Waitaki Water Quality Catchment Modelling
Prepared for Environment Canterbury
May 2015
Prepared by : Christopher Palliser Sandy Elliott Sharleen Yalden Ude Shankar
For any information regarding this report please contact: Christopher Palliser Scientist Catchment Processes +64-7-856 1748 [email protected]
National Institute of Water & Atmospheric Research Ltd PO Box 11115 Hamilton 3251
Phone +64 7 856 7026
NIWA CLIENT REPORT No: HAM2015-002 Report date: May 2015 NIWA Project: ENC14202
Quality Assurance Statement Dr Annette Semadeni-Davies Reviewed by: Urban aquatic scientist NIWA Auckland
Formatting checked by: A. Bartley
Approved for release by: D. Roper
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Whilst NIWA has used all reasonable endeavours to ensure that the information contained in this document is accurate, NIWA does not give any express or implied warranty as to the completeness of the information contained herein, or that it will be suitable for any purpose(s) other than those specifically contemplated during the Project or agreed by NIWA and the Client.
Contents
Executive summary ...... 5
1 Introduction ...... 6
2 Method ...... 9 2.1 The CLUES model ...... 9 2.2 Measured water quality and flow data ...... 25 2.3 Determination of suitable calibration sites ...... 36 2.4 Calibration ...... 39
3 Results ...... 43 3.1 Model fit and uncertainty ...... 43
4 Summary and conclusions ...... 52
5 References ...... 53
Appendix A Waitaki sub-catchments ...... 55
Appendix B Percentage of land use by area for each of the watersheds of the calibrated sites ...... 58
Appendix C TN and TP leaching rates ...... 64
Appendix D Flow diversions ...... 87
Appendix E Detrended concentrations ...... 91
Tables Table 2-1: Map key and annual nutrient loads for point sources. 12 Table 2-2: Combinations of land use, rainfall and soil types in the Upper and Lower Waitaki River catchments used in the customised version of CLUES (ECan, pers. comm .). 15 Table 2-3: Soils in the Upper Waitaki (ECan, pers. comm.). 17 Table 2-4: Soils in the Lower Waitaki (ECan, pers. comm .). 18 Table 2-5: Measured, default CLUES and customised CLUES flows for the water quality calibration sites in the Upper Waitaki. 20 Table 2-6: Measured, default CLUES and customised CLUES flows for the water quality calibration sites in the Lower Waitaki. 23 Table 2-7: Estimated flow diversions in the Waitaki River catchment. 25 Table 2-8: Measured median concentrations for TN and TP in the Upper Waitaki catchment. 28
Waitaki Water Quality Catchment Modelling
Table 2-9: Measured median concentrations for TN and TP in the Lower Waitaki catchment. 32 Table 2-10: Map key for calibration sites. 37 Table 2-11: Adjusted TN and TP leaching rates for the Upper Waitaki. 40 Table 2-12: Adjusted TN and TP leaching rates for the Lower Waitaki. 42 Table 3-1: TN measured and modelled loads and yields at the calibration sites in the Upper Waitaki catchment. 44 Table 3-2: TP measured and modelled loads and yields at the calibration sites in the Upper Waitaki catchment. 45 Table 3-3: TN measured and modelled loads and yields at the calibration sites in the Lower Waitaki catchment. 47 Table 3-4: TP measured loads and yields at the calibration sites in the Lower Waitaki catchment (see Figure 2-4). 49
Table A-1: Figure 1-1 key for sub-catchments. 55 Table B-1: Percentage of land use by area for each of the watersheds of the calibrated water quality monitoring sites. 58 Table C-1: TN and TP leaching rates for the Upper Waitaki (ECan, pers. comm.). 64 Table C-2: TN leaching rates for the Lower Waitaki ( ECan, pers. comm .). 71
Figures Figure 1-1: Waitaki River sub-catchments showing streams of order ≥ 3 and lakes. 8 Figure 2-1: Schematic of SPARROW sources and transport. 10 Figure 2-2: Waitaki River catchment showing streams of order ≥ 3, lakes and point sources. 11 Figure 2-3: The land use in the customised CLUES (ECan, pers. comm .). 14 Figure 2-4: Waitaki River sub-catchments showing streams of order ≥ 3, lakes and calibration sites. 38 Figure 3-1: Measured vs modelled TN and TP loads for the calibration sites in the Upper Waitaki. 50 Figure 3-2: Measured vs modelled TN loads for the calibration sites in the Lower Waitaki. 51
Waitaki Water Quality Catchment Modelling
Executive summary
Environment Canterbury requires a whole-of-catchment model for the Waitaki River catchment to provide a catchment-wide view over the likely impacts of land use changes on nutrient (total nitrogen and total phosphorus) loads. While the CLUES (Catchment Land Use for Environmental Sustainability) model was identified as being suitable for this purpose, the model required customisation to increase the spatial representation of current land use and soil drainage characteristics because of the diverse nature of the land uses, soils and rainfall. The development of the customised version of CLUES and its calibration against measured nutrient loads are described in this report. Additionally, the methods used to calculate loads for calibration are described, the sites suitable for calibration are identified, and the modelled or predicted loads are compared with the measured ones.
