Annual water residence time effects on thermal structure: A potential lake restoration measure?

dc.contributor.authorOlsson, Freyaen
dc.contributor.authorMackay, Eleanor B.en
dc.contributor.authorMoore, Tadhg N.en
dc.contributor.authorBarker, Philen
dc.contributor.authorDavies, Sianen
dc.contributor.authorHall, Ruthen
dc.contributor.authorSpears, Bryanen
dc.contributor.authorWilkinson, Jayneen
dc.contributor.authorJones, Ian D.en
dc.date.accessioned2022-06-07T19:16:31Zen
dc.date.available2022-06-07T19:16:31Zen
dc.date.issued2022-07-15en
dc.description.abstractInnovative methods to combat internal loading issues in eutrophic lakes are urgently needed to speed recovery and restore systems within legislative deadlines. In stratifying lakes, internal phosphorus loading is particularly problematic during the summer stratified period when anoxia persists in the hypolimnion, promoting phos-phorus release from the sediment. A novel method to inhibit stratification by reducing residence times is pro-posed as a way of controlling the length of the hypolimnetic anoxic period, thus reducing the loading of nutrients from the sediments into the water column. However, residence time effects on stratification length in natural lakes are not well understood. We used a systematic modelling approach to investigate the viability of changes to annual water residence time in affecting lake stratification and thermal dynamics in Elterwater, a small strati-fying eutrophic lake in the northwest of England. We found that reducing annual water residence times shortened and weakened summer stratification. Based on finer-scale dynamics of lake heat fluxes and water column sta-bility we propose seasonal or sub-seasonal management of water residence time is needed for the method to be most effective at reducing stratification as a means of controlling internal nutrient loading.en
dc.description.notesThe authors wish to thank the South Cumbria Rivers Trust for their help with data collection and for providing data and information on the Elterwater intervention, and the Environment Agency for providing river flow data. This work was funded by a PhD studentship awarded to FO from the UK Natural Environment Research Council through the Envision Doctoral Training Partnership (grant ref. NE/L002604/1) .en
dc.description.sponsorshipUK Natural Environment Research Council through through the Envision Doctoral Training Partnership [NE/L002604/1]en
dc.description.versionPublished versionen
dc.format.mimetypeapplication/pdfen
dc.identifier.doihttps://doi.org/10.1016/j.jenvman.2022.115082en
dc.identifier.eissn1095-8630en
dc.identifier.issn0301-4797en
dc.identifier.other115082en
dc.identifier.pmid35468434en
dc.identifier.urihttp://hdl.handle.net/10919/110452en
dc.identifier.volume314en
dc.language.isoenen
dc.publisherAcademic Press - Elsevieren
dc.rightsCreative Commons Attribution 4.0 Internationalen
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en
dc.subjectLake managementsen
dc.subjectHeat fluxesen
dc.subjectHypolimnetic anoxiaen
dc.subjectGeneral Ocean turbulence modelen
dc.subjectFlushingen
dc.titleAnnual water residence time effects on thermal structure: A potential lake restoration measure?en
dc.title.serialJournal of Environmental Managementen
dc.typeArticle - Refereeden
dc.type.dcmitypeTexten

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