2008
DOI: 10.1016/j.advwatres.2007.10.001
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Robust data assimilation in hydrological modeling – A comparison of Kalman and H-infinity filters

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Cited by 27 publications
(19 citation statements)
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“…Increasingly, methods of data assimilation are being applied to both hydrological and hydrometeorological problems driven by prospects of better characterization of initial conditions and improved forecasting skill (Mecikalski et al 1999;Reichle et al 2001;Crosson et al 2002;Reichle et al 2002;Heathman et al 2003;Merlin et al 2006;Pan et al 2008;Wang and Cai 2008;Barrett et al 2008). The benefits afforded by the application of data assimilation approaches to hydrometeorological problems include better estimation of initial soil moisture and temperature in mesoscale climatological models (Jones et al 2004;Huang et al 2008), improved energy partitioning between latent and sensible heat fluxes (Pipunic et al 2008), and a concomitant higher skill in quantitative precipitation forecasts (Koster et al 2000).…”
Section: Introductionmentioning
confidence: 99%
“…Increasingly, methods of data assimilation are being applied to both hydrological and hydrometeorological problems driven by prospects of better characterization of initial conditions and improved forecasting skill (Mecikalski et al 1999;Reichle et al 2001;Crosson et al 2002;Reichle et al 2002;Heathman et al 2003;Merlin et al 2006;Pan et al 2008;Wang and Cai 2008;Barrett et al 2008). The benefits afforded by the application of data assimilation approaches to hydrometeorological problems include better estimation of initial soil moisture and temperature in mesoscale climatological models (Jones et al 2004;Huang et al 2008), improved energy partitioning between latent and sensible heat fluxes (Pipunic et al 2008), and a concomitant higher skill in quantitative precipitation forecasts (Koster et al 2000).…”
Section: Introductionmentioning
confidence: 99%
“…These include, for example, the one-, two-, three-and fourdimensional variational algorithms (1D-, 2D-, 3D-, and 4D-VAR, e.g., Seo et al, 2003Seo et al, , 2009Valstar et al, 2004), extended or ensemble Kalman filtering (EKF or EnKF, e.g., Moradkhani et al, 2005b;Slater and Clark, 2006;Weerts and El Serafy, 2006;Shamir et al, 2010), particle filtering (e.g., Moradkhani et al, 2005a;Weerts and El Serafy, 2006;Matgen et al, 2010;DeChant and Moradkhani, 2012), H-infinity filters (Wang and Cai, 2008), hybrid EnKF or 4D-VAR approaches (e.g., Zhang et al, 2009), and other Bayesian approaches (e.g., Reggiani and Weerts, 2008;Todini, 2008;Reggiani et al, 2009). While most DA applications have focused on updating hydrologic model states (e.g., soil moisture and snow water equivalent), recent research has also examined the benefits of estimating model states and model parameters simultaneously (e.g., Moradkhani et al, 2005a, b Vrugt et al, 2005;Lu et al, 2010;Leisenring and Moradkhani, 2011;Nie et al, 2011) as well as the possibility of model structure identification and uncertainty estimation (e.g., Neuman, 2003;Bulygina and Gupta, 2010;Hsu et al, 2009;Parrish et al, 2012).…”
Section: Introductionmentioning
confidence: 99%
“…Although contemporary robust control approaches such as  -controller have been used in many fields [11,12], environmental engineering applications have not seen exhaustive use of the robust system theory tools. However, there are some limited applications such as the comparison of Kalman and H ∞ filters in hydrologic system modeling in which uncertainty is difficult to model [13], the control systems approach to generalized water quality control problems [14], and various convex optimization schemes [15]. In addition, robust control was extended to non-linear systems [16] such as the management of nonlinear soil aquifer treatment systems whose administration appears to be challenging due to its dynamic nonlinearity.…”
Section: Introductionmentioning
confidence: 99%