The model was applied and calibrated separately for the upper and lower sections of the Waitaki Catchment. The calibration results for the model varied with the Root Mean Square Error (RMSE) being 3 m 3/s for flow over the entire catchment, 34.35 t/y for total nitrogen in the Upper Waitaki catchment, 10.38 t/y for total nitrogen in the Lower Waitaki catchment, and 2.00 t/y for total phosphorus in the Upper Waitaki catchment. Environment Canterbury instructed that total phosphorus calibration was not to be done in the Lower Waitaki.
Uncertainty in the modelled loads arises from a number of sources, most notably limited data availability for nitrogen and phosphorus concentrations, both in terms of the number of sites for which water quality is also recorded and the percentage of water quality readings from these sites that were censored. With respect to the latter, techniques were used to enable the use of these concentration data. There is also uncertainty around the flows connected to hydro schemes within the catchment that were used to calculate loads. It was therefore considered wisest to focus on modelled percentage changes when comparing the results from various scenarios.
The CLUES model does not simulate groundwater and assumes that groundwater lags are zero (i.e., that stream concentrations reflect current land use). This means that the model calibration discussed here adjusted key coefficients (e.g., TN and TP yields and stream attenuation coefficients) to match current nutrient load observations. If there are significant groundwater lags in the region, then the CLUES results are likely to under-predict stream loads – that is, the effects of the recent growth in dairying will not yet be fully shown in the measured loads.
Waitaki Water Quality Catchment Modelling 5
1 Introduction Environment Canterbury (ECan) requires a whole-of-catchment model for the Waitaki River catchment to provide a catchment-wide view of the likely impacts of land use changes on nutrient (total nitrogen or TN, and total phosphorus or TP) annual loads in the river drainage network. The Catchment Land Use for Environmental Sustainability model (CLUES; Elliott et al. 2008, Semadeni- Davies et al. 2011) was identified as a suitable model. This model has been set up on a regional basis and has been calibrated nationally. However, to update and improve the spatial representation of the catchment, the default CLUES model was customised and recalibrated specifically for this application. The model was customised (called customised CLUES in this report) in order to provide ECan with a model that is better able to provide robust, defensible estimates of nutrient loads under current and future scenarios at a limited number of nodes in the Waitaki River catchment.
For the purposes of this report, the Waitaki River catchment was divided into Upper and Lower Waitaki catchments, and each was calibrated separately. For the latter, the measured nutrient loads at the bottom of the Upper Waitaki were entered as pseudo point sources into the top of the Lower Waitaki. Both TN and TP loads were calibrated for the Upper Waitaki catchment, whereas just TN load was calibrated for the Lower Waitaki catchment1.
Customisations included:
° Reconfiguration of the drainage network in the upper catchment to take account of the power scheme diversions. This involves prescribing the fraction of load that is diverted via the hydro canals.
° Reconfiguration of the drainage network to re-direct flows in the Kelland Pond/Wairepo Creek area to account for the groundwater divide not following surface topography in that area.
° Introduction of new land-use classes to match classes that are used in scenarios and associated N and P leaching lookup tables and developed by the Land Information Group and Landcare Research, and modification of the GIS user interface to import land-use maps with these classes. These classes split land use into sub-classes according to soil characteristics and rainfall.
° Modification to use N and P leaching lookup tables (developed by Landcare Research and ECan) instead of the simplified version of Overseer 6.1 used in default CLUES.
° Modification of the soil types to match types used in the N and P lookup tables, and importation of this information into the CLUES base information for each subcatchment. For P in the Lower Waitaki, the standard CLUES methods will be used (based on the simplified version of Overseer 6.1 used in default CLUES).
° Adjustment of model parameters where appropriate to improve the fit with measurements.
° Adjustment of flow rates to reflect the diversions.
1 ECan instructed that TP calibration not to be done in Lower Waitaki.
6 Waitaki Water Quality Catchment Modelling
This report describes the development and calibration of the customised version of CLUES for current land use. CLUES was calibrated against measured loads which were determined from nutrient concentrations and flow data from a number of sites in the catchment. This, in addition to model development, the water quality and quantity measurements used are described, the sites suitable for calibration are identified, and the modelled or predicted loads are compared with the measured ones. A brief overview of CLUES is also given.
