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The impact of bias correcting regional climate model results on hydrological indicators for Bavarian catchments
被引:33
|作者:
Willkofer, Florian
[1
]
Schmid, Franz-Josef
[1
]
Komischke, Holger
[2
]
Korck, Jane
[2
]
Braun, Marco
[3
]
Ludwig, Ralf
[1
]
机构:
[1] Ludwig Maximilian Univ Munchen, Dept Geog, Luisenstr 37, D-80333 Munich, Germany
[2] Bavarian Environm Agcy LfU, Hans Hogn Str 12, D-95030 Hof, Germany
[3] Ouranos, 550 Rue Sherbrooke West,West Tower,19th Floor, Montreal, PQ H3A 1B9, Canada
关键词:
Bias correction;
Regional climate model;
Climate change signal;
Hydrological modeling;
Runoff indicators;
Bavaria;
PART II;
PRECIPITATION;
SIMULATIONS;
RIVER;
D O I:
10.1016/j.ejrh.2018.06.010
中图分类号:
TV21 [水资源调查与水利规划];
学科分类号:
081501 ;
摘要:
Study region: The Mindel river catchment, gauge Offingen, Bavaria, Germany. Study focus: The study investigates the potential interference of climate change signals (CCS) in hydrological indicators due to the application of bias correction (BC) of regional climate models (RCM). A validated setup of the hydrological model WaSiM was used for runoff modeling. The CCS, gained by the application of three RCMs (CCLM, REMO-UBA, RACMO2) for a reference period (1971-2000) and a scenario period (2021-2050), are evaluated according to eight hydrological indicators derived from modeled runoff. Three different BC techniques (linear scaling, quantile mapping, local intensity scaling) are applied. New hydrological insights for the region: Runoff indicators are calculated for the investigated catchment using bias corrected RCM data. The quantile mapping approach proves superior to linear scaling and local intensity scaling and is recommended as the bias correction method of choice when assessing climate change impacts on catchment hydrology. Extreme flow indicators (high flows), however, are poorly represented by any bias corrected model results, as current approaches fail to properly capture extreme value statistics. The CCS of mean hydrological indicator values (e.g. mean flow) is well preserved by almost every BC technique. For extreme indicator values (e.g. high flows), the CCS shows distinct differences between the original RCM and BC data.
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页码:25 / 41
页数:17
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