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dc.contributor.authorNadal-Sala, Daniel
dc.contributor.authorGracia, Carlos A.
dc.contributor.authorSabaté, Santiago
dc.date.accessioned2019-09-22T09:03:22Z
dc.date.available2019-09-22T09:03:22Z
dc.date.copyright11/27/2018 12:00:00 AM
dc.date.issued2018
dc.identifier.otherJAMC-D-18-0170.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4262573
dc.description.abstractThis paper describes the assumptions, equations, and procedures of the RheaG weather generator algorithm (WGA). RheaG was conceived for the generation of robust daily meteorological time series, whether in static or transient climate conditions. Here we analyze its performance in four Iberian locations?Bilbao, Barcelona, Madrid, and Sevilla?with differentiated climate characteristics. To validate the RheaG WGA, we compared observed and generated meteorological time series? statistical properties of precipitation, maximum temperature, and minimum temperature for all four locations. We also compared observed and simulated rain events spell length probabilities in all four locations. Finally, RheaG includes two weather generation procedures: one in which monthly mean values for meteorological variables are unconstrained and one in which they are constrained according to a predefined baseline climate variability. Here, we compare the two weather generation procedures included in RheaG using the observed data from Barcelona. Our results present a high agreement in the statistical properties and the rain spell length probabilities between observed and generated meteorological time series. Our results show that RheaG accurately reproduces seasonal patterns of the observed meteorological time series for all four locations, and it is even able to differentiate two climatic seasons in Bilbao that are also present in the observed data. We find a trade-off between generation procedures in which the unconstrained procedure better reproduces the variability of monthly and yearly precipitation than the constrained one, but the constrained procedure is able to keep the same climatic signal across meteorological time series. Thus, the first procedure is more accurate, but the latter is able to maintain spatial autocorrelation among generated meteorological time series.
dc.publisherAmerican Meteorological Society
dc.titleThe RheaG Weather Generator Algorithm: Evaluation in Four Contrasting Climates from the Iberian Peninsula
dc.typeJournal Paper
dc.journal.volume58
dc.journal.issue1
dc.journal.titleJournal of Applied Meteorology and Climatology
dc.identifier.doi10.1175/JAMC-D-18-0170.1
dc.journal.fristpage55
dc.journal.lastpage69
dc.treeJournal of Applied Meteorology and Climatology:;2018:;volume 058:;issue 001
dc.contenttypeFulltext


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