Abstract
Climate model simulations' outputs are prone to biases compared to observations; furthermore, climate projections can be very different in modelling future temperature characteristics. One possible solution for reducing uncertainty and eliminating possible systematic errors within climate projections is the bias-adjustment of the raw climate model data. We used the quantile mapping method for bias-adjustment of a mini ensemble consisting of 8-member high-resolution (0.11°) regional climate model simulations provided by the CORDEX community. As the method requires a reliable observational dataset serving as reference data, we used the quality controlled and homogenized observational dataset: CARPATCLIM. Quantile mapping bias-adjustment technique was applied on the following variables: daily mean, minimum and maximum temperature. We analysed changes in mean temperature characteristics and of climate indices for future periods of 2021–2050 and 2070–2099 with respect to the reference period 1976–2005 for the Carpathian Region. The selected climate indices are based on minimum (frost days, FD) and maximum daily temperature data (summer days, SU). Our bias-adjusted RCM results suggest a similar degree of mean temperature change as the raw RCMs' data. Bias-adjusted and raw RCM data project a remarkable annual temperature increase on average under the RCP8.5 scenario (1.4°C and 3.9°C by 2021–2050 and 2070–2099, respectively). The highest temperature increase is likely to occur in summer: it is 4.3°C on average by the end of the 21st century. More pronounced differences were found for the projected changes of the number of summer and frost days based on the bias-adjusted and the raw RCM data. Our results draw attention to the fact that bias-adjusted RCM data are crucial for the provision of regional climate change impact and adaptation studies for the Carpathian Region.
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Torma, C. Z., & Kis, A. (2022). Bias-adjustment of high-resolution temperature CORDEX data over the Carpathian region: Expected changes including the number of summer and frost days. International Journal of Climatology, 42(12), 6631–6646. https://doi.org/10.1002/joc.7654
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