Pregled bibliografske jedinice broj: 937667
Generalised Pareto distribution : impact of rounding on parameter estimation
Generalised Pareto distribution : impact of rounding on parameter estimation // Theoretical and applied climatology, 136 (2018), 417-427 doi:10.1007/s00704-018-2494-5 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 937667 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Generalised Pareto distribution : impact of rounding on parameter estimation
Autori
Pasarić, Zoran ; Cindrić Kalin, Ksenija
Izvornik
Theoretical and applied climatology (0177-798X) 136
(2018);
417-427
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Generalized Pareto distribution ; dry spells ; L-moments ; Maximum likelihood
Sažetak
Problems that occur when common methods (e.g. maximum likelihood and L-moments) for fitting a generalised Pareto (GP) distribution are applied to discrete (rounded) data sets are revealed by analysing the real, dry spell duration series. The analysis is subsequently performed on generalised Pareto time series obtained by systematic Monte Carlo (MC) simulations. The solution depends on the following: (1) the actual amount of rounding, as determined by the actual data range (measured by the scale parameter, σ) vs. the rounding increment (Δx), combined with ; (2) applying a certain (sufficiently high) threshold and considering the series of excesses instead of the original series. For a moderate amount of rounding (e.g. σ/Δx ≥ 4), which is commonly met in practice (at least regarding the dry spell data), and where no threshold is applied, the classical methods work reasonably well. If cutting at the threshold is applied to rounded data—which is actually essential when dealing with a GP distribution—then classical methods applied in a standard way can lead to erroneous estimates, even if the rounding itself is moderate. In this case, it is necessary to adjust the theoretical location parameter for the series of excesses. The other solution is to add an appropriate uniform noise to the rounded data (“so-called” jittering). This, in a sense, reverses the process of rounding ; and thereafter, it is straightforward to apply the common methods. Finally, if the rounding is too coarse (e.g. σ/Δx~1), then none of the above recipes would work ; and thus, specific methods for rounded data should be applied.
Izvorni jezik
Engleski
Znanstvena područja
Geofizika
POVEZANOST RADA
Projekti:
HRZZ-IP-2013-11-2831 - Klima jadranske regije u njenom globalnom kontekstu (CARE) (Orlić, Mirko, HRZZ - 2013-11) ( CroRIS)
Ustanove:
Državni hidrometeorološki zavod,
Prirodoslovno-matematički fakultet, Zagreb
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus