Worldwide lake level trends and responses to background climate variation

Lakes provide many important benefits to society, including drinking water, flood attenuation, nutrition, and recreation. Anthropogenic environmental changes may affect these benefits by altering lake water levels. However, background climate oscillations such as the El Niño–Southern Oscillation and...

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Published in:Hydrology and Earth System Sciences
Main Authors: Kraemer, Benjamin M., Seimon, Anton, Adrian, Rita, McIntyre, Peter B.
Format: Text
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/hess-24-2593-2020
https://www.hydrol-earth-syst-sci.net/24/2593/2020/
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spelling ftcopernicus:oai:publications.copernicus.org:hess80014 2023-05-15T17:34:56+02:00 Worldwide lake level trends and responses to background climate variation Kraemer, Benjamin M. Seimon, Anton Adrian, Rita McIntyre, Peter B. 2020-05-18 application/pdf https://doi.org/10.5194/hess-24-2593-2020 https://www.hydrol-earth-syst-sci.net/24/2593/2020/ eng eng doi:10.5194/hess-24-2593-2020 https://www.hydrol-earth-syst-sci.net/24/2593/2020/ eISSN: 1607-7938 Text 2020 ftcopernicus https://doi.org/10.5194/hess-24-2593-2020 2020-05-25T16:22:00Z Lakes provide many important benefits to society, including drinking water, flood attenuation, nutrition, and recreation. Anthropogenic environmental changes may affect these benefits by altering lake water levels. However, background climate oscillations such as the El Niño–Southern Oscillation and the North Atlantic Oscillation can obscure long-term trends in water levels, creating uncertainty over the strength and ubiquity of anthropogenic effects on lakes. Here we account for the effects of background climate variation and test for long-term (1992–2019) trends in water levels in 200 globally distributed large lakes using satellite altimetry data. The median percentage of water level variation associated with background climate variation was 58 %, with an additional 10 % explained by seasonal variation and 25 % by the long-term trend. The relative influence of specific axes of background climate variation on water levels varied substantially across and within regions. After removing the effects of background climate variation on water levels, long-term water level trend estimates were lower (median: +0.8 cm yr −1 ) than calculated from raw water level data (median: + 1.2 cm yr −1 ). However, the trends became more statistically significant in 86 % of lakes after removing the effects of background climate variation (the median p value of trends changed from 0.16 to 0.02). Thus, robust tests for long-term trends in lake water levels which may or may not be anthropogenic will require prior isolation and removal of the effects of background climate variation. Our findings suggest that background climate variation often masks long-term trends in environmental variables but can be accounted for through more comprehensive statistical analyses. Text North Atlantic North Atlantic oscillation Copernicus Publications: E-Journals Hydrology and Earth System Sciences 24 5 2593 2608
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collection Copernicus Publications: E-Journals
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language English
description Lakes provide many important benefits to society, including drinking water, flood attenuation, nutrition, and recreation. Anthropogenic environmental changes may affect these benefits by altering lake water levels. However, background climate oscillations such as the El Niño–Southern Oscillation and the North Atlantic Oscillation can obscure long-term trends in water levels, creating uncertainty over the strength and ubiquity of anthropogenic effects on lakes. Here we account for the effects of background climate variation and test for long-term (1992–2019) trends in water levels in 200 globally distributed large lakes using satellite altimetry data. The median percentage of water level variation associated with background climate variation was 58 %, with an additional 10 % explained by seasonal variation and 25 % by the long-term trend. The relative influence of specific axes of background climate variation on water levels varied substantially across and within regions. After removing the effects of background climate variation on water levels, long-term water level trend estimates were lower (median: +0.8 cm yr −1 ) than calculated from raw water level data (median: + 1.2 cm yr −1 ). However, the trends became more statistically significant in 86 % of lakes after removing the effects of background climate variation (the median p value of trends changed from 0.16 to 0.02). Thus, robust tests for long-term trends in lake water levels which may or may not be anthropogenic will require prior isolation and removal of the effects of background climate variation. Our findings suggest that background climate variation often masks long-term trends in environmental variables but can be accounted for through more comprehensive statistical analyses.
format Text
author Kraemer, Benjamin M.
Seimon, Anton
Adrian, Rita
McIntyre, Peter B.
spellingShingle Kraemer, Benjamin M.
Seimon, Anton
Adrian, Rita
McIntyre, Peter B.
Worldwide lake level trends and responses to background climate variation
author_facet Kraemer, Benjamin M.
Seimon, Anton
Adrian, Rita
McIntyre, Peter B.
author_sort Kraemer, Benjamin M.
title Worldwide lake level trends and responses to background climate variation
title_short Worldwide lake level trends and responses to background climate variation
title_full Worldwide lake level trends and responses to background climate variation
title_fullStr Worldwide lake level trends and responses to background climate variation
title_full_unstemmed Worldwide lake level trends and responses to background climate variation
title_sort worldwide lake level trends and responses to background climate variation
publishDate 2020
url https://doi.org/10.5194/hess-24-2593-2020
https://www.hydrol-earth-syst-sci.net/24/2593/2020/
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source eISSN: 1607-7938
op_relation doi:10.5194/hess-24-2593-2020
https://www.hydrol-earth-syst-sci.net/24/2593/2020/
op_doi https://doi.org/10.5194/hess-24-2593-2020
container_title Hydrology and Earth System Sciences
container_volume 24
container_issue 5
container_start_page 2593
op_container_end_page 2608
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