Saturated Zone storage
The Saturated Zone storage includes all water below the water table. All groundwater pumping is from the saturated zone, including irrigation extraction from groundwater.
The items listed in Table 6.5 are those found in the “Saturated Zone - detailed” water balance output in the water balance configuration file:
[WblTypeDefinition]
Name = 'SZ_DETAIL'
DisplayName = 'Saturated Zone - detailed'
Description = 'Detailed Saturated ... balance (depth-integrated)'
NoGroups = 28
Group = 'qszprecip(sz.qszprecip)'
Group = 'qrech(uz.qrech)'
Group = 'qrechmp(uz.qrechmp)'
Group = 'qolszpos(sz.qolszpos)'
Group = 'qolszneg(sz.qolszneg)'
Group = 'qetsz(sz.qetsz)'
Group = 'qszin(sz.qszin)'
Group = 'qszout(sz.qszout)'
Group = 'dszsto(sz.dszsto)'
Group = 'qszabsex(sz.qszabsex)'
Group = 'qszdrin(sz.qszdrin)'
Group = 'qszdrout(sz.qszdrout)'
Group = 'qszdrtorivin(sz.qszdrtorivin)'
Group = 'qszdrtorivex(sz.qszdrtorivex)'
Group = 'qszdrtoM11HPoint(sz.qszdrtoM11HPoint)'
Group = 'qszrivneg(sz.qszrivneg)'
Group = 'qszrivpos(sz.qszrivpos)'
Group = 'qszfloodneg(ol.qsztofloodneg)'
Group = 'qszfloodpos(ol.qsztofloodpos)'
Group = 'qgihbpos(sz.qgihbpos)'
Group = 'qgihbneg(sz.qgihbneg)'
Group = 'qirrwell(sz.qirrwell)'
Group = 'qszdrtoMouse(sz.qszdrtoMouse)'
Group = 'qszMousepos(sz.qszMousepos)'
Group = 'qszMouseneg(sz.qszMouseneg)'
Group = 'qSzExtSink(sz.qSzExtSink)'
Group = 'qSzExtSource(sz.qSzExtSource)'
Group = 'Error(sz.szwblerrtot)'
EndSect // WblTypeDefinition
The sign convention in the SZ water balance is such that infiltration from the unsaturated zone is negative (inflow) and discharge to overland flow is positive (outflow). All of the items together should add to zero.
The use of negative signs in the SZ water balance is avoided by explicitly including both inflow (negative) and outflow (positive) terms. For example, sz.qOlSzPos is the flow from the saturated zone directly to ponded water when the groundwater table is at or above the ground surface. In the MIKE SHE results, this is a positive upwards flow, and in the water balance it is a positive outflow. Similarly, sz.qOlSzNeg is the downward flow from ponded water directly to the saturated zone, which is a negative downward flow and a negative water balance inflow to SZ.
