Seasonal overturn and stratification changes drive deep-water warming in one of Earth’s largest lakes

This study presents hourly data from a thermistor string in Lake Michigan, inspecting its response at depth to surface warming. Based on the data, the study suggests bottom lake temperatures respond to changes in turnover and re-stratification, with the ultimate possibility of the lake shifting from...

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Autores principales:	Eric J. Anderson, Craig A. Stow, Andrew D. Gronewold, Lacey A. Mason, Michael J. McCormick, Song S. Qian, Steven A. Ruberg, Kyle Beadle, Stephen A. Constant, Nathan Hawley
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/963661d850174036943b00ef5c19d6ca
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spelling	oai:doaj.org-article:963661d850174036943b00ef5c19d6ca2021-12-02T11:39:18ZSeasonal overturn and stratification changes drive deep-water warming in one of Earth’s largest lakes10.1038/s41467-021-21971-12041-1723https://doaj.org/article/963661d850174036943b00ef5c19d6ca2021-03-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-21971-1https://doaj.org/toc/2041-1723This study presents hourly data from a thermistor string in Lake Michigan, inspecting its response at depth to surface warming. Based on the data, the study suggests bottom lake temperatures respond to changes in turnover and re-stratification, with the ultimate possibility of the lake shifting from dimictic to monomictic.Eric J. AndersonCraig A. StowAndrew D. GronewoldLacey A. MasonMichael J. McCormickSong S. QianSteven A. RubergKyle BeadleStephen A. ConstantNathan HawleyNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-9 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Eric J. Anderson Craig A. Stow Andrew D. Gronewold Lacey A. Mason Michael J. McCormick Song S. Qian Steven A. Ruberg Kyle Beadle Stephen A. Constant Nathan Hawley Seasonal overturn and stratification changes drive deep-water warming in one of Earth’s largest lakes
description	This study presents hourly data from a thermistor string in Lake Michigan, inspecting its response at depth to surface warming. Based on the data, the study suggests bottom lake temperatures respond to changes in turnover and re-stratification, with the ultimate possibility of the lake shifting from dimictic to monomictic.
format	article
author	Eric J. Anderson Craig A. Stow Andrew D. Gronewold Lacey A. Mason Michael J. McCormick Song S. Qian Steven A. Ruberg Kyle Beadle Stephen A. Constant Nathan Hawley
author_facet	Eric J. Anderson Craig A. Stow Andrew D. Gronewold Lacey A. Mason Michael J. McCormick Song S. Qian Steven A. Ruberg Kyle Beadle Stephen A. Constant Nathan Hawley
author_sort	Eric J. Anderson
title	Seasonal overturn and stratification changes drive deep-water warming in one of Earth’s largest lakes
title_short	Seasonal overturn and stratification changes drive deep-water warming in one of Earth’s largest lakes
title_full	Seasonal overturn and stratification changes drive deep-water warming in one of Earth’s largest lakes
title_fullStr	Seasonal overturn and stratification changes drive deep-water warming in one of Earth’s largest lakes
title_full_unstemmed	Seasonal overturn and stratification changes drive deep-water warming in one of Earth’s largest lakes
title_sort	seasonal overturn and stratification changes drive deep-water warming in one of earth’s largest lakes
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/963661d850174036943b00ef5c19d6ca
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Seasonal overturn and stratification changes drive deep-water warming in one of Earth’s largest lakes

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