BRIEF REVIEW of the WEATHER Percent of Normal in Much of Canterbury and As Low As 50 Percent of Normal in Coastal WINTER 1988 (Fig

Total Page:16

File Type:pdf, Size:1020Kb

BRIEF REVIEW of the WEATHER Percent of Normal in Much of Canterbury and As Low As 50 Percent of Normal in Coastal WINTER 1988 (Fig Weather and Climate (1989) 9: 29-36 29 NEW ZEALAND WEATHER BRIEF REVIEW OF THE WEATHER percent of normal in much of Canterbury and as low as 50 percent of normal in coastal WINTER 1988 (Fig. 1) areas of North Otago. Rainfall for winter was above normal in The mean temperature for New Zealand, calculated from 7 indicator stations (one of central highcountry regions of the North Is- which goes back to 1853) was 9.1°C. This was land, Wanganui, Manawatu, along the west 1.0°C above normal and was the third highest coast of the South Island, in Southland, Otago recorded. The warmest winter was that of and inland highcountry areas of Canterbury. The wettest regions were Manawatu, South 1984 when 9.4°C was recorded. In some places Westland and inland areas of Southland and in central Otago and inland Canterbury mean temperatures were as high as 1.5-2°C above Otago, where rainfall totals ranged between normal. 150 and 190 percent of normal. It was drier than usual in all regions of New One of the major factors which contributed Zealand which were sheltered from the west to the warmer weather was that there were and south-west. Rainfall was less than 60 fewer periods of very cold southerly condi- .1.0 +0.6 —0,6 —1.0 SUNSHINE Pereentege of Normal (1061-00) Seimrture from Mks, 0051 -00) WINTER WINTER ((IV))TEMPERAXURE Nme Zei•land Meteorological Service Neer Unload Mettorotogmal Service 1 Fig. 1: Winter 1988. Rainfall (a) maps based on observations from 46 stations; temperature (b) departure maps based on observations from 43 stations; sunshine (c) based on observations from 33 stations. 30 New Zealand Weather Conditions were generally windier than usu- al in the south of the North Island, and over much of the South Island, especially in South- land and Otago where windy days (gusts of at ISO least 34 knots) occurred with almost twice the 120 normal frequency. Strong winds (recorded by radar balloon flights) at midday, over South- 80 land occurred on 44 percent of the days. This 50 was the most since 45 percent in 1949. MONTHLY SUMMARIES JUNE-AUGUST 1988 June was warmer than usual. Mean daily temperatures were at least 0.5°C above normal throughout much of New Zealand. They were 1.5-2°C higher in places north of Auckland, in western Bay of Plenty, western regions of the North Island from Waikato to Manawatu and in inland Canter- RAINFALL of Nom, (1051-00, WINTER 1988 bury. A very low air temperature of -8.4'c was Mow notiond ifetoorolcoficol Service recorded at Dunedin Airport on the morning of the 16th, together with a -10.3°C ground frost. This was the lowest air temperature recorded there in any month since records began in 1963. Temperatures as high as 22.5°C tions than is usual, and these lasted for only were recorded at Christchurch Airport in brief periods of time. For example, the aver- age number of days in winter (1931-74) with warm dry northwesterly conditions on the 8th. This was the highest in 33 years of records. A maximum temperatures of less than 8.0°C recorded at Kelburn is 9. This winter there maximum temperature of 24.2°C was record- were only 2. ed at Napier Airport in similar conditions on the 19th, which was the highest measured Only one ground frost was recorded at Kel- since records began in 1954. burn (the normal is 2), which was the least since 1971 when there were none. This made Rainfall was only 30-40 percent of normal the winter the second least frosty at Kelburn in Hawkes Bay and northern parts of the since records began in 1928. Auckland region. It was also drier than norm- al in Northland, other parts of Auckland and Cloudier than normal conditions were re- in eastern regions of New Zealand sheltered corded in all western regions of the North from the south-west, where totals ranged Island north of Horowhenua and along the from 40-70 percent of normal. Rainfall was west coast of the South Island. The winter was 120-180 percent of normal in Manawatu, along rather cloudy in Auckland and Waikato. Hours the West Coast of the South Island and in of bright sunshine were only 76 percent of Central Otago. Totals were almost twice normal at Auckland City, which was the low- normal in South Westland. Only 378 mm (59% est since records began in 1963, and 77 