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| 001 | 851423 | ||
| 005 | 20210121101111.0 | ||
| 024 | 7 | _ | |a 10.1007/s00382-018-4147-x |2 doi |
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| 037 | _ | _ | |a FZJ-2018-05070 |
| 041 | _ | _ | |a English |
| 082 | _ | _ | |a 550 |
| 100 | 1 | _ | |a Knist, Sebastian |0 P:(DE-Juel1)158027 |b 0 |e Corresponding author |
| 245 | _ | _ | |a Evaluation and projected changes of precipitation statistics in convection-permitting WRF climate simulations over Central Europe |
| 260 | _ | _ | |a Berlin |c 2020 |b Springer |
| 336 | 7 | _ | |a article |2 DRIVER |
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| 520 | _ | _ | |a We perform simulations with the WRF regional climate model at 12 and 3 km grid resolution for the current and future climates over Central Europe and evaluate their added value with a focus on the daily cycle and frequency distribution of rainfall and the relation between extreme precipitation and air temperature. First, a 9 year period of ERA-Interim driven simulations is evaluated against observations; then global climate model runs (MPI-ESM-LR RCP4.5 scenario) are downscaled and analyzed for three 12-year periods: a control, a mid-of-century and an end-of-century projection. The higher resolution simulations reproduce both the diurnal cycle and the hourly intensity distribution of precipitation more realistically compared to the 12 km simulation. Moreover, the observed increase of the temperature–extreme precipitation scaling from the Clausius–Clapeyron (C–C) scaling rate of ~ 7% K−1 to a super-adiabatic scaling rate for temperatures above 11 °C is reproduced only by the 3 km simulation. The drop of the scaling rates at high temperatures under moisture limited conditions differs between sub-regions. For both future scenario time spans both simulations suggest a slight decrease in mean summer precipitation and an increase in hourly heavy and extreme precipitation. This increase is stronger in the 3 km runs. Temperature–extreme precipitation scaling curves in the future climate are projected to shift along the 7% K−1 trajectory to higher peak extreme precipitation values at higher temperatures. The curves keep their typical shape of C–C scaling followed by super-adiabatic scaling and a drop-off at higher temperatures due to moisture limitation. |
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| 700 | 1 | _ | |a Goergen, Klaus |0 P:(DE-Juel1)156253 |b 1 |
| 700 | 1 | _ | |a Simmer, Clemens |0 0000-0003-3001-8642 |b 2 |
| 770 | _ | _ | |a Convection permitting climate modelling |
| 773 | _ | _ | |a 10.1007/s00382-018-4147-x |0 PERI:(DE-600)1471747-5 |p 325-341 |t Climate dynamics |v 55 |y 2020 |x 0930-7575 |
| 856 | 4 | _ | |u https://juser.fz-juelich.de/record/851423/files/KnistS2018a.pdf |y OpenAccess |
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