2020
DOI: 10.1016/j.advwatres.2019.103483
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Extreme value metastatistical analysis of remotely sensed rainfall in ungauged areas: Spatial downscaling and error modelling

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Cited by 35 publications
(23 citation statements)
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“…The MEVD, on the contrary, uses all the daily rainfall values in the analysis window and is thus not very sensitive to a few large or low values, thereby leading to more stable estimates of the 100‐year event. This time coherence of extremes is characteristic of the MEVD and is entirely analogous to the spatial coherence noted when estimating maps of extreme events from rainfall remote sensing estimates (Zorzetto & Marani, 2020). Fluctuations in h100GEV are more contained for the 30‐year window (Figure 6b), due to the longer sample used for parameter estimation and because short fluctuation frequencies are filtered out by the use of longer analysis windows (which is also visible in the case of MEVD estimates).…”
Section: Resultssupporting
confidence: 54%
“…The MEVD, on the contrary, uses all the daily rainfall values in the analysis window and is thus not very sensitive to a few large or low values, thereby leading to more stable estimates of the 100‐year event. This time coherence of extremes is characteristic of the MEVD and is entirely analogous to the spatial coherence noted when estimating maps of extreme events from rainfall remote sensing estimates (Zorzetto & Marani, 2020). Fluctuations in h100GEV are more contained for the 30‐year window (Figure 6b), due to the longer sample used for parameter estimation and because short fluctuation frequencies are filtered out by the use of longer analysis windows (which is also visible in the case of MEVD estimates).…”
Section: Resultssupporting
confidence: 54%
“…So far, MEV methods have been mostly used for the analysis of extreme daily precipitation relying on Weibull distributions to describe the ordinary events (e.g., Marani & Ignaccolo, 2015; Miniussi & Marani, 2020; Zorzetto et al, 2016). Results showed a number of advantages over traditional methods based on the sampled extremes: (i) rare quantiles, corresponding to return periods longer than the available data record, are estimated with significantly reduced errors; (ii) short records are sufficient to obtain robust estimates; (iii) the method is less sensitive to measurement errors typically affecting extremes (Marra et al, 2018; Miniussi & Marani, 2020; Schellander et al, 2019; Zorzetto et al, 2016; Zorzetto & Marani, 2020). However, two knowledge gaps currently restrain the application of MEV to subdaily durations.…”
Section: Introductionmentioning
confidence: 99%
“…The distribution of extremes arising from mixing different populations of ordinary events is described here using a modified Metastatistical Extreme Value Distribution (MEVD) (Marani & Ignaccolo, 2015), which provides flexibility in incorporating the joint effect of different statistical populations and leverages the added value of incorporating physical mechanisms into statistical analysis (Klemeš, 1974). The MEVD relaxes some of the restrictive assumptions of the traditional Extreme Value Theory (EVT) and has been shown to outperform it in a wide range of applications, from daily and hourly rainfall, to remotely sensed precipitation, to hurricane intensities in the Atlantic Ocean, to peak flood flows (Zorzetto et al, 2016; Marra et al, 2018; Zorzetto & Marani, 2019; Zorzetto & Marani, 2020; Schellander et al, 2019; Hosseini, Scaioni, & Marani, 2020; Miniussi et al, 2020). Here we apply the mixed and original formulations of the MEVD to long series of daily rainfall in several American metropolitan areas, which have a high likelihood of being struck by a TC.…”
Section: Introductionmentioning
confidence: 99%