Seasonal Hydrological and Meteorological Time Series

Time series models are often used in hydrology and meteorology studies to model streamflows series in order to make forecasting and generate synthetic series which are inputs for the analysis of complex water resources systems. In thispaper we introduce a new modeling approach for hydrologic and mete...

Full description

Autores:
Cepeda-Cuervo, Edilberto
Achcar, Jorge Alberto
Andrade, Marinho G.
Tipo de recurso:
Article of journal
Fecha de publicación:
2018
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/68578
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/68578
http://bdigital.unal.edu.co/69611/
Palabra clave:
55 Ciencias de la tierra / Earth sciences and geology
Hydrology time series data
Meteorological time series
Conditional regression models
Bayesian analysis
MCMC methods
Series de tiempo hidrológicas
Series de tiempo meteorológicas
Modelos de regresión condicional
Análisis Bayesiano
Métodos MCMC.
Rights
openAccess
License
Atribución-NoComercial 4.0 Internacional
Description
Summary:Time series models are often used in hydrology and meteorology studies to model streamflows series in order to make forecasting and generate synthetic series which are inputs for the analysis of complex water resources systems. In thispaper we introduce a new modeling approach for hydrologic and meteorological time series assuming a continuous distribution for the data, where both the conditional mean and conditional varianceparameters are modeled. Bayesian methods using standard MCMC (Markov Chain Monte Carlo Methods) are used to simulate samples for the joint posterior distribution of interest. Two applications to real data sets illustrate the proposedmethodology, assuming that the observations come from a normal, a gamma or a beta distribution. A first example is given by a time series of monthly averages of natural streamflows, measured in the year period ranging from1931 to 2010 in Furnas hydroelectric dam, Brazil. A second example is given with a time series of 313 air humidity data measured in a weather station of Rio Claro, a Brazilian city located in southeastern of Brazil. These applications motivate us to introduce new classes of models to analyze hydrological and meteorological time series