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An Application of the T‐TEL Assessment Method to Evaluate Connectivity in a Lake‐Dominated Watershed after Drought
Lakes are landscape features that influence connectivity of mass and energy by being foci for the reception, mixing, and provision of water and material. Where lake fractions are high, they influence hydrological connectivity. This behavior was exemplified in the Baker Creek watershed in Canada'...
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Published in: | Journal of the American Water Resources Association 2019-04, Vol.55 (2), p.318-333 |
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creator | Spence, C. Ali, G. Oswald, C.J. Wellen, C. |
description | Lakes are landscape features that influence connectivity of mass and energy by being foci for the reception, mixing, and provision of water and material. Where lake fractions are high, they influence hydrological connectivity. This behavior was exemplified in the Baker Creek watershed in Canada's Northwest Territories during a two‐year drought in which many lake levels declined below outlet elevations. This study evaluated how lakes controlled surface runoff connectivity reestablishment following the drought using a new assessment method, T‐TEL (time scales — thresholds, excesses, losses). Analysis of daily data showed that during a summer period following the drought, connectivity occurred between 0% and 41% of the time. The size of run‐of‐the‐river lakes relative to their upstream watershed area, and the upstream lake fraction, are two factors for connectivity. These terms represent a lake's ability to control the size of storage deficits relative to rainfall, and evaporation and storage losses along pathways. The connectivity magnitude–duration curve only aligned with the watershed flow duration curve during high‐water conditions, implying lakes functioned as individuals rather than as part of a perennial watercourse during much of the study. The T‐TEL method can be used to quantify consistent metrics of hydrologic connectivity that can be used for regionalization exercises and understanding hydrologic controls on material transport.
Research Impact Statement: This research demonstrated the T‐TEL method can be used successfully to quantify hydrological connectivity in a lake‐dominated watershed. |
doi_str_mv | 10.1111/1752-1688.12702 |
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Research Impact Statement: This research demonstrated the T‐TEL method can be used successfully to quantify hydrological connectivity in a lake‐dominated watershed.</description><identifier>ISSN: 1093-474X</identifier><identifier>EISSN: 1752-1688</identifier><identifier>DOI: 10.1111/1752-1688.12702</identifier><language>eng</language><publisher>Middleburg: Blackwell Publishing Ltd</publisher><subject>Coastal inlets ; connectivity ; Data processing ; Drought ; Duration ; Evaporation ; Flow duration ; Flow duration curves ; Hydrology ; Lakes ; Methods ; Outlets ; Rain ; Rainfall ; Rivers ; Runoff ; Stability ; Surface runoff ; surface water hydrology ; Upstream ; Watersheds</subject><ispartof>Journal of the American Water Resources Association, 2019-04, Vol.55 (2), p.318-333</ispartof><rights>2018 American Water Resources Association and Her Majesty the Queen in Right of Canada. Reproduced with the permission of the Minister of Environment and Climate Change Canada. Journal of the American Water Resources Association © 2018 American Water Resources Association</rights><rights>2019 American Water Resources Association</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3162-6c1d9ed80567cbe65422086f82997136ad4a040fdfd35ac9906281efd8a62f2e3</citedby><cites>FETCH-LOGICAL-c3162-6c1d9ed80567cbe65422086f82997136ad4a040fdfd35ac9906281efd8a62f2e3</cites><orcidid>0000-0003-1059-2217</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Spence, C.</creatorcontrib><creatorcontrib>Ali, G.</creatorcontrib><creatorcontrib>Oswald, C.J.</creatorcontrib><creatorcontrib>Wellen, C.</creatorcontrib><title>An Application of the T‐TEL Assessment Method to Evaluate Connectivity in a Lake‐Dominated Watershed after Drought</title><title>Journal of the American Water Resources Association</title><description>Lakes are landscape features that influence connectivity of mass and energy by being foci for the reception, mixing, and provision of water and material. Where lake fractions are high, they influence hydrological connectivity. This behavior was exemplified in the Baker Creek watershed in Canada's Northwest Territories during a two‐year drought in which many lake levels declined below outlet elevations. This study evaluated how lakes controlled surface runoff connectivity reestablishment following the drought using a new assessment method, T‐TEL (time scales — thresholds, excesses, losses). Analysis of daily data showed that during a summer period following the drought, connectivity occurred between 0% and 41% of the time. The size of run‐of‐the‐river lakes relative to their upstream watershed area, and the upstream lake fraction, are two factors for connectivity. These terms represent a lake's ability to control the size of storage deficits relative to rainfall, and evaporation and storage losses along pathways. The connectivity magnitude–duration curve only aligned with the watershed flow duration curve during high‐water conditions, implying lakes functioned as individuals rather than as part of a perennial watercourse during much of the study. The T‐TEL method can be used to quantify consistent metrics of hydrologic connectivity that can be used for regionalization exercises and understanding hydrologic controls on material transport.
