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Earth Syst. Dynam., 8, 405-418, 2017
https://doi.org/10.5194/esd-8-405-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
14 Jun 2017
Evaluating the atmospheric drivers leading to the December 2014 flood in Schleswig-Holstein, Germany
Nils H. Schade Federal Maritime and Hydrographic Agency (BSH), 20359 Hamburg, Germany
Abstract. Regional analyses of atmospheric conditions that may cause flooding of important transport infrastructure (railway tracks, highways/roads, rivers/channels) and subsequent adaptation measures are part of topic 1 of the network of experts initiated by the German Federal Ministry of Transport and Digital Infrastructure (BMVI). As an example case study, the December 2014 flood in Schleswig-Holstein, Germany, was investigated. Atmospheric conditions at the onset of the flood event are described and evaluated with respect to the general weather circulation, initial wetness, and event precipitation. Persistent, predominantly westerly general weather circulations (GWCs) directed several low-pressure systems over the North Sea to Schleswig-Holstein during December 2014, accompanied by prolonged rainfall and finally a strong precipitation event in southern Schleswig-Holstein, causing several inland gauges to exceed their, by then maximum, water levels. Results show that the antecedent precipitation index (API) is able to reflect the soil moisture conditions and, in combination with the maximum 3-day precipitation sum (R3d), to capture the two main drivers finally leading to the flood: (1) the initial wetness of north-western Schleswig-Holstein and (2) strong event precipitation in southern and eastern Schleswig-Holstein from 21 to 23 December; at the same time, both indices exceeded their respective 5-year return periods. Further, trend analyses show that both API and R3d have been increasing during recent years, while regional patterns match the north-eastward shift of cyclone pathways, leading to a higher risk of flooding in Schleswig-Holstein. Within the network of experts, investigations of these and further indices/drivers for earth system changes (e.g. wind surge and sea level rise) derived from observations, reanalyses, and regional climate model data are planned for all German coastal areas. Results can be expected to lead to improved adaptation measures to floods under climate change conditions wherever catchments have to be drained and infrastructures and ecosystems may be harmed.

Citation: Schade, N. H.: Evaluating the atmospheric drivers leading to the December 2014 flood in Schleswig-Holstein, Germany, Earth Syst. Dynam., 8, 405-418, https://doi.org/10.5194/esd-8-405-2017, 2017.
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Short summary
Atmospheric conditions at the onset of the December 2014 flood in Schleswig-Holstein, Germany, are described. Results show that the antecedent precipitation index (API) is able to reflect soil moisture conditions and, in combination with the maximum 3–day precipitation sum (R3d), to capture the main drivers ultimately leading to this flood. Trend analyses indicate an increasing risk of flood-prone situations over the last decades in this region. Further analyses are planned at the German coasts.
Atmospheric conditions at the onset of the December 2014 flood in Schleswig-Holstein, Germany,...
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