Matches in SemOpenAlex for { <https://semopenalex.org/work/W3203095913> ?p ?o ?g. }
Showing items 1 to 99 of
99
with 100 items per page.
- W3203095913 endingPage "34" @default.
- W3203095913 startingPage "20" @default.
- W3203095913 abstract "Associations between temporal variability in 10 water quality variables and the El Niño–Southern Oscillation (ENSO) climate pattern, quantified by the Southern Oscillation Index (SOI), were assessed at 56 river sites in New Zealand over a 31-year period (1989–2019). Fluctuations in monthly observations of water quality at each site were correlated to varying degrees with the corresponding SOI value (ro). Trends for rolling windows of 5-, 10- and 15-year duration were evaluated for each site and variable using Kendall’s tau (τw) and for the SOI using linear regression (δSOIw). Aggregate trends for each variable, duration and time window were quantified as proportions of site trends that were increasing (Pw). Fluctuations in τw and Pw between time windows for all durations were explained by the corresponding SOI trend (δSOIw). Between-site and between-variable differences in the trend responses to the SOI trends were explained by the corresponding ro values and the median of the ro values (MF21087_IE1.gif) respectively. These results indicate that climate variability makes a significant contribution to water quality trends, even at timescales longer than ENSO cycles. Our models can be used to quantify this contribution for individual sites (i.e. τw) and for aggregate trends (i.e. Pw)." @default.
- W3203095913 created "2021-10-11" @default.
- W3203095913 creator A5007374801 @default.
- W3203095913 creator A5030094628 @default.
- W3203095913 creator A5061726347 @default.
- W3203095913 creator A5070752355 @default.
- W3203095913 date "2021-09-30" @default.
- W3203095913 modified "2023-10-17" @default.
- W3203095913 title "Effect of climate variability on water quality trends in New Zealand rivers" @default.
- W3203095913 cites W1204544352 @default.
- W3203095913 cites W1660213354 @default.
- W3203095913 cites W1886430567 @default.
- W3203095913 cites W1973717707 @default.
- W3203095913 cites W1976691478 @default.
- W3203095913 cites W1982729439 @default.
- W3203095913 cites W1984231257 @default.
- W3203095913 cites W2014485783 @default.
- W3203095913 cites W2016726538 @default.
- W3203095913 cites W2021236326 @default.
- W3203095913 cites W2022935286 @default.
- W3203095913 cites W2074108815 @default.
- W3203095913 cites W2080981104 @default.
- W3203095913 cites W2087292762 @default.
- W3203095913 cites W2108922337 @default.
- W3203095913 cites W2109374394 @default.
- W3203095913 cites W2110065044 @default.
- W3203095913 cites W2110613778 @default.
- W3203095913 cites W2137595065 @default.
- W3203095913 cites W2148420545 @default.
- W3203095913 cites W2163904950 @default.
- W3203095913 cites W2340935001 @default.
- W3203095913 cites W2415155232 @default.
- W3203095913 cites W2463816905 @default.
- W3203095913 cites W2498747851 @default.
- W3203095913 cites W2589861771 @default.
- W3203095913 cites W2604300224 @default.
- W3203095913 cites W2767392820 @default.
- W3203095913 cites W2783273745 @default.
- W3203095913 cites W2788464250 @default.
- W3203095913 cites W2803324490 @default.
- W3203095913 cites W2894594444 @default.
- W3203095913 cites W2900735416 @default.
- W3203095913 cites W2943517255 @default.
- W3203095913 cites W2974397324 @default.
- W3203095913 cites W3027408461 @default.
- W3203095913 cites W3204881300 @default.
- W3203095913 doi "https://doi.org/10.1071/mf21087" @default.
- W3203095913 hasPublicationYear "2021" @default.
- W3203095913 type Work @default.
- W3203095913 sameAs 3203095913 @default.
- W3203095913 citedByCount "5" @default.
- W3203095913 countsByYear W32030959132021 @default.
- W3203095913 countsByYear W32030959132022 @default.
- W3203095913 countsByYear W32030959132023 @default.
- W3203095913 crossrefType "journal-article" @default.
- W3203095913 hasAuthorship W3203095913A5007374801 @default.
- W3203095913 hasAuthorship W3203095913A5030094628 @default.
- W3203095913 hasAuthorship W3203095913A5061726347 @default.
