/10.1002/joc.6678
Rodell M, Famiglietti JS, Wiese DN, Reager JT, Beaudoing HK, Landerer FW, Lo M-H, 2018. Emerging trends in global freshwater availability. Nature 557:651–659. DOI: https://doi.org/10.1038/s41586-018-0123-1
Saidi H, Dresti C, Ciampittiello M, 2016. Fluctuations of Lake Orta water levels: preliminary analyses. J Limno 75:1230. DOI: https://doi.org/10.4081/jlimnol.2016.1230
Soria J, Apostolova N, 2022. Decrease in the water level of Lake Prespa (North Macedonia) studied by remote sensing methodology: relation with hydrology and agriculture. Hydrology 9:99. DOI: https://doi.org/10.3390/hydrology9060099
Szentimrey T, 2003. Multiple analysis of series for homogenization (MASH), Verification procedure for homogenized time series. Proc. 4th Seminar for homogenization and quality control in climatological databases, Budapest. WMO-TD No. 1236.
Šrajbek M, Đurin B, Sušilović P, Singh SK, 2023. Application of the RAPS method for determining the dependence of nitrate concentration in groundwater on the amount of precipitation. Earth 4:266-277. DOI: https://doi.org/10.3390/earth4020014
Yao F, Livneh B, Rajagoplan B, Wang J, Cretauh JF, Wada Y, Berge–Nguyen M, 2023. Satellites reveal widespread decline in global lake water storage. Science 380:743-749. DOI: https://doi.org/10.1126/science.abo2812
Yeboah KA, Akpoti K, Kabo-bah AT, Ofosu EA, Siabi EK, Mortey EM, Okyereh SA, 2022. Assessing climate change projections in the Volta Basin using the CORDEX–Africa climate simulations and statistical bias-correction. Environ Chall 6:100439. DOI: https://doi.org/10.1016/j.envc.2021.100439
Yücel A, Marković M, Atilgan A, Rolbiecki R, Ertop H, Jagosz B, et al., 2022. Investigation of annual lake water levels and water volumes with Şen innovation and Mann-Kendall rank correlation trend tests: example of Lake Eğirdir, Turkey. Water 14:2374. DOI: https://doi.org/10.3390/w14152374
Edited by
Marco Toffolon, Department of Civil, Environmental and Mechanical Engineering, University of Trento, ItalyCRediT authorship contribution
All authors made a substantive intellectual contribution, read and approved the final version of the manuscript and agreed to be accountable for all aspects of the work
Data Availability Statement
Data are available from the corresponding author on reasonable request
How to Cite
1.
Burić D, Doderović M, Penjišević I, Dragojlović J, Jandžiković B. The impact of climate change on the dynamics of the water level of Lake Skadar. J Limnol [Internet]. 2026 Feb. 5 [cited 2026 Feb. 11];85(1). Available from: https://www.jlimnol.it/jlimnol/article/view/2243
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