There are three components to theas applied to the model, these are: diffuse recharge due to rainfall, flood recharge due to overbank flooding from the river, and irrigation recharge under areas that are irrigated. They were implemented in the model using the Recharge (RCH) package for MODFLOW-USG.
Rainfall recharge is spatially and temporally varying, reflecting spatial differences in near-surface geology and temporal variation in rainfall. The derivation of a mean annual recharge surface for the Namoi subregion using a chloride mass balance approach is described in Section 2.1.3 of companion product 2.1-2.2 for the Namoi subregion (). The temporal variation of rainfall recharge is provided by the Australian Water Resources Assessment (AWRA) landscape model (AWRA-L) (see companion product 2.6.1 for the Namoi subregion for details ( )). This is normalised so its average throughout the period 1983 to 2012 is 1, and the resultant time series is multiplied by the spatial variation from the chloride mass balance to yield the final spatial and temporally varying recharge as applied to the model (more details of this process are in ).
In addition to the rainfall recharge, groundwater Figure 12. Flood and irrigation recharge are applied to the groundwater model cells that are contained within the floodplain and irrigation areas.from flood and irrigation recharge were added to the recharge package. The depth of flood and irrigation recharge is calculated on a daily time step at the reach scale in the AWRA river model (AWRA-R) (for details see companion product 2.6.1 for the Namoi subregion ( )). The reaches that contain floodplain and irrigation areas are shown in
Recharge is applied as a source of water of prescribed rate to the land surface of the model. To account forin both the temporal and spatial variation of recharge, its magnitude is varied in the analysis for each of the three components (see companion submethodology M07 (as listed in Table 1) for groundwater modelling ( )).
AWRA-R = Australian Water Resources Assessment river model
Data: Bioregional Assessment Programme ()
Evapotranspiration is represented by a sink of Figure 13) plus 1, this means that with 40 m vegetation height there is an extinction depth of 11 m and for vegetation that has zero height (i.e. bare ground) there is an extinction depth of 1 m.applied across the entire land surface of the model using the EVT package in MODFLOW-USG. Generally in groundwater models, evapotranspiration from groundwater is assumed to be a maximum when the is at ground surface, or above it (e.g. in the case of ponding). Conversely, evapotranspiration from groundwater is generally assumed to be zero when the watertable is deep below the ground surface where plant roots cannot draw water from the deep groundwater reserves. There is an analysis of the depth to watertable for the in companion product 2.1-2.2 ( ) which is indicative of where an evapotranspiration flux from groundwater may be significant. The maximum evapotranspiration rate was set as a constant across the model domain and the extinction depth was related to the vegetation height using the assumption that taller vegetation have deeper roots. The extinction depth was calculated as a quarter of the vegetation height (
Data: Caltech/JPL ()
Product Finalisation date
- 126.96.36.199 Methods
- 188.8.131.52 Review of existing models
- 184.108.40.206 Model development
- 220.127.116.11 Boundary and initial conditions
- 18.104.22.168 Implementation of the coal resource development pathway
- 22.214.171.124 Parameterisation
- 126.96.36.199 Observations and predictions
- 188.8.131.52 Uncertainty analysis
- 184.108.40.206 Limitations
- Currency of scientific results
- Contributors to the Technical Programme
- About this technical product