none2This study considers the use of the maximum likelihood estimator proposed by Whittle for calibrating the parameters of hydrological models. Whittle’s likelihood provides asymptotically consistent estimates for Gaussian and non Gaussian data, even in the presence of long range dependence. This method may represent a valuable opportunity in the context of ungauged or scarcely gauged catchments. In fact, the only information required for model parameterization is the spectral density function of the actual process simulated by the model. When long series of calibration data are not available, the spectral density can be inferred by using old and sparse records, regionalization methods or information on the correlation properties of the ...
Estimation of parameter and predictive uncertainty of hydrologic models has traditionally relied on ...
Estimation of parameter and predictive uncertainty of hydrologic models has traditionally relied on ...
Traditional procedures for rainfall\u2013runoff model calibration are generally based on the fit of ...
This study considers the use of the maximum likelihood estimator proposed by Whittle for calibrating...
When extended hydrological information is lacking, it becomes extremely important to be able to cali...
For a stationary time series, Whittle constructed a likelihood for the spectral density based on th...
Parameter estimation for rainfall-runoff models in ungauged basins is a challenging task that is re...
Parameter estimation for rainfall-runoff models in ungauged basins is a challenging task that is rec...
This paper proposes a spectral domain likelihood function for the Bayesian estimation of hydrologica...
Abstract: Estimating the uncertainty of hydrological models remains a relevant challenge in applied ...
Hydrologic models use relatively simple mathematical equations to conceptualize and aggregate the co...
This paper presents a calibration framework based on the generalized likelihood uncertainty estimati...
Estimating the uncertainty of hydrological models remains a relevant challenge in applied hydrology,...
Abstract Hydrological models contain parameters, values of which cannot be directly measured in the...
Hydrologic Research Laboratory of the National Weather Service, U.S. Dept. of Commerce NA 80AA-H-000...
Estimation of parameter and predictive uncertainty of hydrologic models has traditionally relied on ...
Estimation of parameter and predictive uncertainty of hydrologic models has traditionally relied on ...
Traditional procedures for rainfall\u2013runoff model calibration are generally based on the fit of ...
This study considers the use of the maximum likelihood estimator proposed by Whittle for calibrating...
When extended hydrological information is lacking, it becomes extremely important to be able to cali...
For a stationary time series, Whittle constructed a likelihood for the spectral density based on th...
Parameter estimation for rainfall-runoff models in ungauged basins is a challenging task that is re...
Parameter estimation for rainfall-runoff models in ungauged basins is a challenging task that is rec...
This paper proposes a spectral domain likelihood function for the Bayesian estimation of hydrologica...
Abstract: Estimating the uncertainty of hydrological models remains a relevant challenge in applied ...
Hydrologic models use relatively simple mathematical equations to conceptualize and aggregate the co...
This paper presents a calibration framework based on the generalized likelihood uncertainty estimati...
Estimating the uncertainty of hydrological models remains a relevant challenge in applied hydrology,...
Abstract Hydrological models contain parameters, values of which cannot be directly measured in the...
Hydrologic Research Laboratory of the National Weather Service, U.S. Dept. of Commerce NA 80AA-H-000...
Estimation of parameter and predictive uncertainty of hydrologic models has traditionally relied on ...
Estimation of parameter and predictive uncertainty of hydrologic models has traditionally relied on ...
Traditional procedures for rainfall\u2013runoff model calibration are generally based on the fit of ...