Research Impact Statement: This research demonstrated the T‐TEL method can be used successfully to quantify hydrological connectivity in a lake‐dominated watershed.</description><subject>Coastal inlets</subject><subject>connectivity</subject><subject>Data processing</subject><subject>Drought</subject><subject>Duration</subject><subject>Evaporation</subject><subject>Flow duration</subject><subject>Flow duration curves</subject><subject>Hydrology</subject><subject>Lakes</subject><subject>Methods</subject><subject>Outlets</subject><subject>Rain</subject><subject>Rainfall</subject><subject>Rivers</subject><subject>Runoff</subject><subject>Stability</subject><subject>Surface runoff</subject><subject>surface water hydrology</subject><subject>Upstream</subject><subject>Watersheds</subject><issn>1093-474X</issn><issn>1752-1688</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNqFkMtOwzAQRSMEEqWwZmuJdVo_EidZRm15KQgJFZWdZWKbuKRxiJ2i7vgEvpEvwSWILbOYuRqdOyPdIDhHcIJ8TVES4xDRNJ0gnEB8EIz-Nodew4yEURI9HQcn1q4hRDFKySjY5g3I27bWJXfaNMAo4CoJll8fn8tFAXJrpbUb2ThwJ11lBHAGLLa87rmTYGaaRpZOb7XbAd0ADgr-Kr11bja68YQAK987W3nFlVdg3pn-pXKnwZHitZVnv3McPF4ulrPrsLi_upnlRVgSRHFISyQyKVIY06R8ljSOMIYpVSnOsgQRykXEYQSVUILEvMwySHGKpBIpp1hhScbBxXC37cxbL61ja9N3jX_J_CWCohhlxFPTgSo7Y20nFWs7veHdjiHI9uGyfZRsHyX7Cdc76OB417Xc_Yez23z1MBi_AU6kfZc</recordid><startdate>201904</startdate><enddate>201904</enddate><creator>Spence, C.</creator><creator>Ali, G.</creator><creator>Oswald, C.J.</creator><creator>Wellen, C.</creator><general>Blackwell Publishing Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7ST</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H97</scope><scope>KR7</scope><scope>L.G</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0003-1059-2217</orcidid></search><sort><creationdate>201904</creationdate><title>An Application of the T‐TEL Assessment Method to Evaluate Connectivity in a Lake‐Dominated Watershed after Drought</title><author>Spence, C. ; Ali, G. ; Oswald, C.J. ; Wellen, C.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3162-6c1d9ed80567cbe65422086f82997136ad4a040fdfd35ac9906281efd8a62f2e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Coastal inlets</topic><topic>connectivity</topic><topic>Data processing</topic><topic>Drought</topic><topic>Duration</topic><topic>Evaporation</topic><topic>Flow duration</topic><topic>Flow duration curves</topic><topic>Hydrology</topic><topic>Lakes</topic><topic>Methods</topic><topic>Outlets</topic><topic>Rain</topic><topic>Rainfall</topic><topic>Rivers</topic><topic>Runoff</topic><topic>Stability</topic><topic>Surface runoff</topic><topic>surface water hydrology</topic><topic>Upstream</topic><topic>Watersheds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Spence, C.</creatorcontrib><creatorcontrib>Ali, G.</creatorcontrib><creatorcontrib>Oswald, C.J.</creatorcontrib><creatorcontrib>Wellen, C.</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Journal of the American Water Resources Association</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Spence, C.</au><au>Ali, G.</au><au>Oswald, C.J.</au><au>Wellen, C.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>An Application of the T‐TEL Assessment Method to Evaluate Connectivity in a Lake‐Dominated Watershed after Drought</atitle><jtitle>Journal of the American Water Resources Association</jtitle><date>2019-04</date><risdate>2019</risdate><volume>55</volume><issue>2</issue><spage>318</spage><epage>333</epage><pages>318-333</pages><issn>1093-474X</issn><eissn>1752-1688</eissn><abstract>Lakes are landscape features that influence connectivity of mass and energy by being foci for the reception, mixing, and provision of water and material. Where lake fractions are high, they influence hydrological connectivity. This behavior was exemplified in the Baker Creek watershed in Canada's Northwest Territories during a two‐year drought in which many lake levels declined below outlet elevations. This study evaluated how lakes controlled surface runoff connectivity reestablishment following the drought using a new assessment method, T‐TEL (time scales — thresholds, excesses, losses). Analysis of daily data showed that during a summer period following the drought, connectivity occurred between 0% and 41% of the time. The size of run‐of‐the‐river lakes relative to their upstream watershed area, and the upstream lake fraction, are two factors for connectivity. These terms represent a lake's ability to control the size of storage deficits relative to rainfall, and evaporation and storage losses along pathways. The connectivity magnitude–duration curve only aligned with the watershed flow duration curve during high‐water conditions, implying lakes functioned as individuals rather than as part of a perennial watercourse during much of the study. The T‐TEL method can be used to quantify consistent metrics of hydrologic connectivity that can be used for regionalization exercises and understanding hydrologic controls on material transport.
Research Impact Statement: This research demonstrated the T‐TEL method can be used successfully to quantify hydrological connectivity in a lake‐dominated watershed.</abstract><cop>Middleburg</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1111/1752-1688.12702</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0003-1059-2217</orcidid></addata></record> |
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subjects | Coastal inlets connectivity Data processing Drought Duration Evaporation Flow duration Flow duration curves Hydrology Lakes Methods Outlets Rain Rainfall Rivers Runoff Stability Surface runoff surface water hydrology Upstream Watersheds |
title | An Application of the T‐TEL Assessment Method to Evaluate Connectivity in a Lake‐Dominated Watershed after Drought |
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