The sub-catchments, streams of order ≥ 3 and the lakes are mapped in Figure 1-1, details about the nutrient point sources and calibration sites are given later in the report.
Waitaki Water Quality Catchment Modelling 7
Figure 1-1: Waitaki River sub-catchments showing streams of order ≥ 3 and lakes. See Table A-1 in Appendix A for the list of sub-catchments (small-case numbers). The border between the upper and lower catchments is shown in bold.
8 Waitaki Water Quality Catchment Modelling
2 Method
2.1 The CLUES model CLUES is a steady-state, spatially-distributed modelling system within ArcGIS which operates at a minimum scale of sub-catchments (~10 km 2 and above). CLUES simulates the effects of land use and farm practices on water quality as indicated by annual loads of total nitrogen, total phosphorus, total suspended sediments and E. coli . The basic spatial unit within CLUES is the River Environments Classification (REC; Snelder et al. 2010) river reach and surrounding contributing area, called a REC unit in this report. CLUES was developed by NIWA for the Ministry of Primary Industries (MPI) and the Ministry for the Environment (MfE) in partnership with AgResearch, Lincoln Ventures, Harris Consulting, Plant and Food Research and Landcare Research. CLUES is provided to users as a front- end interface for ESRI ArcGIS which queries a geo-spatial database that is provided with the model software. The geo-spatial input data comes from a range of national sources including the Land Cover Database, Agribase, and the Land Resource inventory (LRI, Newsome et al. 2008). CLUES has been calibrated nationally against available contaminant load data. The CLUES interface contains tools which allow users to develop land use change and farm practice scenarios. Farm practices are applied to dairy, sheep and beef and deer farming. CLUES results are provided as maps and tables which can be exported to other applications for further analysis or reporting.
The CLUES modelling system couples modified versions of several water quality models which are used for specific modelling tasks, these are:
° OVERSEER® (AgResearch, Wheeler et al. 2006) – a customised, pre-parameterised, and simplified version of OVERSEER® 6 is provided within CLUES which computes nutrient leaching for dairy, sheep and beef, and deer farming. It provides annual average estimates of nutrient losses from these land uses, given information on rainfall, soil order and topography. For other variables, such as stocking and fertiliser application rates, typical values are used based on the region and land use.
° SPARROW (SPAtially Referenced Regression On Watershed attributes) – predicts E. coli and sediment yields from all land uses and nutrient yields from sources other than pasture and horticulture. SPARROW is also used to simulate contaminant transport in the drainage network (i.e., annual average stream loads) and includes provisions for stream routing and loss processes (storage and attenuation). The modelling procedure was originally developed by the United States Geological Survey (Smith et al. 1997) and has since been applied and modified in the New Zealand context with extensive liaison with the developers. SPARROW has been applied to nitrogen and phosphorus routing in Waikato (Alexander et al. 2002) and subsequently to the whole New Zealand landscape (Elliott et al. 2005). The SPARROW sediment transport routines were assessed by (Elliott et al. 2008) and simulations compared favourably with measured sediment load data.
° SPASMO (Soil Plant Atmosphere System MOdel) – calculates the nitrogen budget for a range of horticultural enterprise scenarios. Detailed simulations for many cases (combinations of crops, climate, fertiliser use) have been run (using a daily time step) to build lookup tables that CLUES queries. It has been validated against data from grazed pasture (Rosen et al. 2004) and pasture treated with herbicide (Close et al. 2003, Sarmah et al. 2005).
Waitaki Water Quality Catchment Modelling 9
Further details on the modelling framework can be found in (Woods et al. 2006) and information on setting up and running CLUES scenarios can be found in the model manual (Semadeni-Davies et al. 2011).
2.1.1 Routing along the drainage network As noted above, in addition to simulating sediment and E. coli loads, the SPARROW component of CLUES is used to route contaminants along the drainage network. A schematic of the routing routine in Sparrow is shown in Figure 2-1. Contaminant loads generated by each reach’s REC unit from diffuse sources are added to the instream load for reach. The load of contaminant generated for a particular source type ( source load ) is the product of the amount of source (area of land cover) times a source coefficient (yield for diffuse sources). This source load is then modified by a land-to-water delivery term , which is an exponential function of a number of delivery variables (such as rainfall or land drainage class) and delivery coefficients. An additional source term for TP associated with mass erosion of sediment was also added (Elliott et al. 2008). These modified sources are then summed for a given REC reach to give the total load entering the associated stream reach. Annual loads from any point sources located within the REC unit (as shown in Figure 2-2 and Table 2-1 for Waitaki) are added to total load as a model input. In-stream losses are modelled by a first-order decay term, and the load is then accumulated and attenuated during movement down the reach or stream network. A separate attenuation factor for reservoirs (e.g., lakes), is also calculated (Elliott et al. 2005). The result of the calculations is the modelled mean annual load for each stream reach.
