As a regional function Gisborne District Council has the responsibility to monitor and manage rivers in the Gisborne district. We have live monitoring on a number of rivers, where you can see up-to-date river level information.
Summer flow data
During summer, flow data is plotted on a rating curve fortnightly and emailed to water permit holders during prolonged particularly dry periods. This provides users with up-to-date flow information to help with planning irrigation, and an overall view of river fluctuations over the entire irrigation seasons.
More information on river low flows
Gisborne district rivers
The Gisborne district contains the headwaters of 4 major rivers that flow into other regions. The Hangaroa River flows south into Hawke’s Bay; the Motu, Waioeka and Waikura rivers flow into the Bay of Plenty. The north-flowing rivers are clear, fast-flowing and highly regarded for their recreational value of fishing, canoeing and white-water rafting.
The Waipaoa River catchment is extensively farmed. It covers 216,484 ha and has formed the fertile and highly productive Poverty Bay flats on the edge of Gisborne city. It is an important source of water for irrigation, a back-up source of water for Gisborne city, and the major recharge source for extensively used aquifers. Key subcatchments of the Waipaoa include the Waikohu, Mangatu, Waingaromia, Wharekopae, and Te Arai.
Some of the subcatchments are particularly susceptible to soil erosion, notably in the Waingaromia and Mangatu areas. As a result, the bed in the lower reaches of the catchment is building up due to sediment and gravel deposition. The Poverty Bay flats and the city are protected by the stopbanks of the Waipaoa River Flood Control Scheme but since their construction 60 years ago, flood capacity has been lost and the scheme is about to be upgraded again at substantial cost. Annual suspended sediment load for the Waipaoa catchment is 15 million tonnes or 33.54 cubic metres per second. This amount of sediment enters Poverty Bay.
Despite the high sediment loads of the lower reaches of the Waipaoa catchment many of the tributaries in the headwaters provide habitat for a range of indigenous fish species. These species rely on migration up the river system as juveniles and return to the sea as adults. Eels are one example in the fishery that requires this ability to migrate. Trout are present in the Wharekopae tributary. They have been introduced and are not known to migrate.
The Waipaoa River is the main source of surface water for irrigation on the Poverty Bay Flats and the major recharge source for aquifers.
Information on Waipaoa River low flow
The Waikohu River is one of 5 main tributaries of the Waipaoa River which is the main source of surface water for irrigation on the Poverty Bay flats. Prior to 2001 the Waikohu River had largely been an untapped water resource, other than for permitted takes, and there was no water strategy or allocation plan in place for this river. Currently there are 5 irrigation takes and one small scale hydro-power diversion.
The Maraetaha River is a meandering river with the river channel comprising of pools and riffles. The river is known to be saline from the river’s mouth up to the Maraetaha state highway No.1 bridge.
Te Arai River
The Te Arai River, located to the south-east of Gisborne, is also a tributary of the Waipaoa and has a catchment of approximately 18,900 hectares. The upper catchment of 1,050 hectares is in native bush and is managed by the Gisborne District Council as the catchment for the main water supply to Gisborne city. The river then flows through steeper pastoral land and out to lowland plains.
The Te Arai River flows into the Waipaoa River approximately 4.5km upstream of the river mouth. The lower Waipaoa and the lower reaches of the Te Arai experience tidal effects and associated water quality. There are 12 water permits including one for frost protection.
Information on Te Arai River low flow
The Taruheru River flows through a highly modified environment which includes horticultural and agricultural land and residential properties.
The Waiapu River is formed with the joining of the Mata River, which flows north-east from the Raukumara Ranges, with the Tapuaeroa River near Ruatoria township. The Waiapu is perhaps the most famous river in our region from a perspective of pre-European history. Its name is found in Tahiti and it offered a protected region where people could settle and find safety in times of war, the river valley is referred to in a tribal saying: “Hoake tāua ki Waiapu ki tātara e maru ana.” In English this means “Let us shelter under the thick matted cloak of Waiapu.” (source www.teara.govt.nz(external link))
Further inland, the Waitohaia River flows into the Mata River.
The Waiapu River has a catchment of 173,400 hectares, much of which is very prone to erosion. Much progress has been made over the past 40 years in planting the eroding areas and encouraging native scrub reversion, but the Waiapu remains the most sediment laden river in the district. The annual suspended sediment load is 36 million tonnes, this equates to 90.47 cubic metres of sediment flowing out to sea per second.
The eroding gravels are rapidly raising the bed of the river in the lower reaches, causing riverbank erosion that is threatening Ruatoria township. A number of bridges over tributaries have been raised in recent years in response to rising riverbeds. The river catchment is mostly covered in native bush (more than 80%) with the remaining area covered in scrub and coastal forest.
Waiapu River Catchment Study
The Ngati Porou deed of settlement recognises the significance of the Waiapu River to Ngati Porou. The Crown formed a Waiapu River Catchment Erosion Assessment Project Steering Committee with representatives from Ministry of Primary Industries, Department of Conservation, Ministry for Environment, Ngati Porou and Council. The committee commissioned an independent assessment of the size and scope of issues impacting on erosion in the catchment.
The study, by Crown Research Institute Scion, confirmed that the rates of natural erosion and sedimentation are high in the Waiapu catchment and afforestation, where it has been applied, is a most effective method of controlling erosion.
East Coast rivers
The area of land to the east of the Raukumara Ranges contains 2 main catchments the Waipaoa and Waiapu, but smaller coastal catchments include the Awatere and Uawa. The geology of the Gisborne region is complex but generally comprises sedimentary sandstone and mudstone geology in the upper catchments of the Waipaoa and Waiapu River catchments. Hillside erosion, slips and river aggradation are common in the East Coast region, the Waipaoa and Waiapu Rivers are examples of aggrading rivers.