Item |
Description |
Sign Convention in the Water balance |
Included in Wbl Error |
---|---|---|---|
sz.qSzPrecip |
Precipitation added directly to the SZ layer. This can only be non-zero when the simulation does not include UZ. If UZ is included, but the groundwater table is at the ground surface (no UZ cells), the precipitation to SZ is included in the term sz.qOlSzNeg. Can be an outflow if the negative precipitation option specified in the Extra Parameters (Negative Precipitation (V1 p. 737)). In this case, negative precipitation can be removed from multiple SZ layers. |
Inflow - negative Can be positive (outflow) if negative precipitation option specified. |
yes |
sz.qszin (per layer) |
SZ flow into the subcatchment |
Positive out of SZ (always negative, but printed as a positive value in the WB table) |
|
uz.rech |
Recharge out of the bottom of the UZ soil column to SZ via the UZ soil matrix. In the MIKE SHE results, recharge is a vertical downward flow, thus in the negative direction. This is the same sign as the water balance convention of negative inflow. |
Inflow - negative |
yes |
uz.rechmp |
Recharge out of the bottom of the UZ soil column to SZ via the UZ macropores or by-pass flow. In the MIKE SHE results, recharge is a vertical downward flow, thus in the negative direction. This is the same sign as the water balance convention of negative inflow. |
Inflow - negative |
yes |
sz.qOlSzPos |
Upward flow directly from SZ to ponded water. This is non-zero only when the groundwater table is at or above the ground surface. The sign is positive upwards which is the same as the positive outflow water balance sign convention. |
Outflow - positive |
yes |
sz.qOlSzNeg |
Downward flow directly from ponded water to SZ. This is non-zero only when the groundwater table is at or above the ground surface. The sign is positive upwards which is the same as the negative inflow water balance sign convention. |
Inflow - negative |
yes |
sz.EtSz |
Evapotranspiration directly from SZ. |
Positive - outflow |
yes |
sz.qSzIn |
Inflow to SZ storage across the boundary of the model, or inflow across the boundary of the water balance sub-area. Inflow from internal fixed head cells is also included in this term. |
Inflow - negative |
yes |
sz.qSzOut |
Outflow from SZ storage across the boundary of the model, or outflow across the boundary of the water balance sub-area. Outflow to internal fixed head cells is also included in this term, as well as drainage to local depressions that contain a fixed head boundary condition. |
Outflow - positive |
yes |
sz.dSzSto |
Change in SZ storage |
Positive when storage increases |
yes |
sz.dszsto_dead (per layer) |
how can this be by layer????? |
|
|
sz.szsto |
|
|
|
sz.qSzAbsEx |
Groundwater pumping from SZ. This does not include irrigation wells and shallow irrigation wells, but includes outflow to fixed head drain internal boundary conditions. |
Outflow - positive Can be negative (Inflow) if injection specified for wells. |
yes |
sz.qUZfeedback |
how can this be by layer????? |
|
|
sz.qSzDrIn |
SZ drainage to local depressions in the current water balance area from areas outside of the current water balance sub-area. This term also includes inflow to the SZ drainage system added via OpenMI. |
Inflow - negative |
yes |
sz.qSzDrOut |
SZ drainage to the model boundary, SZ drainage removed directly from the model. This term also includes SZ drainage to local depressions located outside of the current water balance sub-area. |
Outflow - positive |
yes |
sz.qSzDrToRivIn |
SZ drainage to MIKE SHE River Links inside of the water balance sub-area. |
Outflow - positive |
yes |
sz.qSzDrToRivEx |
SZ drainage to MIKE SHE River Links outside of the water balance sub-area. This can only be non-zero if the water balance is calculated for a sub-area. |
Outflow - positive |
yes |
sz.qszdrtoM11HPoint |
SZ drainage to specified MIKE 11 H-points |
|
|
sz.qSzDrToM11HPoint |
SZ drainage to specified MIKE Hydro River h-points. These are specified in the Extra Parameter option in SZ Drainage to Specified MIKE Hydro River H-points (V1 p. 758) |
Outflow - positive |
yes |
sz.qSzRivPos |
Baseflow from SZ to MIKE SHE River Links |
Outflow - positive |
yes |
sz.qSzRivNeg |
Infiltration from MIKE SHE River Links to SZ |
Inflow - negative |
yes |
ol.qSZToFloodPos |
Direct flow upwards from SZ to an active flood code cell (active means that it is actually flooded and the water level is controlled by the water level in MIKE Hydro River). This is a positive upwards flow in the MIKE SHE results files. Only non-zero when the groundwater table is at or above the ground surface. |
