This paper investigates the climate change effects on the hydrological and meteorological parameters of the Navrood Basin (a Caspian Hyrcanian forest watershed) in the north of Iran. Outputs of seven CMIP6 GCMs (Tmin, Tmax, and precipitation) under two scenarios, SSP2-4.5 and SSP5-8.5, were utilized. This study considered the historical period (1994 to 2014), the near future (2025 to 2049), the middle future (2050 to 2074), and the far future (2075 to 2099). The EDCDFm and MBA methods were used for bias correction of the outputs of GCMs and combine GCMs, respectively. The LARS-WG model was used for statistical downscaling. The IHACRES model calculated the runoff. The annual Tmin under SSP2-4.5 and SSP5-8.5 will increase 1.04 °C and 1.25 °C in the near future, 1.55 °C and 2.48 °C in the middle future and, 2.09 °C and 4.11 °C in the far future, respectively. The annual Tmax under SSP2-4.5 and SSP5-8.5 will increase 1.59 °C and 1.38 °C in the near future, 1.98 °C and 3.02 °C in the middle future and, 2.58 °C and 4.94 °C in the far future, respectively. The annual precipitation (PCP) under SSP2-4.5 and SSP5-8.5 will increase 6.81% and 7.11% in the near future, 6.15% and 4.43% in the middle future, 8.63% and 6.58% in the far future, respectively. Finally, the annual runoff under SSP2-4.5 and SSP5-8.5 will increase 16.3% and 15.4% in the near future, 14.8% and 10.6% in the middle future and, 19.2% and 15.1% in the far future, respectively.