Articles | Volume 30, issue 12
https://doi.org/10.5194/hess-30-3903-2026
https://doi.org/10.5194/hess-30-3903-2026
Research article
 | 
24 Jun 2026
Research article |  | 24 Jun 2026

Assessing future streamflow in Cyprus through hydrological model calibration under non-stationary climate and regional climate model ensemble selection

Ioannis Sofokleous, George Zittis, Gerald Dörflinger, and Adriana Bruggeman

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Cited articles

Asadieh, B. and Krakauer, N. Y.: Global change in streamflow extremes under climate change over the 21st century, Hydrol. Earth Syst. Sci., 21, 5863–5874, https://doi.org/10.5194/hess-21-5863-2017, 2017. 
Bağçaci, S. Ç., Yucel, I., Duzenli, E., and Yilmaz, M. T.: Intercomparison of the expected change in the temperature and the precipitation retrieved from CMIP6 and CMIP5 climate projections: A Mediterranean hot spot case, Turkey, Atmos. Res., 256, 105576, https://doi.org/10.1016/j.atmosres.2021.105576, 2021. 
Broderick, C., Matthews, T., Wilby, R. L., Bastola, S., and Murphy, C.: Transferability of hydrological models and ensemble averaging methods between contrasting climatic periods, Water Resour. Res., 52, 8343–8373, https://doi.org/10.1002/2016WR018850, 2016. 
Camera, C., Bruggeman, A., Hadjinicolaou, P., Pashiardis, S., and Lange, M. A.: Evaluation of interpolation techniques for the creation of gridded daily precipitation (1×1 km2); Cyprus, 1980–2010, J. Geophys. Res.-Atmos., 119, 693–712, https://doi.org/10.1002/2013JD020611, 2014. 
Camera, C., Zomeni, Z., Noller, J. S., Zissimos, A. M., Christoforou, I. C., and Bruggeman, A.: A high resolution map of soil types and physical properties for Cyprus: A digital soil mapping optimization, Geoderma, 285, 35–49, https://doi.org/10.1016/j.geoderma.2016.09.019, 2017. 
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Short summary
We developed a new method to improve numerical models that predict future water availability under climate change. The method works across different regions and climate scenarios. Applying the method to mountain river basins in the Eastern Mediterranean island of Cyprus showed that streamflow could drop by 39 % on average between 2030 and 2060, and by up to 70 % during the driest years. These findings help support better water planning in a changing climate.
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