Source Source
Land -to -water Sub -catchment delivery
Lake Point source Monitoring site
Figure 2-1: Schematic of SPARROW sources and transport.
10 Waitaki Water Quality Catchment Modelling
Figure 2-2: Waitaki River catchment showing streams of order ≥ 3, lakes and point sources. See Table 2-1 for a list of point sources (denoted by P).
Waitaki Water Quality Catchment Modelling 11
Table 2-1: Map key and annual nutrient loads for point sources. See Figure 2-2. Loads obtained from ECan which were based on a review of the discharge consents.
Label Name TN load (t/y) TP load (t/y)
P1 Salmon farm at Wairepo Arm/Ohau B 6.000 –
P2 Salmon farm at Ohau B-C 40.000 –
P3 Salmon farm at Ohau A 14.000 –
P4 Salmon farm at Tekapo B 19.400 –
P5 WWTP at Kurow 1.291 0.244
P6 Lake Ohau 0.100 0.025
P7 Twizel 3.371 0.884
P8 Omarama 1.604 0.360
P9 Lake Tekapo 2.129 0.779
P10 Mount Cook Village 0.921 0.200
P11 Otematata 0.921 0.200
2.1.2 CLUES customisation for Waitaki catchment This section describes how the default version of CLUES summarised above was adjusted for application to the Waitaki catchment by refining the characterisation of land use, reconfiguring some of the drainage network and adding flow diversions to simulate the effect of hydropower flow regulation.
Characterisation of geo-spatial data
CLUES represents land use in each REC unit by the percentage of the REC unit area covered by various land use classes including agriculture, crops and horticulture. Soil within each REC unit is represented by the area weighted average drainage class (i.e., poor to well drained) and by the dominant NZ soil order (e.g., ultic, podzols etc.,) taken from the LRI. Rainfall is represented by the reach’s annual average rainfall.
While the spatial scale of the model has remained unchanged, and the model still uses soil and rainfall as described above as model inputs, the customised version of CLUES has refined the characterisation of land use to take into account the influence of intra-unit variations in soil and rainfall on nutrient losses from different land use classes. Moreover, the default stock land uses were extended to include the type of irrigation, dairy for example, has been replaced by dairy and dairy support with no irrigation, with border dykes or with spray irrigation. That is, each REC unit was divided into unique combinations of land use (inclusive of irrigation) soil and rainfall class each with their own set of nutrient generated yields. There are 114 and 531 unique combinations in the Upper and Lower Waitaki catchments respectively. The land use proportions in the default model were then replaced by the proportions of each combination. The spatial disaggregation leading to the various
12 Waitaki Water Quality Catchment Modelling
combinations and their respective nutrient yields were provided by ECan. The proportion of each combination aggregated from REC units by river subcatchment for the calibrated water quality sites is given in Appendix B and the leaching rates for each combination are discussed further below and are given in Appendix C. These refinement enables the customised CLUES to better represent the Waitaki catchment in terms of land use/soil/rainfall with the hope of improving model fit. For example, in the customised Waitaki model, a REC unit which was originally classified in the default version as half and half dairy and arable land may, may be reclassified as 50% by area of dairy with spray irrigation/a medium-deep soil/800 mm of annual rainfall and 50% arable with no irrigation/a light soil/650 mm of annual rainfall. Another example could be a REC unit originally classed as dairy being split in the customised version into a combination of three dairy areas:
° dairy/no irrigation/a poorly drained soil/500 mm of annual rainfall
° dairy/spray irrigation/a light soil/650 mm of annual rainfall
° dairy/borderdyke irrigation/a medium-deep soil/800 mm of annual rainfall. The land use types in the default CLUES have been replaced in the customised version by land use and irrigation classes mapped in Figure 2-3. These were further split by the soil and rainfall classes given in Table 2-2. Table 2-3 and Table 2-4 describe the soil characteristics in Table 2-2 for the Upper and Lower Waitaki catchments respectively. Annual rainfall has been categorised into four bands relating to 475, 500, 650 and 800 mm/year. As described above, this breakdown or disaggregation is for the purpose of applying nutrient yields to each of the unique combinations.
Waitaki Water Quality Catchment Modelling 13
Figure 2-3: The land use in the customised CLUES (ECan, pers. comm .). See Table 2-2 for descriptions of land use, Table B-1 in Appendix B for the percentage of land use by area for each of the watersheds of the calibrated water quality monitoring sites, and Table A-1 in Appendix A for the sub-catchment.