Outflow - positive (Note sign change compared to detailed Ponded Storage water balance) |
yes |
ol.qSZToFloodNeg |
Direct flow downwards from an an active flood code cell to SZ. (active means that it is actually flooded and the water level is controlled by the water level in MIKE Hydro River). This is a negative downwards flow in the MIKE SHE results files. Only non-zero when the groundwater table is at or above the ground surface. |
Inflow - negative (Note sign change compared to detailed Ponded Storage water balance)
|
yes |
sz.qGihbPos |
Outflow from SZ storage to internal general head boundaries (GHB cells) |
Outflow - positive |
yes |
sz.qGihbNeg |
Inflow from internal general head boundaries (GHB cells) to SZ storage |
Inflow - negative |
yes |
sz.qIrrWell |
Groundwater pumping from irrigation wells. This includes both specified irrigation wells and shallow wells. |
Outflow - positive |
yes |
sz.qSzDrToMouse |
SZ drainage to specified MOUSE/MIKE Urban manholes. These are specified in the Extra Parameter option in Time varying SZ drainage parameters (V1 p. 761) |
Outflow - positive |
yes |
sz.qSzMousePos |
Outflow from SZ storage to Mouse/MIKE Urban pipes |
Outflow - positive |
yes |
sz.qSzMouseNeg |
Inflow from Mouse/MIKE Urban pipes to SZ storage |
Inflow - negative |
yes |
sz.qSzExtSink |
Outflow to external sinks specified via OpenMI |
Outflow - positive |
yes |
sz.qSzExtSource |
Inflow from external sources specified via OpenMI |
Inflow - negative |
yes |
sz.qSzExtSink (per layer) |
|
|
|
sz.qSzExtSource (per layer) |
|
|
|
sz.szWblErrTot |
Aggregated SZ water balance error for all layers |
Positive if water generated (Dstorage + Outflow > Inflow) |
|
sz.qsztofloodpos |
Upward flow from SZ to flooded areas (not in list) |
Positive up (always positive) |
|
sz.qsztofloodneg |
Downward flow from flooded areas to SZ (not in list) |
Positive up (always negative)
|
|
Saturated Zone layers
The Saturated Zone water balance can also be calculated by numerical layer. This means that all of the items in Table 6.5 are repeated for each numerical layer. However, in this case the water balance error term, sz.szWblErrTot is replace by a water balance error for each layer.
The layer water balance is slightly more complicated. It includes terms for the exchange between layers, and the upper layer includes the terms for the exchange with UZ and ponded water.
In particular, the output for each SZ layer water balance only includes the exchange with the layer above. This is found in the two additional layer water balance terms qSzZpos and qSzZneg.
The first term, qSzZpos, is the flow from the current layer upwards to the layer above. In the results files, this term is in the positive (upwards) direction. In the water balance, the term is also a positive outflow.
The second term, qSzZneg, is the flow from the layer above downwards into the current layer. In the results files, this term is in the negative (downwards) direction. In the water balance, the term is also a negative inflow to the current layer.
Note: The layer water balance error includes the flows to and from the layers above and below. However, when summing up the flows, the sign must be changed for the qSzZpos and qSzZneg terms that originate from the layer below.
Saturated Zone Linear Reservoir water balance
If the linear reservoir method is used for the saturated zone, the water balance terms are basically the same but are slightly less transparent.
The layer output for the linear reservoir method divides the SZ into two layers - the interflow reservoirs and the baseflow reservoirs. For the linear reservoir layers, there is no distinction between the two parallel baseflow reservoirs, or the cascading interflow reservoirs.
The items listed in Table 6.7 are those found in the “Saturated Zone - layers(Linear Reservoir)” water balance output in the water balance configuration file:
[WblTypeDefinition]
Name = 'SZ_LAYER_LR'
DisplayName = 'Saturated Zone - layers(Linear Reservoir)'
Description = 'Saturated zone water balance for linear reservoir'
NoGroups = 13
Group = 'recharge(uz.qrech+uz.qrechmp)'
Group = 'evapotranspirationSZ(sz.qetsz)'
Group = 'lateral IN(sz.qszin)'
Group = 'lateral OUT(sz.qszout)'
Group = 'percolation(sz.qszzneg)'
Group = 'To river(sz.qszrivpos)'
Group = 'From river(sz.qszrivneg)'
Group = 'storagechange(sz.dszsto)'
Group = 'deadzonestoragechange(sz.dszsto_dead)'
Group = 'pumping(sz.qszabsex)'
Group = 'Irr.pumping(sz.qirrwell)'
Group = 'feedbackUZ(sz.qUZfeedback)'
Group = 'Error(sz.szwblerr)'
EndSect // WblTypeDefinition