Multiscaling pulse representation of temporal rainfall
By Daniele Veneziano, Vito Iacobellis. 2002
64 citations recorded by the source corpus.
Subfields: Economics and Econometrics, Environmental Engineering, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/0ef7714413970a12e09832b5e96f39eb7c8b8b84
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Economics and Econometrics
- F. Serinaldi
- Andreas Langousis
- Marco Marani
- Daniele Veneziano
- P. Furcolo
- Vito Iacobellis
- L. Alfieri
- Francesco Laio
In Environmental Engineering
- L. Alfieri
- Francesco Laio
- P. Claps
- Marco Marani
- F. Serinaldi
- P. Furcolo
- Daniele Veneziano
- Andreas Langousis
In Global and Planetary Change
Citations in the corpus
- Multifractality, imperfect scaling and hydrological properties of rainfall time series simulated by continuous universal multifractal and discrete random cascade models (2010, background): “intervals at the beginning, middle, or end of a rainfall event (Olsson, 1998; Olsson and Berndtsson, 1998; Güntner et al., 2001; Veneziano and Iacobellis, 2002).”
- Time scale and intensity dependency in multiplicative cascades for temporal rainfall disaggregation (2009, background): “[37] A conspicuous feature of the cascade weights (W) is that they are asymmetric for the starting and ending interval classes [Olsson, 1998; Güntner et al., 2001; Veneziano and Iacobellis, 2002].”
- Imperfect scaling of time and space–time rainfall (2006, background): “The rain gauge record from the Osservatorio Ximeniano in Florence, Italy (Becchi and Castelli, 1989), which has a temporal resolution of 5 min and covers the 24-year period from 1962 to 1985; see Veneziano and Iacobellis (2002) for an analysis of this data set.”
- A simulation experiment for optimal design hyetograph selection (2008, methodology): “The IRP model (Veneziano and Iacobellis, 2002) is adopted to generate rainfall time-series.”
- Marginal methods of intensity‐duration‐frequency estimation in scaling and nonscaling rainfall (2007, background): “A notable exception is when the rainfall model has multifractal scale invariance [Schertzer and Lovejoy, 1987, Lovejoy and Schertzer, 1995; Olsson, 1995; Veneziano and Iacobellis, 2002].”
- Non‐power‐law‐scale properties of rainfall in space and time (2005, background): “Correspondingly, an entire family of rainfall models exhibiting fractal and multifractal properties has been developed [e.g., Lovejoy and Mandelbrot, 1985; Gupta and Waymire, 1993; Over and Gupta, 1996; Schertzer and Lovejoy, 1987; Schmitt et al., 1998; Veneziano and Iacobellis, 2002], complementing”
- Multifractality and rainfall extremes: A review (2006, background): “This is for example clear from the spectral analysis of rainfall records [Fraedrich and Larnder, 1993; Olsson et al., 1993; Olsson, 1995] and from the distribution of dry periods [Schmitt et al., 1998; Veneziano and Iacobellis, 2002 ].”