per- of normal) was recorded at Kelburn in the 6 cent of normal at Ruakura which was the months ending 30 June. This was the lowest lowest since records began in 1937. since 287 mm in 1939 and the 9th lowest since Sunnier than normal conditions prevailed in recording began in 1862. Heavy rain, totalling eastern regions of New Zealand from Hawkes 153 mm, was recorded at Glenorchy (near Bay to South Canterbury. Just over 120 per- Awakino) in the 24 hours to 9am on the 8th. cent of normal sunshine was recorded at Five houses were evacuated and hundreds of hectares of farmland were flooded due to Christchurch Airport, making it the sunniest since 1959. heavy rain in the same area on the 19th. On New Zealand Weather 31 the same day heavy rain caused slips and ter many homes were flooded. About 10 closed the Manawatu Gorge road for a time. houses were seriously damaged by the water Hours of bright sunshine were 110-120 per- and more than 100 were evacuated. The flood cent of normal over much of the South Island. was reported as being the worst affecting the In Canterbury and Southland they were as region since 1976 and damage was estimated high as 125 percent of normal. Over the North at $2-3 million. Island it was cloudier than usual (especially in Drier than normal conditions were recorded Horowhenua and Manawatu with 65-75 per- in eastern regions of the South Island from cent of normal hours). The region from East Kaikoura to North Otago. In these regions Cape to Poverty Bay had near normal totals ranged from 40-60 percent of normal. sunshine. Only 8 mm was recorded at Oamaru. On the whole, July was wndier than average For the 7 months from 1 January to 31 July, over much of New Zealand, especially in the only 200 mm had been recorded at Christ- far south. church Airport. This was the least ever Strong winds occurred for 37 percent of the recroded for that period since records began time, for the period 1 January to 31 July over in 1944, being only 50 percent of normal. the south of the South Island. This was equal Temperatures were much warmer than to 37 percent in the same period in 1987, and usual over most of New Zealand in July. Mean was the highest since records began in 1956. daily temperatures were 1-1.5°C above norm- Rainfall was above normal in eastern re- al in many regions. They were about 2°C gions of the North Island north of Wairarapa, above in Waikato, Manawatu and eastern re- high country regions, Southland, much of gions of the South Island (north of Southland Otago and in most regions exposed to the west and coastal Otago). In some inland areas of or south-west. It was very wet in Auckland Canterbury and Otago they were as much as City, western Manawatu, Fiordland and 3°C above normal. The mean temperature for Southland, with totals being approximately New Zealand, calculated from 7 indicator sta- twice normal (and up to three times normal in tions, was 8.9°C. This was 1.3°C above normal Central Otago). A total of 154 mm (214% of and was the highest on record (equal with normal) recorded at Invercargill Airport was 8.9°C in 1985). The mean temperature record- the highest recorded there in July, since ed at Kelburn was 9.7°C (1.3°C above normal), records began in 1939. which was the second equal highest since records began in 1928. Other Wellington Heavy rain was recorded in Auckland on the records indicate that, for Kelburn, it was 17th, where in most places totals for the 24 likely to have been the second highest since hours to 9am on the 18th ranged from 60-95 1862. The highest was 9.8°C in July 1985. The mm, with some surface flooding. Flooding also occurred in Gisborne when over 100 mm mean temperature at Christchurch of 7.1°C was recorded in the 48 hours to 9am on the (2.0°C above normal) was the highest since 18th. A total of 304 mm was recorded at records began in 1954. Coromandel in the 72 hours to 9am on the Hours of bright sunshine were below normal 18th; 186 mm having been recorded in the 24 in most western regions of New Zealand. They hours to 9am on the 17th. were very low in Auckland, Bay of Plenty, Taranaki, and central regions of the North A total of 31 mm was recorded at Kelburn, Island, where they ranged from 65-80 percent Wellington, in moist north-west conditions, in of normal. Only 98 hours (74 % of normal) the hour from just before midnight on the 23rd were recorded at New Plymouth Airport, until just before 1 lam on the 24th. This which was the lowest since records began in equalled the all time record for one hour's rain at Kelburn.
