Hydroecological responses of the Athabasca Delta, Canada, to changes in river flow and climate during the 20th century

• Published in: Ecohydrology
• Main Authors: Wolfe, Brent B., Hall, Roland I., Edwards, Thomas W. D., Vardy, Sheila R., Falcone, Matthew D., Sjunneskog, Charlotte, Sylvestre, Florence, Mcgowan, Suzanne, Leavitt, Peter R., Driel, Peter, Van
• Other Authors: Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE), Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2008
• Subjects: [SDU.STU]Sciences of the Universe [physics]/Earth Sciences; Athabasca River; Canada; Embarras; Embarras River
• Online Access: https://hal.science/hal-01795358; https://doi.org/10.1002/eco.13

International audience We employ water-isotope tracers and multi-proxy paleolimnological records to characterize contemporary controls onwater balances of floodplain lakes in the Athabasca Delta. Canada, within the context of its hydroecological evolution over the 20th century. The insight gained from these approaches is necessary to gauge the hydroecological resiliency of the Athabasca Delta to past and future changes in Athabasca River flow regime. Results obtained from three lakes located in different regions of the Athabasca Delta indicate that hydroecological conditions were strongly affected by an engineered meander cut-off on the Athabasca River in 1972 intended to maintain flow in the river main stem, and a natural bifurcation of one of the major distributaries (Embarras River) in 1982 in response to progressive overextension of the delta to the east. Climate warming and naturally declining river discharge have also contributed to directional change. Recent drying trends reconstructed from sediment cores at two of the three lakes are likely representative of rapidly evolving hydroecological conditions in the south-eastern sector based on mappoing of a recent high-magnitude ice-jam flood that failed to recharge this portion of the delta, while wetting in the region of the third lake due to increased frequency of river flooding reflects increasing of the magnitude and timing of discharge in the Athabasca River and heighten the need for informed management strategies to safeguard the integrity of this unique wetland ecosystem. Copyright (C) 2008 John Wiley & Sons, Ltd.