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Venetsanou P.1,2, Lazoglou G.3, Anagnostopoulou C.4, Voudouris K.1,5 Thessaloniki, Greece 2Energy, Environment and Water Research Center, The Cyprus Institute, 2121 Nicosia, Cyprus saloniki, Greece Abstract: During the last decades, climate change impacts on hydrology have been assessed by coupling the Regional correction methods were developed to overcome this issue. In this paper, the delta change, the linear scaling, and the empirical quantile mapping were applied to climate input data to a semi distributed hydrological model. The Regional simulation was enhanced after the bias correction methods application. The discrepancies in simulated and observed precipitation, temperature). 1 Introduction The most common approach to assessing future climate change impacts on hydrological processes involves the coupling are directly nested to the hydrological models. The present paper deals with the evaluation of the ability of the bias correction methods to reasonably simulate the watershed hydrological simulation under climate change conditions. The watershed simulation was carried out by the Soil watershed process modeling, namely those that correspond to the water balance, crop growth, quality land management river basin. It is an agricultural and touristic watershed situated in Halkidiki (Greece), surrounded by Taxiarchis, Plana and Ormylia villages, covering an area of 472 km2 Climate dynamics / Climate change type. Regarding the land use, the Havrias river basin is mainly occupied by olive groves, broad-leaved, coniferous and tered in the coastal part and host a multiple-layer aquifer system with high permeability and productivity. This aquifer on water, sediment, and agricultural chemical yields at a watershed scale. Based on the morphological characteristics, the watershed is divided into sub- watersheds. Then, each sub-watershed is copernicus.eu/pan-european/corine-land-cover/clc-2018). The soil map was created by the laboratory soil tests results, Fig. 1. The morphological map of the Havrias River basin. mate data. Daily precipitation, maximum and minimum air temperature, solar radiation, wind speed and relative humid- The investigation of the climate change impacts on the hydrological watershed process was conducted by driving the - Climate dynamics / Climate change al. 2015; Shrestha et al. 2017). The fundamental basis of these methods is to transfer the mean change signal between the period 1981-1990 was selected as training period. 3 Results and Discussion 3.1 ArcSWAT Application - - - by this method. It might be attributed to its ability to perform the most essential improvement of the precipitation. Based tion. Fig. 2 and the bias correction methods. Climate dynamics / Climate change Table 1. Water balance. 4 Conclusions In the present paper, an attempt was made to investigate the capability of the bias correction methods to reasonably simulate the climate change impacts on the watershed hydrological process. For this scope the delta change, the linear The evaluation of the bias corrected hydrological results showed that the bias correction methods reasonably represent - cal parameter. References 1508. - 7619- 8. - w12020482. - Climate dynamics / Climate change - 020-03130-6. Climate dynamics / Climate change