- W3203095913 hasAuthorship W3203095913A5070752355 @default.
- W3203095913 hasBestOaLocation W32030959131 @default.
- W3203095913 hasConcept C105795698 @default.
- W3203095913 hasConcept C127142870 @default.
- W3203095913 hasConcept C127313418 @default.
- W3203095913 hasConcept C187320778 @default.
- W3203095913 hasConcept C33923547 @default.
- W3203095913 hasConcept C39432304 @default.
- W3203095913 hasConcept C49204034 @default.
- W3203095913 hasConcept C507956050 @default.
- W3203095913 hasConcept C76886044 @default.
- W3203095913 hasConceptScore W3203095913C105795698 @default.
- W3203095913 hasConceptScore W3203095913C127142870 @default.
- W3203095913 hasConceptScore W3203095913C127313418 @default.
- W3203095913 hasConceptScore W3203095913C187320778 @default.
- W3203095913 hasConceptScore W3203095913C33923547 @default.
- W3203095913 hasConceptScore W3203095913C39432304 @default.
- W3203095913 hasConceptScore W3203095913C49204034 @default.
- W3203095913 hasConceptScore W3203095913C507956050 @default.
- W3203095913 hasConceptScore W3203095913C76886044 @default.
- W3203095913 hasIssue "1" @default.
- W3203095913 hasLocation W32030959131 @default.
- W3203095913 hasOpenAccess W3203095913 @default.
- W3203095913 hasPrimaryLocation W32030959131 @default.
- W3203095913 hasRelatedWork W1967150532 @default.
- W3203095913 hasRelatedWork W1991420611 @default.
- W3203095913 hasRelatedWork W2003357297 @default.
- W3203095913 hasRelatedWork W2296297430 @default.
- W3203095913 hasRelatedWork W2387731412 @default.
- W3203095913 hasRelatedWork W2388296530 @default.
- W3203095913 hasRelatedWork W2911516818 @default.
- W3203095913 hasRelatedWork W3043802276 @default.
- W3203095913 hasRelatedWork W3145266005 @default.
- W3203095913 hasRelatedWork W4280504281 @default.
- W3203095913 hasVolume "73" @default.
- W3203095913 isParatext "false" @default.
- W3203095913 isRetracted "false" @default.
- W3203095913 magId "3203095913" @default.
- W3203095913 workType "article" @default.
%20climate%20pattern%2C%20quantified%20by%20the%20Southern%20Oscillation%20Index%20(SOI)%2C%20were%20assessed%20at%2056%20river%20sites%20in%20New%20Zealand%20over%20a%2031-year%20period%20(1989%E2%80%932019).%20Fluctuations%20in%20monthly%20observations%20of%20water%20quality%20at%20each%20site%20were%20correlated%20to%20varying%20degrees%20with%20the%20corresponding%20SOI%20value%20(ro).%20Trends%20for%20rolling%20windows%20of%205-%2C%2010-%20and%2015-year%20duration%20were%20evaluated%20for%20each%20site%20and%20variable%20using%20Kendall%E2%80%99s%20tau%20(%CF%84w)%20and%20for%20the%20SOI%20using%20linear%20regression%20(%CE%B4SOIw).%20Aggregate%20trends%20for%20each%20variable%2C%20duration%20and%20time%20window%20were%20quantified%20as%20proportions%20of%20site%20trends%20that%20were%20increasing%20(Pw).%20Fluctuations%20in%20%CF%84w%20and%20Pw%20between%20time%20windows%20for%20all%20durations%20were%20explained%20by%20the%20corresponding%20SOI%20trend%20(%CE%B4SOIw).%20Between-site%20and%20between-variable%20differences%20in%20the%20trend%20responses%20to%20the%20SOI%20trends%20were%20explained%20by%20the%20corresponding%20ro%20values%20and%20the%20median%20of%20the%20ro%20values%20(MF21087_IE1.gif)%20respectively.%20These%20results%20indicate%20that%20climate%20variability%20makes%20a%20significant%20contribution%20to%20water%20quality%20trends%2C%20even%20at%20timescales%20longer%20than%20ENSO%20cycles.%20Our%20models%20can%20be%20used%20to%20quantify%20this%20contribution%20for%20individual%20sites%20(i.e.%20%CF%84w)%20and%20for%20aggregate%20trends%20(i.e.%20Pw).%22){kind=link}