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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.

A warming climate is expected to have an impact on the magnitude and timing of river floods; however, no consistent large-scale climate change signal in observed flood magnitudes has been identified so far. We analyzed the timing of river floods in Europe over the past five decades, using a pan-European database from 4262 observational hydrometric stations, and found clear patterns of change in flood timing. Warmer temperatures have led to earlier spring snowmelt floods throughout northeastern Europe; delayed winter storms associated with polar warming have led to later winter floods around the North Sea and some sectors of the Mediterranean coast; and earlier soil moisture maxima have led to earlier winter floods in western Europe. Our results highlight the existence of a clear climate signal in flood observations at the continental scale., (Copyright © 2017 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works.)

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.

The alpha-adducin gene contributes significantly to hypertension in MHS rats (rats of the Milan hypertensive strain) and in some white and Japanese populations, causing a low renin, sodium, and diuretic-sensitive hypertension. No data are available from populations of African ancestry who have a high prevalence of low renin, sodium, and diuretic-sensitive hypertension. We studied the relationship between the 460-Trp variant of alpha-adducin gene with hypertension using a case-control study design in black South Africans. Surprisingly we found that the overall frequency of the 460-Trp allele was low (approximately 6%), but in spite of such relatively low frequency, the 460-Trp allele was 2.5-fold more frequent in hypertensives than normotensives (P = .028), with an odds ratio for hypertension associated to the state of carrier of at least one 460-Trp allele of 2.68. The finding of such low frequency of the 460-Trp allele in individuals of African ancestry points to the substantial ethnic variability of the genes that have been found to be associated with hypertension. On the other hand, it suggests an association of the 460-Trp allele with hypertension also in subjects of African origin.

Objective: To determine whether or not beta2 adrenoceptor polymorphism is a risk factor for the development of hypertension in a Black South African population., Background: Attenuated vasodilator responses to endogenous catecholamines may contribute to the aetiology of hypertension. Downregulation of beta2 adrenoreceptors (beta2AR) following stimulation with agonists is determined in part by variation at the beta2AR gene locus. The Glu27 beta2AR genotype results in attenuated downregulation compared with the wild-type Gln27 receptor, whereas Gly16 exhibits enhanced down-regulation compared to Arg16. Possible racial differences in the prevalence of the beta2AR polymorphisms may be an explanation for the blunted responses to isoprenaline and the increased prevalence of hypertension in Black African populations., Methods: One hundred and ninety-two unrelated hypertensives and 123 normotensives of Black South African origin were studied. Hypertensives were recruited from hospital hypertension clinics in the province of Gauteng and if on treatment, had a 2-4 week washout period before 24-h ambulatory blood pressure assessment Normotensive controls were recruited from the same community., Results: There was no significant association between either the Arg-Gly16 polymorphism or the Gln-Glu27 polymorphism and hypertension status. Furthermore, in the hypertensives, no significant association was seen between beta2AR genotype at either site and clinical blood pressure, 24-h blood pressure or left ventricular mass. A significant association was seen between Arg16 homozygotes and lower body mass index in hypertensives (P = 0.007) although this was not a primary end point. Interestingly, the Glu27 polymorphism was much rarer in this population (allelic frequency 17%) compared to a Caucasian population., Conclusion: These data suggest that beta2AR polymorphism is not a risk factor for hypertension per se in this defined population. The possibility that the decreased prevalence of Glu27 in black South African populations explains blunted vasodilator responses to isoprenaline requires further study.

