Royal Dutch Meteorological Institute; Ministery Of Infrastructure And The Environment

Publications, presentations and other activities
The Impact of Meteorological and Hydrological Memory on Compound Peak Flows in the Rhine River Basin
by S. Khanal (Future Water), A. Lutz (Future Water), W. Immerzeel (Future Water), H. de Vries (KNMI), N. Wanders (Utrecht University)B.J.J. van den Hurk (KNMI)

Spatio-temporal variation of hydrological processes that have a strong lagged autocorrelation (memory), such as soil moisture, snow accumulation and the antecedent hydro-climatic conditions, significantly impact the peaks of flood waves. Ignoring these memory processes leads to biased estimates of floods and high river levels that are sensitive to the occurrence of these compounding hydro-meteorological processes. Here, we investigate the role of memory in hydrological and meteorological systems at different temporal scales for the Rhine basin. We simulate the hydrological regime of the Rhine river basin using a distributed hydrological model (SPHY) forced with 19502000 atmospheric conditions from an ensemble simulation with a high resolution (0.11/12 km) regional climate model (RACMO2). The findings show that meltwater from antecedent anomalous snowfall results in a time shift of the discharge peak. Soil moisture modulates the rainfall-runoff relationship and generates a strong runoff response at high soil moisture levels and buffers the generation of runoff peaks at low levels. Additionally, our results show that meteorological autocorrelation (manifesting itself by the occurrence of clustered precipitation events) has a strong impact on the magnitude of peak discharge. Removing meteorological autocorrelation at time scales longer than five days reduces peak discharge by 80% relative to the reference climate. At time scales longer than 30 days this meteorological autocorrelation loses its significant role in generating high discharge levels

Bibliographic data
Khanal, S., A. Lutz, W. Immerzeel, H. de Vries, N. Wanders and B.J.J. van den Hurk, The Impact of Meteorological and Hydrological Memory on Compound Peak Flows in the Rhine River Basin
Atmosphere, 2019, 10, 4, 171, doi:10.3390/atmos10040171.
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