Recommended publications
  • Regional Variation in New Zealand English Is Something of a Conundrum
    Regional variation in NZ English Regional variation in New Zealand English is something of a conundrum. Although a dialect of the Southland/Otago region is well-known and documented (Bartlett 1992, 2003; Hay, Maclagan and Gordon 2008), linguists have yet to find concrete evidence of other regional New Zealand English dialects. Yet the general New Zealand public are often adamant that there are regional differences in how New Zealand English is spoken. Folklinguistic evidence of regional variation Studies dealing with societal attitudes towards and beliefs about a language are called folklinguistic studies. Folklinguistic studies (Gordon 1997; Nielsen and Hay 2005) show that New Zealanders do tend to believe that there are regional differences in New Zealand English but, when asked to provide information about these differences, comments usually refer to characteristics of the region or the people living in the region rather than aspects of the language itself. For example, a study by Nielsen and Hay (2005) invited University students to rate their perceptions of New Zealand English in different regions according to its ‘pleasantness' and 'correctness' and to annotate a map of New Zealand with comments about speech in different regions. Although regions were rated differently, the ratings appeared to be based on stereotypes of the regions in question, rather than on any identifiable linguistic differences. People tended to rate their own region more highly for pleasantness and correctness and notes on the map mainly consisted of stereotypical descriptions such as ‘official’ for Wellington and ‘farmer speech’ for Taranaki. This inability to identify specific linguistic features that differ from one geographical area to the next stands in contrast to New Zealanders’ awareness of a ‘rolled’, or rather postvocalic /r/, in Southland.
    [Show full text]
  • 1. INTRODUCTION the Presentation and Interpretation of The
    Lecturer PhD Petronela SCUTARIU “Ștefan cel Mare” University of Suceava, Faculty of Law and Administration Sciences, Suceava, Romania [email protected] Student Liviu Otniel FEDUR “Ștefan cel Mare” University of Suceava, Faculty of Law and Administration Sciences, Suceava, Romania Android Developer, Protovate LLC, Hickory, North Carolina, USA Director, Livtech Soft SRL, Suceava, Romania [email protected] Abstract: The parallel examination of different states with their government systems is, was and will always be a necessary inurement for their in-depth knowledge and for the discovery of generalized orientations and developments. Regarding this affirmation, in the present article we intend to analyze from a comparative perspective two administrative systems, one from New Zealand and the other from South Africa, to identify the particularities in their organization and the way of functioning and to determine the similarities and differences between them. This research begins with the presentation of main identification data of the states, namely etymological explanations, continuing with the geographical locations and ending with the national emblems and flags. Afterwards, the present study provides insights into the genesis of the mentioned states, presenting brief historical records of how they appeared and developed. According to administrative-territorial organization criteria, New Zealand is divided into non-unitary and unitary regions, containing a territory as well, while South Africa is divided into provinces which, in turn, are divided into districts that are subdivided into local municipalities. From the point of view of the form of government, New Zealand is a unitary parliamentary constitutional monarchy, while South Africa is a unitary parliamentary republic with an executive presidency.
    [Show full text]
  • Apfsos/Wp/05 in Depth Country Study
    ASIA-PACIFIC FORESTRY SECTOR OUTLOOK STUDY WORKING PAPER SERIES Working Paper No: APFSOS/WP/05 IN DEPTH COUNTRY STUDY - NEW ZEALAND by Chris Brown Consultant FAO Forestry Planning and Statistics Branch Rome Forestry Policy and Planning Division, Rome Regional Office for Asia and the Pacific, Bangkok May 1997 Asia-Pacific Forestry Sector Outlook Study Working Paper Series No: 5 1 In Depth Country Study - New Zealand 2 Chris Brown The Asia-Pacific Forestry Sector Outlook Study is being undertaken under the auspices of the Asia-Pacific Forestry Commission. This report comes under Workplan Number D23 (iii). In Depth Country Study - New Zealand Asia-Pacific Forestry Sector Outlook Study Working Paper Series No: 5 3 TABLE OF CONTENTS INFORMATION NOTE ON ASIA-PACIFIC FORESTRY SECTOR OUTLOOK STUDY..................... i INTRODUCTION ....................................................................................................................1 CONTEXT ................................................................................................................................ 1 The New Zealand Economy and Economic Policy ......................................................................................... 1 Political Situation in New Zealand .................................................................................................................. 5 Social and Human Context for Forestry......................................................................................................... 6 THE NEW ZEALAND FOREST RESOURCE ....................................................................8
    [Show full text]
  • Southland Civil Defence Emergency Management Group Agenda.Docx