14 Waitaki Water Quality Catchment Modelling
Table 2-2: Combinations of land use, rainfall and soil types in the Upper and Lower Waitaki River catchments used in the customised version of CLUES (ECan, pers. comm .). UW Land use in Upper Waitaki (UW). LW Land use in Lower Waitaki (LW). 1 475, 500, 650 and 800 are millimetres of annual rainfall. See Table 2-3 and Table 2-4 for a description of the soils.
Land use Description Rainfall for Rainfall Soils for UW Soils for LW UW 1 for LW 1
Arable UW Arable UW475, Light, Medium- UW650, deep, Poorly UW800 drained
Arable_Bdyke_Irr LW Arable, borderdyke Blank, Class 4 to LW500, irrigation 6, Class 6, Class LW650, 7, H, L, M, Pd, LW800 PdL, VL, XL
Arable_Dry LW Arable, no irrigation LW500, Blank, Class 4 to LW650, 6, Class 6, Class LW800 7, H, L, M, Pd, PdL, VL, XL
Arable_Spray_Irr LW Arable, spray LW500, Blank, Class 4 to irrigation LW650, 6, Class 6, Class LW800 7, H, L, M, Pd, PdL, VL, XL
Dairy_Bdyk UW, LW Dairy, borderdyke UW475, LW500, Light, Medium- Blank, Class 4 to irrigation UW650, LW650, deep, Poorly 6, Class 6, Class UW800 LW800 drained 7, H, L, M, Pd, PdL, VL, XL
Dairy_Dry LW Dairy, no irrigation LW500, Blank, Class 4 to LW650, 6, Class 6, Class LW800 7, H, L, M, Pd, PdL, VL, XL
Dairy_Spra UW, LW Dairy, spray irrigation UW475, LW500, Light, Medium- Blank, Class 4 to UW650, LW650, deep, Poorly 6, Class 6, Class UW800 LW800 drained 7, H, L, M, Pd, PdL, VL, XL
DairySuppB UW, LW Dairy support, UW475, LW500, Light, Medium- Blank, Class 4 to borderdyke irrigation UW650, LW650, deep, Poorly 6, Class 6, Class UW800 LW800 drained 7, H, L, M, Pd, PdL, VL, XL
DairySuppS UW, LW Dairy support, spray UW475, LW500, Light, Medium- Blank, Class 4 to irrigation UW650, LW650, deep, Poorly 6, Class 6, Class UW800 LW800 drained 7, H, L, M, Pd, PdL, VL, XL
Waitaki Water Quality Catchment Modelling 15
Land use Description Rainfall for Rainfall Soils for UW Soils for LW UW 1 for LW 1
DairySuppD UW, LW Dairy support, no UW475, LW500, Light, Medium- Blank, Class 4 to irrigation UW650, LW650, deep, Poorly 6, Class 6, Class UW800 LW800 drained 7, H, L, M, Pd, PdL, VL, XL
Deer_BDyke LW Deer, borderdyke LW500, Blank, Class 4 to irrigation LW650, 6, Class 6, Class LW800 7, H, L, M, Pd, PdL, VL, XL
Deer_Dry LW Deer, no irrigation LW500, Blank, Class 4 to LW650, 6, Class 6, Class LW800 7, H, L, M, Pd, PdL, VL, XL
Deer_Spray LW Deer, spray irrigation LW500, Blank, Class 4 to LW650, 6, Class 6, Class LW800 7, H, L, M, Pd, PdL, VL, XL
SBF_BDyke UW Sheep & beef on the UW475, Light, Medium- flat, borderdyke UW650, deep, Poorly irrigation UW800 drained
SB_BDyke LW Sheep & beef, LW500, Blank, Class 4 to borderdyke irrigation LW650, 6, Class 6, Class LW800 7, H, L, M, Pd, PdL, VL, XL
SBF_Dry UW Sheep & beef on the UW475, Light, Medium- flat, no irrigation UW650, deep, Poorly UW800 drained
SB_Dry LW Sheep & beef, no LW500, Blank, Class 4 to irrigation LW650, 6, Class 6, Class LW800 7, H, L, M, Pd, PdL, VL, XL
SBF_Spray UW Sheep & beef on the UW475, Light, Medium- flat, spray irrigation UW650, deep, Poorly UW800 drained
SB_Spray LW Sheep & beef, spray LW500, Blank, Class 4 to irrigation LW650, 6, Class 6, Class LW800 7, H, L, M, Pd, PdL, VL, XL
SBH_Dry UW Sheep & beef on hill UW475, Light, Medium- country, no irrigation UW650, deep, Poorly UW800 drained
16 Waitaki Water Quality Catchment Modelling
Land use Description Rainfall for Rainfall Soils for UW Soils for LW UW 1 for LW 1
SBF_Dry_Dev UW Sheep & beef on the UW475, Light, Medium- flat, no irrigation, UW650, deep, Poorly developed land UW800 drained
SBH_Dry_Dev UW Sheep & beef on hill UW475, Light, Medium- country, no UW650, deep, Poorly irrigation, developed UW800 drained land
ExoticFor UW, LW Exotic forest UW475, LW500, Light, Medium- All, Blank UW650, LW650, deep, Poorly UW800 LW800 drained
NativeFor UW, LW Native forest UW475, LW500, Light, Medium- All, Blank UW650, LW650, deep, Poorly UW800 LW800 drained
Other UW, LW Other land covers, UW475, LW500, Light, Medium- All, Blank e.g. ice, bare soil, UW650, LW650, deep, Poorly rock UW800 LW800 drained
Tussock UW, LW Tussock UW475, LW500, Light, Medium- All, Blank UW650, LW650, deep, Poorly UW800 LW800 drained
Scrub UW, LW Scrub UW475, LW500, Light, Medium- All, Blank UW650, LW650, deep, Poorly UW800 LW800 drained
Urban UW, LW Urban UW475, LW500, Light, Medium- All, Blank UW650, LW650, deep, Poorly UW800 LW800 drained
Table 2-3: Soils in the Upper Waitaki (ECan, pers. comm.).
