Matches in SemOpenAlex for { <https://semopenalex.org/work/W2533088897> ?p ?o ?g. }
- W2533088897 endingPage "5581" @default.
- W2533088897 startingPage "5547" @default.
- W2533088897 abstract "Abstract. In this paper, we present a unique 9.5 m palaeo-lacustrine record of 771 palaeofloods which occurred over a period of 9.3 kyr in the Piànico–Sèllere Basin (southern Alps) during an interglacial period in the Pleistocene (sometime from 780 to 393 ka) and analyse its correlation, clustering, and cyclicity properties. We first examine correlations, by applying power-spectral analysis and detrended fluctuation analysis (DFA) to a time series of the number of floods per decade, and find weak long-range persistence: a power-spectral exponent βPS ≈ 0.39 and an equivalent power-spectral exponent from DFA, βDFA ≈ 0.25. We then examine clustering using the one-point probability distribution of the inter-flood intervals and find that the palaeofloods cluster in time as they are Weibull distributed with a shape parameter kW = 0.78. We then examine cyclicity in the time series of number of palaeofloods per year, and find a period of about 2030 years. Using these characterizations of the correlation, clustering, and cyclicity in the original palaeoflood time series, we create a model consisting of the superposition of a fractional Gaussian noise (FGN) with a 2030-year periodic component and then peaks over threshold (POT) applied. We use this POTFGN + Period model to create 2 600 000 synthetic realizations of the same length as our original palaeoflood time series, but with varying intensity of periodicity and persistence, and find optimized model parameters that are congruent with our original palaeoflood series. We create long realizations of our optimized palaeoflood model, and find a high temporal variability of the flood frequency, which can take values of between 0 and > 30 floods century−1. Finally, we show the practical utility of our optimized model realizations to calculate the uncertainty of the forecasted number of floods per century with the number of floods in the preceding century. A key finding of our paper is that neither fractional noise behaviour nor cyclicity is sufficient to model frequency fluctuations of our large and continuous palaeoflood record, but rather a model based on both fractional noise superimposed with a long-range periodicity is necessary." @default.
- W2533088897 created "2016-10-28" @default.
- W2533088897 creator A5002738445 @default.
- W2533088897 creator A5019365659 @default.
- W2533088897 creator A5050325759 @default.
- W2533088897 creator A5058798659 @default.
- W2533088897 date "2017-11-14" @default.
- W2533088897 modified "2023-09-30" @default.
- W2533088897 title "Analysis and modelling of a 9.3 kyr palaeoflood record: correlations, clustering, and cycles" @default.
- W2533088897 cites W139100814 @default.
- W2533088897 cites W1513643134 @default.
- W2533088897 cites W1520051030 @default.
- W2533088897 cites W1542776814 @default.
- W2533088897 cites W1564179327 @default.
- W2533088897 cites W1595138243 @default.
- W2533088897 cites W1596900083 @default.
- W2533088897 cites W1656129546 @default.
- W2533088897 cites W1660357404 @default.
- W2533088897 cites W1853205936 @default.
- W2533088897 cites W1878944287 @default.
- W2533088897 cites W1889294784 @default.
- W2533088897 cites W190565870 @default.
- W2533088897 cites W1941158494 @default.
- W2533088897 cites W1949645224 @default.
- W2533088897 cites W1964355054 @default.
- W2533088897 cites W1965865893 @default.
- W2533088897 cites W1967081204 @default.
- W2533088897 cites W1968721411 @default.
- W2533088897 cites W1973227610 @default.
- W2533088897 cites W1973429805 @default.
- W2533088897 cites W1974352335 @default.
- W2533088897 cites W1975902658 @default.
- W2533088897 cites W1976630949 @default.
- W2533088897 cites W1978986135 @default.
- W2533088897 cites W1982082363 @default.
- W2533088897 cites W1983599285 @default.
- W2533088897 cites W1984589466 @default.
- W2533088897 cites W1985013302 @default.
- W2533088897 cites W1985048042 @default.
- W2533088897 cites W1986271191 @default.
- W2533088897 cites W1991557232 @default.
- W2533088897 cites W1995778358 @default.
- W2533088897 cites W1998999027 @default.
- W2533088897 cites W1999921196 @default.
- W2533088897 cites W2001712064 @default.
- W2533088897 cites W2005148469 @default.
- W2533088897 cites W2006535771 @default.
- W2533088897 cites W2008875043 @default.
- W2533088897 cites W2008992984 @default.
- W2533088897 cites W2015459095 @default.
- W2533088897 cites W2017821362 @default.
- W2533088897 cites W2019368654 @default.
- W2533088897 cites W2021745986 @default.
- W2533088897 cites W2022599646 @default.
- W2533088897 cites W2024697317 @default.
- W2533088897 cites W2027339831 @default.
- W2533088897 cites W2031753087 @default.
- W2533088897 cites W2033050927 @default.
- W2533088897 cites W2036904089 @default.
- W2533088897 cites W2037511507 @default.
- W2533088897 cites W2037726243 @default.
- W2533088897 cites W2037948499 @default.
- W2533088897 cites W2038878767 @default.
- W2533088897 cites W2039842895 @default.
- W2533088897 cites W2047126007 @default.
- W2533088897 cites W2050489762 @default.
- W2533088897 cites W2054270169 @default.
- W2533088897 cites W2056843990 @default.
- W2533088897 cites W2057953526 @default.
- W2533088897 cites W2058024320 @default.
- W2533088897 cites W2061756144 @default.
- W2533088897 cites W2073332216 @default.
- W2533088897 cites W2073513240 @default.
- W2533088897 cites W2073676564 @default.
- W2533088897 cites W2074647934 @default.
- W2533088897 cites W2075514521 @default.
- W2533088897 cites W2078824647 @default.
- W2533088897 cites W2087148916 @default.
- W2533088897 cites W2091080894 @default.
- W2533088897 cites W2091494038 @default.
- W2533088897 cites W2094891710 @default.
- W2533088897 cites W2099529384 @default.
- W2533088897 cites W2100010101 @default.
- W2533088897 cites W2103300685 @default.
- W2533088897 cites W2103484453 @default.
- W2533088897 cites W2106814658 @default.
- W2533088897 cites W2109106775 @default.
- W2533088897 cites W2123598166 @default.
- W2533088897 cites W2128349082 @default.
- W2533088897 cites W2137047853 @default.
- W2533088897 cites W2138599756 @default.
- W2533088897 cites W2145996966 @default.
- W2533088897 cites W2156148063 @default.
- W2533088897 cites W2163464784 @default.
- W2533088897 cites W2314115852 @default.
- W2533088897 cites W2315293567 @default.
- W2533088897 cites W2338714606 @default.
- W2533088897 cites W2341760625 @default.