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The current work addresses one of the key building blocks towards an improved understanding of flood processes and associated changes in flood characteristics and regimes in Europe: the development of a comprehensive, extensive European flood database. The presented work results from ongoing cross-border research collaborations initiated with data collection and joint interpretation in mind. A detailed account of the current state, characteristics and spatial and temporal coverage of the European Flood Database, is presented. At this stage, the hydrological data collection is still growing and consists at this time of annual maximum and daily mean discharge series, from over 7000 hydrometric stations of various data series lengths. Moreover, the database currently comprises data from over 50 different data sources. The time series have been obtained from different national and regional data sources in a collaborative effort of a joint European flood research agreement based on the exchange of data, models and expertise, and from existing international data collections and open source websites. These ongoing efforts are contributing to advancing the understanding of regional flood processes beyond individual country boundaries and to a more coherent flood research in Europe.

Climate change has led to concerns about increasing river floods resulting from the greater water-holding capacity of a warmer atmosphere 1 . These concerns are reinforced by evidence of increasing economic losses associated with flooding in many parts of the world, including Europe 2 . Any changes in river floods would have lasting implications for the design of flood protection measures and flood risk zoning. However, existing studies have been unable to identify a consistent continental-scale climatic-change signal in flood discharge observations in Europe 3 , because of the limited spatial coverage and number of hydrometric stations. Here we demonstrate clear regional patterns of both increases and decreases in observed river flood discharges in the past five decades in Europe, which are manifestations of a changing climate. Our results-arising from the most complete database of European flooding so far-suggest that: increasing autumn and winter rainfall has resulted in increasing floods in northwestern Europe; decreasing precipitation and increasing evaporation have led to decreasing floods in medium and large catchments in southern Europe; and decreasing snow cover and snowmelt, resulting from warmer temperatures, have led to decreasing floods in eastern Europe. Regional flood discharge trends in Europe range from an increase of about 11 per cent per decade to a decrease of 23 per cent. Notwithstanding the spatial and temporal heterogeneity of the observational record, the flood changes identified here are broadly consistent with climate model projections for the next century 4,5 , suggesting that climate-driven changes are already happening and supporting calls for the consideration of climate change in flood risk management.

Background: In a single-center study, we compared to what extent changes in conventional and ambulatory blood pressure (BP) predicted regression of left ventricular mass (LVM) index in response to antihypertensive treatment in previously untreated and treated patients with sustained hypertension., Methods and Results: We enrolled 173 black African patients who, off treatment, had a daytime diastolic BP ranging from 90 to 114 mm Hg. Antihypertensive drugs were titrated and combined to reduce the daytime diastolic BP below 90 mm Hg. Echocardiograms were obtained at baseline and follow-up. Mean systolic/diastolic clinic BP, 24-hour BP, and LVM index were similar in previously untreated (n=64) and previously treated (n=109) patients and averaged 171/102 mm Hg, 151/97 mm Hg, and 118 g/m2, respectively. At 4 months, these values had decreased (P<0.001) by 26/12 mm Hg, 23/14 mm Hg, and 14 g/m2 in previously untreated patients and by 22/9 mm Hg, 21/13 mm Hg, and 19 g/m2 in previously treated patients. In the previously untreated patients, the regression in LVM index correlated to a similar degree (P=0.09) with the decreases in the conventional (r=0.34; P=0.005) and the 24-hour (r=0.26; P=0.04) systolic BP. In the previously treated patients, the corresponding correlations were 0.02 (P=0.82) and -0.10 (P=0.32), respectively. Compared with the 24-hour systolic BP, automated oscillometric measurements of systolic BP obtained at the clinic yielded similar results., Conclusions: In previously untreated patients with sustained hypertension followed at a single center, reductions in clinic and ambulatory systolic pressure in response to antihypertensive treatment equally predicted the regression in LVM index.