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dc.contributor.authorTempero, Grant Wayneen_NZ
dc.contributor.authorPaul, Wendy J.en_NZ
dc.date.accessioned2015-11-10T20:11:20Z
dc.date.available2015en_NZ
dc.date.available2015-11-10T20:11:20Z
dc.date.issued2015en_NZ
dc.identifier.citationTempero, G. W., & Paul, W. J. (2015). Destratification – fact sheet. Hamilton, New Zealand: Lake Ecosystem Restoration New Zealand (LERNZ), University of Waikato.en
dc.identifier.urihttps://hdl.handle.net/10289/9723
dc.description.abstractDuring summer, the surface waters of lakes warm and become less dense than the colder bottom waters. This process is known as stratification and prevents surface and bottom water mixing. Stratification can occur intermittently in shallower lakes or for up to 9 months in deeper lakes (Figure 1). Under natural conditions stratification normally breaks down during the winter months when surface temperatures equilibrate with the bottom of the lake.
dc.format.mimetypeapplication/pdf
dc.language.isoen
dc.publisherLake Ecosystem Restoration New Zealand (LERNZ), University of Waikatoen_NZ
dc.relation.urihttps://www.lernz.co.nz/tools-and-resources/fact-sheetsen_NZ
dc.titleDestratification – fact sheeten_NZ
dc.typeOther
pubs.confidentialfalseen_NZ
pubs.elements-id133096
pubs.notesAuthor information located in pdf properties, ie. open pdf, click file and click properties to viewen_NZ
pubs.organisational-group/Waikato
pubs.organisational-group/Waikato/FSEN
pubs.organisational-group/Waikato/FSEN/School of Science
pubs.place-of-publicationHamilton, New Zealanden_NZ


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