SDC Stratford WWTP Annual Report 2023-2024
SDC Stratford WWTP Annual Report 2023-2024
SDC Stratford WWTP Annual Report 2023-2024
owns the venue through the Taranaki Stadium Trust, said contractors had pulled out all the stops to get the roof done and dusted but the winter weather has meant the construction crew had been unable to complete this part of the project safely. “The team has worked very hard to get the roof installed in time for this season’s games but unfortunately the weather has not played ball. The project team had allowed for 25 rain days in the programme and the number of rain delay days to the project has
page Doc. No: 2835178 TARANAKI REGIONAL COUNCIL MONTHLY RAINFALL AND RIVER REPORT FOR July 2021 Provisional Data Only Note: some sites record a number of parameters Table 1: Rainfall at 27 sites throughout the region Station Sub-region Monthly Year to Date Records Began Number of rain days (>0.5mm) Total Monthly Rainfall (mm) % of Monthly Normal (%) Total to date (mm) % of Normal for year to date % of average full calendar year Nth Egmont
material deposited on the ground in the log and coal storage areas. When it rains this material washes into the stormwater system, and discharges into the harbour via the numerous piped outlets. To minimise deleterious effects on the receiving environment, Port Taranaki have implemented several preventative measures since 2012, including upgrading the stormwater treatment system and improving stormwater management procedures. This work is ongoing, as log exports continue to increase. Another
Autumn arrived in Taranaki in March with an average air tempeature of 14.5°C - 1.7°C cooler than normal. The highest temperature was 25.7°C at Inglewood at Oxidation Ponds. There was an average of 95.9mm rainfall – 14% less than usual – although there were some big downpours on te Maunga with 374.5mm at the North Egmont Visitors Centre and 351mm at Dawson Falls. There was 41% less rain at Brooklands Zoo at New Plymouth and 33% more at Kotare at OSullivans. Mean river flows for March were 38.7%
2015 with 15.192m recorded as stage height at Riminui station, in the middle of the Waitotara catchment. This compared with 13.5m at the same site recorded in 2004 and 10.8 in July 2006.This was the highest water level recorded since the site was installed in 1993. Riminui recorded a total rainfall of 307.5mm (226% of normal) for the month of June, with 174 mm of that total falling over the 19-20 June period. Despite the high levels of rain and river flow, the peak flood levels in the
of Waitara East School on their epic Taranaki Mounga Field Trip! [Taranaki Regional Council] 5,141 224 8 July was wet, wet, wet! Dawson Falls had a whopping 1,418mm of rain in July…. (map) [Taranaki Regional Council] 4,340 62 9 CONNECTOR SERVICE ALERT - Tuesday 2nd August 2022 OFF-PEAK SERVICES CANCELLED Waka Kotahi will be completing high priority asphalt repairs at Tariki on TUESDAY 2nd August. 3.182 16 Executive, Audit & Risk Committee - Financial and
August was exceptionally wet, with many rain-gauges collecting more than twice the typical rain for the month. The average was 176.6% of the long-term average, and ranged from 80% at Rimunui Station to 387% at Dawson Falls. Year to date rainfall is sitting between 113% (Manganui at SH3 Midhirst) and 211% (Dawson Falls) with an average of 141.7% of normal. Cape Egmont remains at around 211% of normal to date and has already received 95% of a typical year’s rain in eight months. Mean river flows
January was warmer than usual while rainfall for the month was just slightly above normal – but with some big differences across the region. Waitotara at Ngutuwera had 53% less rain than usual while Uruti at Kaka Rd had 39% more. The average rainfall for the region was 108.4mm, 2% more than usual. The average air temperature for the region (excluding Te Maunga sites) was 18.2°C, which is 0.6°C warmer than long-term January averages. The highest temperature was 30.3°C at Waitotara at Hawken Rd.
flank, causing fires in the native bush which swept 3km northwards across the western slopes of the Pouakai Range (Druce, 1970, cited in Neall, 2003). 150 years later a pumice lapilli fall and pyroclastic flows covered Maori villages, inferred from the discovery of Maori ovens (umu) beneath the deposits. In 1755 A.D. small hot avalanches occurred from eruptions at Taranaki. Recent evidence from Platz (2007) suggests that the most recent eruption was between 1839 and 1866 A.D., and potentially in