A single-center, prospective double-blind randomized trial was conducted to compare the efficacy and safety of the calcium channel blocker nisoldipine in a sustained release coat-core formulation (CC), titrated from 10 mg to 40 mg daily, with the angiotensin converting enzyme inhibitor enalapril, titrated from 10 to 40 mg daily, in the treatment of black South African patients with severe hypertension (sitting diastolic blood pressure [DBP] between 115 and 140 mm Hg, confirmed by 24-h ambulatory blood pressure monitoring). Treatment target was a sitting DBP < 95 mm Hg by the 9th week of treatment. This was followed by a 4-month open phase using nisoldipine CC 10 to 60 mg daily. Ninety-six patients had complete data at baseline, and at the end of the double-blind and open phases, and were included in this analysis. In both groups, all patients required titration up to the maximal dose of double-blind medication. Monotherapy with nisoldipine CC, but not enalapril, significantly reduced both sitting and 24-h ambulatory blood pressure (BP). Twenty-four-hour BP in the nisoldipine CC group decreased from 179+/-14 / 118+/-7 to 144+/-16 / 94+/-10 mm Hg (P < .0001) versus 181+/-13 / 117+/-5 to 171+/-17 / 110+/-11 mm Hg in the enalapril group (P = ns). The profound decrease in blood pressure achieved with nisoldipine CC was accompanied by a significant reduction in left ventricular [LV] mass index, observed after only 2 months of treatment (from 146+/-40 to 129+/-35 g/m2, P = .05). In contrast, enalapril had no effect on LV mass (from 139+/-36 to 142+/-50 g/m2, P = NS). The antihypertensive effect of nisoldipine CC was further demonstrated in the open phase, during which 24-h BP decreased from 180+/-14 / 118+/-6 mm Hg (at baseline) to 142+/-16 / 92+/-10 mm Hg at the end of the 16-week open phase (P < .0001). This effect was sustained with trough-to-peak ratio of 74% for systolic and 67% for diastolic BP, with further regression in LV mass. Reduction in 24-h systolic BP to < 135 mm Hg was associated with a greater degree of regression of LV mass index in patients treated with nisoldipine CC. The incidence of adverse events in both groups was low and both nisoldipine CC and enalapril were well tolerated. The incidence of significant ventricular arrhythmia was also low and did not change with treatment. In conclusion, our findings suggest that nisoldipine CC administered once daily could be considered as a suitable first-line antihypertensive agent in black patients with severe hypertension, based on its profound and sustained blood-pressure-lowering effect, associated with significant regression of left ventricular mass and its low side effect profile.

OBJECTIVE: To examine the extent to which one session of repeated automated (30-45 min) blood pressure measurements in non-treated, hypertensive patients can be used to predict daytime ambulatory blood pressure (ABP). METHODS: Two hundred untreated black hypertensive patients (mean age 50.2+/-11.2) were retrospectively stratified on the basis of the daytime ambulatory diastolic blood pressure (DBP) into mild, moderate and severe hypertensives (90 mmHg

Using ambulatory blood pressure (BP) monitoring, a potent ACE-inhibitor/calcium channel blocker combination was tested in 21 Black patients (age 52 +/- 10 years; 10 males, 11 females) with mild to moderate hypertension (mean 12-hour daytime diastolic BP > or = 90 mmHg and < or = 114 mmHg). After a 14-day wash-out and a 14-day placebo run-in period, therapy was initiated with verapamil 180 mg plus trandolapril 2 mg. At monthly visits, if mean daytime diastolic BP remained > or = 90 mmHg, the dose combination was uptitrated stepwise to verapamil 240 mg plus trandolapril 4 mg, verapamil 360 mg plus trandolapril 4 mg, and finally hydrochlorothiazide 12.5 mg were added. Mean 24-hour BP dropped from 150 +/- 14/96 +/- 7 mmHg at baseline to 131 +/- 13/82 +/- 8 mmHg after 4 months treatment (p < 0.001). In 16 (76%) patients mean 24-hour diastolic BP was < 90 mmHg at the end of the trial and 15 (71%) patients achieved a reduction of > 10 mmHg. Five out of 5 patients finishing on dose I were controlled, 5/6 patients on dose II, 5/8 patients on dose III, and 1/2 patients who received additional hydrochlorothiazide. The 24-hour BP load fell from 72 +/- 8% at baseline to 35 +/- 25% in 4 months (p < 0.001). Mean diastolic BP drop for the 2 peak hours during daytime was 20 mmHg and for the last 2 hours of monitoring was 13 mmHg, resulting in a trough to peak ratio of 65%. There were no significant adverse events or biochemical abnormalities. It is concluded that the combination doses tested showed a sustained and marked antihypertensive effect throughout the 24-hour dosing interval, and the starting dose (verapamil 180 mg plus trandolapril 2 mg) seems appropriate in this group of patients.