Model | Reservoir/ Component | Water Balance or State Equations | Constitutive Relations | State Variables | Model Fluxes | Model Parameters | |
HyMod | Soil Moisture (Sm) |
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| Sm is the soil moisture in the upper soil layer [mm]. Sq1 is the total water content in tank 1 [mm]. Sq2 is the total water content in tank 2 [mm]. Sq3 is the total water content in tank 3 [mm]. Ss is the total water content in the lower soil layer [mm]. Sm = 0; at t = 0 is the initial basin storage [mm]. Sq = 0; at t = 0 is the initial storage of quick-flow tanks [mm]. Ss = 0; at t = 0 is the initial storage of slow = flow tanks [mm]. | P is the Precipitation [mm∙d−1]. Pe is the effective Precipitation [mm∙d−1]. ET is the Evapo-transpiration from the soil [mm∙d−1]. PET is the Potential Evapotranspiration [mm∙d−1]. Qqi is the quick surface runoff in Sqi [mm∙d−1]. QS is the slow groundwater runoff in Ss [mm∙d−1]. | b is the shape parameter of the distribution of storage capacities within the basin [0.05 - 1.95]. α is the routing ratio quick to slow pathway [0.01 - 1]. Kq is the conductivity of the quick-flow routing tanks [0.001 - 0.1 day−1]. Ks is the conductivity of the slow-routing tanks [0.001-0.95 day−1] Nq is the number of quick flow linear tanks [1] - [5] . In this description Nq = 3. | |
Quick Routing Reservoir 1 (Sq1) |
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Quick Routing Reservoir 2 (Sq2) |
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Quick Routing Reservoir 3 (Sq3) |
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Slow Routing Reservoir (SS) |
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ARX | Autoregressive Component |
| | α is a parameter calculated from the autoregressive component applied to streamflow. β is a parameter calculated from the autoregressive component applied to rainfall. na is the lag number for streamflow. nb is the lag number for rainfall. | |||
DKF | Discrete Kalman Filter Component |
| | A and B are matrices containing α and β parameters from the series of streamflow and rainfall data in the ARX model. H is a transformed matrix that contains the states of the measurements. Q and R are matrices containing the covariance for the noise in the process and the measurements. | |||