Is daily precipitation Gamma-distributed? Adverse effects of an incorrect use of the Kolmogorov-Smirnov test
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F09%3A00328587" target="_blank" >RIV/68378289:_____/09:00328587 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Is daily precipitation Gamma-distributed? Adverse effects of an incorrect use of the Kolmogorov-Smirnov test
Popis výsledku v původním jazyce
The applicability of the Gamma distribution for the description of daily precipitation amounts within a single winter, spring, summer, and autumn season is tested on 90 European stations. The Lilliefors modi?cation of the Kolmogorov?Smirnov (KS) test isused to assess the goodness-of-?t of the Gamma distribution to daily precipitation in every year and season of the reference period. The possible rejection of the Gamma distribution for a particular station and season is based on the number of years in which the distribution is rejected. The results are compared with those obtained from the non-modi?ed KS test, whose application is incorrect when the ?t to the theoretical distribution is tested on the same data from which its parameters were estimated.We con?rm that the two tests yield considerably different results. The validity of the Gamma dist. is not as wide as it is commonly believed: in winter, precipitation at more than 40% of the examined stations is not Gamma-distributed.
Název v anglickém jazyce
Is daily precipitation Gamma-distributed? Adverse effects of an incorrect use of the Kolmogorov-Smirnov test
Popis výsledku anglicky
The applicability of the Gamma distribution for the description of daily precipitation amounts within a single winter, spring, summer, and autumn season is tested on 90 European stations. The Lilliefors modi?cation of the Kolmogorov?Smirnov (KS) test isused to assess the goodness-of-?t of the Gamma distribution to daily precipitation in every year and season of the reference period. The possible rejection of the Gamma distribution for a particular station and season is based on the number of years in which the distribution is rejected. The results are compared with those obtained from the non-modi?ed KS test, whose application is incorrect when the ?t to the theoretical distribution is tested on the same data from which its parameters were estimated.We con?rm that the two tests yield considerably different results. The validity of the Gamma dist. is not as wide as it is commonly believed: in winter, precipitation at more than 40% of the examined stations is not Gamma-distributed.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DG - Vědy o atmosféře, meteorologie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/IAA300420806" target="_blank" >IAA300420806: Pravděpodobnostní scénáře klimatu pro Českou republiku</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)
Ostatní
Rok uplatnění
2009
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Atmospheric Research
ISSN
0169-8095
e-ISSN
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Svazek periodika
93
Číslo periodika v rámci svazku
4
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
8
Strana od-do
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Kód UT WoS článku
000268352000009
EID výsledku v databázi Scopus
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