Name Available water to a 60 cm depth (mm)
Light <60
Medium-deep ≥ 60
Poorly drained Poorly drained or very poorly drained
Waitaki Water Quality Catchment Modelling 17
Table 2-4: Soils in the Lower Waitaki (ECan, pers. comm .).
Name Assumption
All A convenience group – used for a set of non-productive land uses.
Blank Gaps in the soil layer, most commonly riverbed/water/rock
Class 4 to 6 Hill soils – equivalent to light soils in Upper Waitaki
Class 6 Hilly/steep soils – equivalent to light soils in Upper Waitaki
Class 7 Steep soils – equivalent to light soils in Upper Waitaki
XL Equivalent to light soils in Upper Waitaki
VL Equivalent to light soils in Upper Waitaki
L Equivalent to light soils in Upper Waitaki
M Equivalent to medium-deep soils in Upper Waitaki
H Equivalent to medium-deep soils in Upper Waitaki
Pd Equivalent to poorly drained soils in Upper Waitaki
PdL Equivalent to poorly drained soils in Upper Waitaki
TN and TP leaching rates
As stated above, leaching rates were provided by ECan and varied according to the land use, soil type and rainfall combinations; these are given in Table C-1 and Table C-2 in Appendix C.
In the default version of CLUES, leaching rate tables are held in a geodatabase that is inaccessible to the user. For the Waitaki customised version, they were made available via a lookup table that the user can access and alter if necessary. The lookup table consists of three columns: the first lists the land use/soil/rainfall combinations, and the next two columns have the corresponding leaching rates for N and P.
Flows
The default version of CLUES uses estimated flows from Woods et al. (2006). The customised version instead uses a combination of measured flows where available and estimated flows. Some of the estimated flows from the default version were also updated in the customised version using more recent data from flow monitoring sites. Corrections between the old flows and updated flows were done by calculating the percentage difference between old and updated values at the flow monitoring station, then propagating this difference to all the downstream reaches, right down to the sea. Table 2-5 and Table 2-6 compare the updated flows in the customised version with the flows in the default version used for the water quality calibration sites.
For example, the flow at bottom of the Upper Waitaki catchment (see Waitaki at Kurow site in Table 2-5) for the default and customised versions was 435 and 354 m 3/s respectively, with the measured flow being 360 m 3/s. Similarly, the flow at the bottom of the Lower Waitaki catchment, i.e., at the
18 Waitaki Water Quality Catchment Modelling
coast, for the default and customised versions was 449 and 371 m 3/s respectively. The measured flow at Waitaki at SH1 Bridge which is a site near the coast is 367 m 3/s. Therefore the customised version better fits the measured flow better at the bottom of the Upper and Lower Waitaki catchments.
The fit of the default and customised versions to the measured flows is described using the root mean square error (RMSE) 2 for the Upper and Lower Waitaki (Table 2-5 and Table 2-6). The RMSE is calculated using the following equation (Chai & Draxler 2014):
RMSE = √ ∑ − / (2.1) The RMSE for the default and customised versions of CLUES equals 62 and 3 respectively. This means that the customised version is a better fit to the measured data than the default version.
2 The RMSE is used as a standard statistical metric to measure model performance in many fields, including meteorology, air quality, climate research and agriculture. It assumes the errors (= modelled – measured) are unbiased and follow a normal distribution (Chai & Draxler 2014).
