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• W4309639308 abstract "Abstract. Extreme precipitation is a weather phenomenon with tremendous damaging potential for property and human life. As the intensity and frequency of such events is projected to increase in a warming climate, there is an urgent need to advance the existing knowledge on extreme precipitation processes, statistics and impacts across scales. To this end, a working group within the Germany-based project, ClimXtreme, has been established to carry out multidisciplinary analyses of high-impact events. In this work, we provide a comprehensive assessment of the 29 June 2017 heavy precipitation event (HPE) affecting the Berlin metropolitan region (Germany), from the meteorological, impacts and climate perspectives, including climate change attribution. Our analysis showed that this event occurred under the influence of a mid-tropospheric trough over western Europe and two shortwave surface lows over Britain and Poland (Rasmund and Rasmund II), inducing relevant low-level wind convergence along the German–Polish border. Over 11 000 convective cells were triggered, starting early morning 29 June, displacing northwards slowly under the influence of a weak tropospheric flow (10 m s−1 at 500 hPa). The quasi-stationary situation led to totals up to 196 mm d−1, making this event the 29 June most severe in the 1951–2021 climatology, ranked by means of a precipitation-based index. Regarding impacts, it incurred the largest insured losses in the period 2002 to 2017 (EUR 60 million) in the greater Berlin area. We provide further insights on flood attributes (inundation, depth, duration) based on a unique household-level survey data set. The major moisture source for this event was the Alpine–Slovenian region (63 % of identified sources) due to recycling of precipitation falling over that region 1 d earlier. Implementing three different generalised extreme value (GEV) models, we quantified the return periods for this case to be above 100 years for daily aggregated precipitation, and up to 100 and 10 years for 8 and 1 h aggregations, respectively. The conditional attribution demonstrated that warming since the pre-industrial era caused a small but significant increase of 4 % in total precipitation and 10 % for extreme intensities. The possibility that not just greenhouse-gas-induced warming, but also anthropogenic aerosols affected the intensity of precipitation is investigated through aerosol sensitivity experiments. Our multi-disciplinary approach allowed us to relate interconnected aspects of extreme precipitation. For instance, the link between the unique meteorological conditions of this case and its very large return periods, or the extent to which it is attributable to already-observed anthropogenic climate change." @default.
• W4309639308 created "2022-11-28" @default.
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• W4309639308 date "2022-11-17" @default.
• W4309639308 modified "2023-10-17" @default.
• W4309639308 title "Meteorological, impact and climate perspectives of the 29 June 2017 heavy precipitation event in the Berlin metropolitan area" @default.
• W4309639308 cites W1497810761 @default.
• W4309639308 cites W1513919779 @default.
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• W4309639308 cites W1689307259 @default.
• W4309639308 cites W1746274139 @default.
• W4309639308 cites W1831098712 @default.
• W4309639308 cites W1862346859 @default.
• W4309639308 cites W1977889939 @default.
• W4309639308 cites W1981501315 @default.
• W4309639308 cites W1983349412 @default.
• W4309639308 cites W1985623131 @default.
• W4309639308 cites W1986722213 @default.
• W4309639308 cites W1991179779 @default.
• W4309639308 cites W1993953606 @default.
• W4309639308 cites W1996509234 @default.
• W4309639308 cites W1998525562 @default.
• W4309639308 cites W2007431139 @default.
• W4309639308 cites W2015241713 @default.
• W4309639308 cites W2018997274 @default.
• W4309639308 cites W2020085556 @default.
• W4309639308 cites W2026342944 @default.
• W4309639308 cites W2039785873 @default.
• W4309639308 cites W2044387082 @default.
• W4309639308 cites W2050962456 @default.
• W4309639308 cites W2053531474 @default.
• W4309639308 cites W2064061204 @default.
• W4309639308 cites W2066078666 @default.
• W4309639308 cites W2069225437 @default.
• W4309639308 cites W2072836388 @default.
• W4309639308 cites W2080398386 @default.
• W4309639308 cites W2081334319 @default.
• W4309639308 cites W2091762623 @default.
• W4309639308 cites W2103261689 @default.
• W4309639308 cites W2109294560 @default.
• W4309639308 cites W2112005460 @default.
• W4309639308 cites W2113633153 @default.
• W4309639308 cites W2119031233 @default.
• W4309639308 cites W2120373626 @default.
• W4309639308 cites W2123834969 @default.
• W4309639308 cites W2127488336 @default.
• W4309639308 cites W2131792133 @default.
• W4309639308 cites W2136923819 @default.
• W4309639308 cites W2137354438 @default.
• W4309639308 cites W2142416981 @default.
• W4309639308 cites W2143837721 @default.
• W4309639308 cites W2145808843 @default.
• W4309639308 cites W2149197032 @default.
• W4309639308 cites W2151514073 @default.
• W4309639308 cites W2162760508 @default.
• W4309639308 cites W2174435849 @default.
• W4309639308 cites W2175098853 @default.
• W4309639308 cites W2178352276 @default.
• W4309639308 cites W2178959498 @default.
• W4309639308 cites W2282552493 @default.
• W4309639308 cites W2291268986 @default.
• W4309639308 cites W2292668626 @default.
• W4309639308 cites W2301135663 @default.
• W4309639308 cites W2337225114 @default.
• W4309639308 cites W2338040649 @default.
• W4309639308 cites W2479478582 @default.
• W4309639308 cites W2485106301 @default.
• W4309639308 cites W2512462031 @default.
• W4309639308 cites W2552494199 @default.
• W4309639308 cites W2556607975 @default.
• W4309639308 cites W2557008146 @default.
• W4309639308 cites W2559367804 @default.
• W4309639308 cites W2581791961 @default.

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