    Committee Members Mayor Tim Shadbolt, Invercargill City Council Cr Neville Cook, Environment Southland (Chair) Mayor Gary Tong, Southland District Council Mayor Tracy Hicks, Gore District Council or their alternates Southland Civil Defence Emergency Management Group (Te Manatu Arai Mate Ohorere o te Tonga) Council Chambers 10.00 am Environment Southland 8 November 2019 Cnr Price Street and North Road Invercargill A G E N D A (Rarangi Take) 1. Welcome (Haere mai) 2. Apologies (Nga Pa Pouri) 3. Declarations of Interest 4. Public Forum, Petitions and Deputations (He Huinga tuku korero) 5. Confirmation of Minutes (Whakau korero) – 15 March 2019 6. Notification of Extraordinary and Urgent Business (He Panui Autaia hei Totoia Pakihi) 6.1 Supplementary Reports 6.2 Other 7. Questions (Patai) 8. Chairman’s Report (Te Purongo a Tumuaki) 9. Report – 19/SCDEMG/93 Item 1 - Election of Chairperson and Deputy Chairperson .............................................11 Item 2 - Co-ordinating Executive Group (CEG) Chair Report ..........................................12 Item 3 - Health & Safety ..................................................................................................13 Item 4 – EMS Annual Report ...........................................................................................14 Item 5 – AF8 [Alpine Fault magnitude 8] ........................................................................27 Item 6 – EMS Update and Work Programme ..................................................................41 Item 7 – Transition
    [Show full text]
  • 2018: New Zealand's Equal-2Nd Warmest Year on Record
    New Zealand Climate Summary: 2018 Issued: 8 January 2019 2018: New Zealand’s equal-2nd warmest year on record Temperature Annual temperatures were above average (+0.51°C to +1.20°C above the annual average) across the majority of New Zealand, including much of the North Island as well as the western and southern South Island. A small strip of well above average (>1.20°C from average) temperatures were observed in southern Manawatu-Whanganui. Elsewhere, near average (within -0.50°C to +0.50°C of average) temperatures occurred in parts of southern Canterbury, Otago, small parts of Auckland and the Far North. 2018 was the equal 2nd-warmest year on record for New Zealand, based on NIWA’s seven- station series which began in 1909. Rainfall Yearly rainfall in 2018 was above normal (120-149% of the annual normal) across much of the eastern and upper South Island, as well as parts of Wellington, Wairarapa, Bay of Plenty, northern Waikato, and Auckland. Well above normal rainfall (>149% of normal) was observed in portions of southern Canterbury. Rainfall was near normal (80-119% of normal) for the remainder of New Zealand. Soil moisture 2018 began with below or well below normal soil moisture nearly nationwide, but soil moisture in the North Island and upper South Island gradually increased during January. Widespread heavy rainfall from ex-tropical cyclones Fehi and Gita during February resulted in well above normal soil moisture across most of New Zealand. Near to above normal soil moisture persisted through autumn, with near normal soil moisture widespread during the winter.
    [Show full text]
  • The Rural Vote and the Rise of the Labour Party, 1931-1935
    THE RURAL VOTE AND THE RISE OF THE LABOUR PARTY, 1931-1935. A thesis submitted in partial fulfilment of the requirements for the Degree of Doctor of Philosophy in History in the University of Canterbury by Stephen W. McLeod University of Canterbury 2005 Contents List of Figures .............................................................................................................................................. 4 List of Tables ................................................................................................................................................ 7 Abstract ...................................................................................................................................................... 10 Map of Urban Polling Areas Exceeding 10 Percent of the Electorate's Votes, 10 Rural (Dairying) Electorates in the North Island of New Zealand, 1935 ................................................................ 11 Part I: Backgroulld .................................................................................................................................... 12 Chapter 1: Introduction ............................................................................................................................... 12 Chapter 2: FIistoliography ........................................................................................................................... 19 Chapter 3: Methodology ............................................................................................................................
    [Show full text]
  • Drought in a Changing Climate
    Drought in a Changing Climate New Zealand’s future climate will be different What’s in store for farmers? to the one we have The most likely scenario sees farmers in most North Island regions, as well as those in eastern experienced so far. regions of the South Island – especially Canterbury and eastern Southland – spending 5-10 per cent Scientists expect wind more of the year in drought by the middle of this century. This means that if you spend an average of and rainfall patterns to 10 per cent of your time in drought at the moment, by 2040, you might expect to spend as much as 20 shift, bringing more rain per cent – although this figure will naturally vary from year to year. to western regions, with Between 2070 and 2090, that overall trend will intensify to the point where most of the country – with the east becoming drier. the likely exception of the West Coast of the South Island – will experience more time in drought. Even under very mild climate change, the Canterbury Plains will experience more frequent droughts. A 2011 study (see sidebar) highlighted the Less-likely scenarios implications for primary Drought scenarios for the period 2030 to 2050 range from small increases in the amount of time producers, many of spent in drought in eastern regions, through to a much more arid climate over most of the country. whom already have to Time spent in drought could double by the middle of the century, depending on the climate model deal with drought. and scenario considered.
