Inconsequential effects of flooding in 2014 on lakes in the Peace‐Athabasca Delta (Canada) due to long‐term drying
Abstract Climate‐driven decline in freshwater supplied by rivers draining the hydrographic apex of western North America has ramifications for downstream ecosystems and society. For the Peace‐Athabasca Delta (PAD), floods from the Peace and Athabasca rivers are critical for sustaining abundant shall...
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Online Access: | http://dx.doi.org/10.1002/lno.10787 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Flno.10787 https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.10787 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/lno.10787 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.10787 |
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crwiley:10.1002/lno.10787 2024-06-23T07:53:05+00:00 Inconsequential effects of flooding in 2014 on lakes in the Peace‐Athabasca Delta (Canada) due to long‐term drying Remmer, Casey R. Klemt, Wynona H. Wolfe, Brent B. Hall, Roland I. Natural Sciences and Engineering Research Council of Canada BC Hydro Canadian Natural Resources Limited Alberta Environment and Parks Suncor Energy Incorporated 2018 http://dx.doi.org/10.1002/lno.10787 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Flno.10787 https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.10787 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/lno.10787 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.10787 en eng Wiley http://creativecommons.org/licenses/by/4.0/ Limnology and Oceanography volume 63, issue 4, page 1502-1518 ISSN 0024-3590 1939-5590 journal-article 2018 crwiley https://doi.org/10.1002/lno.10787 2024-06-11T04:41:42Z Abstract Climate‐driven decline in freshwater supplied by rivers draining the hydrographic apex of western North America has ramifications for downstream ecosystems and society. For the Peace‐Athabasca Delta (PAD), floods from the Peace and Athabasca rivers are critical for sustaining abundant shallow water habitat, but their frequency has been in decline for decades over much of its area. Here, we assess current hydrological and limnological status in the PAD by integrating spatial and temporal data. Analysis of water isotope compositions and water chemistry measured at numerous lakes across the delta shows that hydro‐limnological effects of the large‐scale ice‐jam flood event of 2014 failed to persist beyond the early ice‐free season of 2015. Isotope‐inferred paleohydrological records from five hydrologically representative lakes in the PAD indicate that periodic desiccation during the Little Ice Age occurred at the most elevated basin in response to locally arid climatic conditions, yet other lower elevation sites were influenced by high water level on Lake Athabasca owing to increased snowmelt‐ and glacier‐derived river discharge. In contrast, water isotope data during the past 15 yr at all five lakes consistently document the strong role of evaporation, a trend which began in the early to mid‐20 th century according to sediment records and is indicative of widespread aridity unprecedented during the past 400 yr. We suggest that integration of hydrological and limnological approaches over space and time is needed to inform assessment of contemporary lake conditions in large, complex floodplain landscapes. Article in Journal/Newspaper glacier* Lake Athabasca Wiley Online Library Canada Peace-Athabasca Delta ENVELOPE(-111.502,-111.502,58.667,58.667) Limnology and Oceanography 63 4 1502 1518 |
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Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
Abstract Climate‐driven decline in freshwater supplied by rivers draining the hydrographic apex of western North America has ramifications for downstream ecosystems and society. For the Peace‐Athabasca Delta (PAD), floods from the Peace and Athabasca rivers are critical for sustaining abundant shallow water habitat, but their frequency has been in decline for decades over much of its area. Here, we assess current hydrological and limnological status in the PAD by integrating spatial and temporal data. Analysis of water isotope compositions and water chemistry measured at numerous lakes across the delta shows that hydro‐limnological effects of the large‐scale ice‐jam flood event of 2014 failed to persist beyond the early ice‐free season of 2015. Isotope‐inferred paleohydrological records from five hydrologically representative lakes in the PAD indicate that periodic desiccation during the Little Ice Age occurred at the most elevated basin in response to locally arid climatic conditions, yet other lower elevation sites were influenced by high water level on Lake Athabasca owing to increased snowmelt‐ and glacier‐derived river discharge. In contrast, water isotope data during the past 15 yr at all five lakes consistently document the strong role of evaporation, a trend which began in the early to mid‐20 th century according to sediment records and is indicative of widespread aridity unprecedented during the past 400 yr. We suggest that integration of hydrological and limnological approaches over space and time is needed to inform assessment of contemporary lake conditions in large, complex floodplain landscapes. |
author2 |
Natural Sciences and Engineering Research Council of Canada BC Hydro Canadian Natural Resources Limited Alberta Environment and Parks Suncor Energy Incorporated |
format |
Article in Journal/Newspaper |
author |
Remmer, Casey R. Klemt, Wynona H. Wolfe, Brent B. Hall, Roland I. |
spellingShingle |
Remmer, Casey R. Klemt, Wynona H. Wolfe, Brent B. Hall, Roland I. Inconsequential effects of flooding in 2014 on lakes in the Peace‐Athabasca Delta (Canada) due to long‐term drying |
author_facet |
Remmer, Casey R. Klemt, Wynona H. Wolfe, Brent B. Hall, Roland I. |
author_sort |
Remmer, Casey R. |
title |
Inconsequential effects of flooding in 2014 on lakes in the Peace‐Athabasca Delta (Canada) due to long‐term drying |
title_short |
Inconsequential effects of flooding in 2014 on lakes in the Peace‐Athabasca Delta (Canada) due to long‐term drying |
title_full |
Inconsequential effects of flooding in 2014 on lakes in the Peace‐Athabasca Delta (Canada) due to long‐term drying |
title_fullStr |
Inconsequential effects of flooding in 2014 on lakes in the Peace‐Athabasca Delta (Canada) due to long‐term drying |
title_full_unstemmed |
Inconsequential effects of flooding in 2014 on lakes in the Peace‐Athabasca Delta (Canada) due to long‐term drying |
title_sort |
inconsequential effects of flooding in 2014 on lakes in the peace‐athabasca delta (canada) due to long‐term drying |
publisher |
Wiley |
publishDate |
2018 |
url |
http://dx.doi.org/10.1002/lno.10787 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Flno.10787 https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.10787 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/lno.10787 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.10787 |
long_lat |
ENVELOPE(-111.502,-111.502,58.667,58.667) |
geographic |
Canada Peace-Athabasca Delta |
geographic_facet |
Canada Peace-Athabasca Delta |
genre |
glacier* Lake Athabasca |
genre_facet |
glacier* Lake Athabasca |
op_source |
Limnology and Oceanography volume 63, issue 4, page 1502-1518 ISSN 0024-3590 1939-5590 |
op_rights |
http://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.1002/lno.10787 |
container_title |
Limnology and Oceanography |
container_volume |
63 |
container_issue |
4 |
container_start_page |
1502 |
op_container_end_page |
1518 |
_version_ |
1802644578156675072 |