Waitaki Water Quality Catchment Modelling 19
Table 2-5: Measured, default CLUES and customised CLUES flows for the water quality calibration sites in the Upper Waitaki. . The water quality site used the flow site(s) in the same row to calculate the nutrient loads. Water quality sites without superscripts 1 or 2 have coincident flow data.
Flow site name Flow site ID Mean measured Flow from Flow from Water quality site Water quality site Approximate flow (m3/s), date default CLUES customised CLUES name ID distance range (m3/s) (m3/s) between flow site and water quality site (m)
– 19.72 16.73 Ahuriri River M1 0 Headwater (upper Ahuriri) 1
Ahuriri at South 71116 23.27, 25.24 23.89 Ahuriri River M3 32500 3 2 Diadem 1/1/1990– mouth 31/12/2013
Grays River at 1875 2.94, 5.09 3.60 Grays River - SQ35117 0 Above Tekapo 1/1/1990– Lower Above Ford Confluence 31/12/2013
Hen Burn @ U/S 2146 0.78, 0.54 0.63 Henburn Rd 2 SQ10824 600 Quail Burn Downs 15/10/1986– Intake 17/12/2013
Mary Burn at SH8 71130 0.57, 0.93 0.74 Maryburn SH8 SQ10275 0 12/6/2003– Bridge 14/1/2014
Mary Burn @ 1872 2.75, 2.89 3.02 Maryburn Stream SQ35115 0 Above Tekapo 1/1/1990– - Lower u/s Confluence 31/12/2013 Tekapo River
20 Waitaki Water Quality Catchment Modelling
Flow site name Flow site ID Mean measured Flow from Flow from Water quality site Water quality site Approximate flow (m3/s), date default CLUES customised CLUES name ID distance range (m3/s) (m3/s) between flow site and water quality site (m)
Ohau C Power 38748 258.15, 0.0007 266.00 Ohau C M10 0 Station at 22/9/1985– Machine Output 6/1/2014
Omarama at 71136 2.09, 1.99 2.54 Omarama Stream SQ10005 400 2 Wardells Bridge 3/8/1988– Omarama (SH8) 31/1/2014
Quailburn 71118 0.89, 0.88 0.55 Quailburn Road SQ35792 0 15/10/1986– Recorder 17/12/2013
– 0.24 0.18 Sutherlands Creek SQ10037 0 Ben Omar Road 1
Forks at Balmoral 71129 3.17, 3.82 3.16 9600 1/1/1990– 31/12/2013
Tekapo at Spillway 71131 14.95, 110.21 5.00 Tekapo at Forks 2 M11 7700 6/6/1968– 7/11/2013
Total = 18.12 Total = 114.03 Total = 8.16
Waitaki Water Quality Catchment Modelling 21
Flow site name Flow site ID Mean measured Flow from Flow from Water quality site Water quality site Approximate flow (m3/s), date default CLUES customised CLUES name ID distance range (m3/s) (m3/s) between flow site and water quality site (m)
Mary Burn @ 1872 2.75, 2.89 3.02 1600 Above Tekapo 1/1/1990– Confluence 31/12/2013
Tekapo Grays River at 1875 2.94, 5.09 3.60 downstream M4 3500 Above Tekapo 1/1/1990– Greys Hill 2 Confluence 31/12/2013
Total = 5.69 Total = 7.98 Total = 6.62
– 300.39 31.05 Tekapo Pukaki M12 0 Mouth 1
Waitaki at Kurow 71104 360.32, 435.49 354.10 Waitaki at Kurow 71104 0 7/9/1964– 18/11/2013
Willow Burn at 1071110 0.92, 0.33 0.66 Willowburn SQ10012 0 Quailburn Rd 14/6/2013– Quailburn Road 14/1/2014 Bridge
Mary Burn at Mt 71122 0.55, 0.72 0.55 Mary Burn Mary SQ26372 1200 2 MacDonald 1/1/1990– Burn Fill 31/12/2013
– 1.14 0.60 Wairepo Creek SQ10804 0 Arm Inlet 1
22 Waitaki Water Quality Catchment Modelling
1 No measured flows so CLUES flow used. 2 Flow and water quality sites not coincident but data from the closest flow monitoring site were adjusted and used. 3 See Footnote in Section 2.2.1.
Table 2-6: Measured, default CLUES and customised CLUES flows for the water quality calibration sites in the Lower Waitaki. The water quality site used the flow site(s) in the same row to calculate the nutrient loads. Water quality sites without superscripts 1 or 2 have coincident flow data.