    [Show full text]
  • Chapter 36D. South Pacific Ocean
    Chapter 36D. South Pacific Ocean Contributors: Karen Evans (lead author), Nic Bax (convener), Patricio Bernal (Lead member), Marilú Bouchon Corrales, Martin Cryer, Günter Försterra, Carlos F. Gaymer, Vreni Häussermann, and Jake Rice (Co-Lead member and Editor Part VI Biodiversity) 1. Introduction The Pacific Ocean is the Earth’s largest ocean, covering one-third of the world’s surface. This huge expanse of ocean supports the most extensive and diverse coral reefs in the world (Burke et al., 2011), the largest commercial fishery (FAO, 2014), the most and deepest oceanic trenches (General Bathymetric Chart of the Oceans, available at www.gebco.net), the largest upwelling system (Spalding et al., 2012), the healthiest and, in some cases, largest remaining populations of many globally rare and threatened species, including marine mammals, seabirds and marine reptiles (Tittensor et al., 2010). The South Pacific Ocean surrounds and is bordered by 23 countries and territories (for the purpose of this chapter, countries west of Papua New Guinea are not considered to be part of the South Pacific), which range in size from small atolls (e.g., Nauru) to continents (South America, Australia). Associated populations of each of the countries and territories range from less than 10,000 (Tokelau, Nauru, Tuvalu) to nearly 30.5 million (Peru; Population Estimates and Projections, World Bank Group, accessed at http://data.worldbank.org/data-catalog/population-projection-tables, August 2014). Most of the tropical and sub-tropical western and central South Pacific Ocean is contained within exclusive economic zones (EEZs), whereas vast expanses of temperate waters are associated with high seas areas (Figure 1).
    [Show full text]
  • Does Collaborative Governance Increase Public Confidence in Water Management? Survey Evidence from Aotearoa New Zealand
    www.water-alternatives.org Volume 13 | Issue 2 Tadaki, M.; Sinner, J.; Stahlmann-Brown, P. and Greenhalgh, S. 2020. Does collaborative governance increase public confidence in water management? Survey evidence from Aotearoa New Zealand. Water Alternatives 13(2): 302-323 Does Collaborative Governance Increase Public Confidence in Water Management? Survey Evidence from Aotearoa New Zealand Marc Tadaki Cawthron Institute, Nelson, New Zealand; [email protected] Jim Sinner Cawthron Institute, Nelson, New Zealand; [email protected] Philip Stahlmann-Brown Manaaki Whenua – Landcare Research, Wellington, New Zealand; [email protected] Suzie Greenhalgh Manaaki Whenua – Landcare Research, Auckland, New Zealand; [email protected] ABSTRACT: Collaborative decision-making is widely understood as a democratic corrective to top-down forms of environmental management; it is a way in which citizens can contribute local knowledge to the policy process and have a more direct role in shaping policies and rules that affect them and their environments. However, while the democratic virtues of collaborative governance are often asserted, they are rarely evidenced; this leaves claims of democratic empowerment open to question. This study used a longitudinal survey of three New Zealand regions (n = 1350) to identify whether major multi-year investments in collaborative decision-making (2012-2018) are leading to increased public confidence in the effectiveness, responsiveness and fairness of water management institutions. Residents in collaborative catchments were found to have scores that were statistically indistinguishable from residents of non-collaborative catchments on management effectiveness, perceived agreement about water management, and fairness. Collaborative catchment residents did assign higher scores for water management responsiveness than did other residents, but the size of this difference was small compared to the effects of gender, ethnicity, region and level of individuals’ prior engagement in water management.