Flow site name Flow site ID Mean measured Flow from Flow from Water quality site Water quality site Approximate flow (m3/s), date default CLUES customised CLUES name ID distance range (m3/s) (m3/s) between flow site and water quality site (m)
Cattle Creek at 73 0.47, 0.09 0.21 Cattle Creek SQ10814 4500 Cattle Yards 1/1/1990– Morland 2 31/12/2013 Settlement Road
– 0.01 0.12 Rocky Point SQ10816 0 Stream Hakataramea Valley Road 1
– 0.02 0.03 Deadman Stream SQ10818 0 Hakataramea Valley Road 1
– 0.34 0.17 Penticotico Stream SQ10174 0 SH83 1
– 0.32 1.05 Otiake River Mt SQ10167 0 Bell Station 1
Waitaki Water Quality Catchment Modelling 23
Flow site name Flow site ID Mean measured Flow from Flow from Water quality site Water quality site Approximate flow (m3/s), date default CLUES customised CLUES name ID distance range (m3/s) (m3/s) between flow site and water quality site (m)
Maerewhenua 2006 2.49, 2.18 2.57 Maerewhenua SQ10160 0 River at SH83 1/1/1990– River Duntroon Bridge (Duntroon) 31/12/2013
– 0.16 0.15 Waikakahi Stream SQ21160 0 Cock & Hen Road 1
Hakataramea at 71103 5.63, 6.78 5.67 Hakataramea at 71103 0 Above MHBr 1/1/1990– Above MHBr 22/10/2014
– 0.003 0.003 Waikakahi Stream SQ21255 0 Old Ferry Road 1
Otekaieke River at 71102 2.48, 1.05 1.14 Otekaieke River SQ35871 1800 Weir 30/1/2013– D/S of Bushy 2 16/7/2014 Creek
Waikakahi at Te 71195 0.59, 0.56 0.48 Waikakahi Stream SQ21162 0 Maiharoa Rd 23/5/2001– Glenavy Tawai Rd 4/8/2014
Waikakahi at Te 71195 0.59, 0.56 0.48 Waikakahi Stream SQ21254 0 Maiharoa Rd 23/5/2001– Te Maiharoa Road 4/8/2014
1 No measured flows so CLUES flow used. 2 Flow and water quality sites not coincident but data from the closest flow monitoring site were adjusted and used
24 Waitaki Water Quality Catchment Modelling
Flow diversions
The flow diversions due to the hydro scheme were introduced in the customised version of CLUES, with Table 2-7 giving a summary. There are four hydro dams in the catchment and flow regulation from these has changed the natural flow paths requiring flow diversion to be taken into account in the model (which doesn’t happen in the default). Diversions range from 85% of the annual flow from Lake Ohau to 99% of the annual flow from Lake Ruataniwha (see Table 2-7).
The diversions were modelled by splitting the flow and nutrient loads from the outlet reach of each lake between the next REC reach in the REC flow sequence and a second reach representing the divert. Details on how the flow distributions were estimated are given in Appendix D.
Table 2-7: Estimated flow diversions in the Waitaki River catchment.
Lake or river Outlet Flow distribution (%)
Tekapo Canal 95 Lake Tekapo Tekapo River 5
Ohau C Canal 99 Lake Ruataniwha (including Wairepo Arm) Lower Ohau River 1
Ohau A Canal 85 Lake Ohau Upper Ohau River 15
Pukaki Canal 95 Lake Pukaki Pukaki River 5
Ahuriri River 70 Wairepo Creek Wairepo Arm 30
2.2 Measured water quality and flow data The flow and TN and TP concentration data that were used to calculate the measured mean annual loads came from three sources: ECan, NIWA and Meridian Energy. These data are described below.
2.2.1 Flows
Load for a point in space and time is calculated as the product of flow and concentration, and for this reason flow data were needed for the calculation of loads. However, as seen in Table 2-5 and Table 2-6, not all the water quality monitoring sites have coincident flow data recorded at the site. For some of these water quality sites, flow data from the closest flow monitoring site were adjusted and used instead, see below for details. For the rest of these water quality sites, i.e., ones that had no
Waitaki Water Quality Catchment Modelling 25
flow monitoring site close by, CLUES estimated flows (Woods et al. 2006) were used for the load calculations.
For those water quality sites that have no measured flow data but have a flow monitoring site close by, an estimate of the measured flow at the water quality site was calculated as follows:
° the modelled mean flow at the water quality site (Q(mean wq )mod ) from Woods et al. 3 (2006) was divided by the modelled mean flow (Q(mean flow )mod ) at the closest flow site (i.e., has measured flow data) – this quotient called ‘multiplier’.
° The ‘multiplier’ was then applied to the measured flow at the flow site (Q(flow) meas ) to
obtain an estimate of the measured flow at the water quality site (Q(wq) meas ).