    [Show full text]
  • New Zealand’S Sixth National Report to the United Nations Convention on Biological Diversity
    New Zealand’s Sixth National Report to the United Nations Convention on Biological Diversity Reporting period: 2014–2018 Cover: View of Palliser Bay, looking west from Mt Surf, Aorangi Mountains, southern North Island, New Zealand. Photo: Joe Hansen. This document may be cited as: Department of Conservation 2019: New Zealand’s Sixth National Report to the United Nations Convention on Biological Diversity. Reporting period: 2014–2018. Department of Conservation, Wellington, New Zealand. Available at: https://www.cbd.int/countries/?country=nz. and https://www.doc.govt.nz/about-us/international-agreements/convention-on-biological-diversity/ ISBN (electronic) 978-1-98-851491-8 ISBN (print) 978-1-98-851492-5 Department of Conservation PO Box 10420 Wellington 6143 New Zealand This work is licensed under the Creative Commons Attribution 4.0 International licence. In essence, you are free to copy, distribute and adapt the work, as long as you attribute the work to the Crown and abide by the other licence terms. To view a copy of this licence, visit creativecommons.org/licenses/by/4.0/. Table of Contents INTRODUCTION TO THE 6TH NATIONAL REPORT ........................................................................................................................ 5 1. PEOPLE’S LIVES ARE ENRICHED THROUGH CONNECTION TO NATURE ................................................................................ 7 I. General information .........................................................................................................................................................
    [Show full text]
  • The State of Knowledge of Deep-Sea Corals in the New Zealand Region Di Tracey1 and Freya Hjorvarsdottir2 (Eds, Comps) © 2019
    The state of knowledge of deep-sea corals in the New Zealand region Di Tracey1 and Freya Hjorvarsdottir2 (eds, comps) © 2019. All rights reserved. The copyright for this report, and for the data, maps, figures and other information (hereafter collectively referred to as “data”) contained in it, is held by NIWA is held by NIWA unless otherwise stated. This copyright extends to all forms of copying and any storage of material in any kind of information retrieval system. While NIWA uses all reasonable endeavours to ensure the accuracy of the data, NIWA does not guarantee or make any representation or warranty (express or implied) regarding the accuracy or completeness of the data, the use to which the data may be put or the results to be obtained from the use of the data. Accordingly, NIWA expressly disclaims all legal liability whatsoever arising from, or connected to, the use of, reference to, reliance on or possession of the data or the existence of errors therein. NIWA recommends that users exercise their own skill and care with respect to their use of the data and that they obtain independent professional advice relevant to their particular circumstances. NIWA SCIENCE AND TECHNOLOGY SERIES NUMBER 84 ISSN 1173-0382 Citation for full report: Tracey, D.M. & Hjorvarsdottir, F. (eds, comps) (2019). The State of Knowledge of Deep-Sea Corals in the New Zealand Region. NIWA Science and Technology Series Number 84. 140 p. Recommended citation for individual chapters (e.g., for Chapter 9.: Freeman, D., & Cryer, M. (2019). Current Management Measures and Threats, Chapter 9 In: Tracey, D.M.
    [Show full text]
  • Water Quality in New Zealand's Planted Forests: a Review
    Baillie and Neary New Zealand Journal of Forestry Science (2015) 45:7 DOI 10.1186/s40490-015-0040-0 REVIEW Open Access Water quality in New Zealand’s planted forests: a review Brenda R Baillie1* and Daniel G Neary2 Abstract This paper reviewed the key physical, chemical and biological water quality attributes of surface waters in New Zealand’s planted forests. The purpose was to: a) assess the changes in water quality throughout the planted forestry cycle from afforestation through to harvesting; b) compare water quality from planted forests with other land uses in New Zealand; and c) identify knowledge gaps and opportunities for future research. Afforestation of pasture land significantly improved a wide range of water quality attributes such as stream temperature, nutrient and sediment concentrations and microbial contamination within 4-6 years of planting. Water quality in mid-rotation to mature forests, a large proportion of the forestry cycle, was highly variable but characterised by cool water temperatures, low concentrations of sediment and nutrients, with aquatic invertebrate communities indicative of high water quality. Impacts of timber harvesting on water quality attributes were greatest when clear-cut harvesting up to the stream edge. Harvest impacts were mediated by the retention of intact riparian buffers and to a lesser extent by retention of moderate quantities of logging slash across small stream channels. Temporal and spatial factors influenced the magnitude of response to harvesting activities and duration of the recovery period. Land-use comparisons generally showed improving water quality from pasture to planted forest to indigenous forest. Continued research to identify management systems that mitigate impacts on water quality, particularly during harvesting, remains a priority.
    [Show full text]