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Peace-Athabasca Delta water surface elevations and slopes mapped from AirSWOT Ka-band InSAR
In late 2023 the Surface Water and Ocean Topography (SWOT) satellite mission will release unprecedented high-resolution measurements of water surface elevation (WSE) and water surface slope (WSS) globally. SWOT's exciting Ka-band near-nadir wide-swath interferometric radar (InSAR) technology co...
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Published in: | Remote sensing letters 2023-12, Vol.14 (12), p.1238-1250 |
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container_title | Remote sensing letters |
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creator | Smith, Laurence C. Fayne, Jessica V. Wang, Bo Kyzivat, Ethan D. Gleason, Colin J. Harlan, Merritt E. Langhorst, Theodore Feng, Dongmei Pavelsky, Tamlin M. Peters, Daniel L. |
description | In late
2023 the Surface Water and Ocean Topography (SWOT) satellite mission will release
unprecedented high-resolution measurements of water surface elevation (WSE) and
water surface slope (WSS) globally. SWOT's exciting Ka-band near-nadir
wide-swath interferometric radar (InSAR) technology could transform studies of surface
water hydrology, but remains highly experimental. We examine Airborne SWOT
(AirSWOT) data acquired twice over Canada's Peace-Athabasca Delta (PAD), a
large, low-gradient, ecologically important riverine wetland complex. While
noisy and susceptible to "dark water" (low-return) data losses, spatially
averaged AirSWOT WSE observations reveal a broad-scale water-level decline of ~44
cmn (σ =271 cm) between 9 July and 13 August 2017, similar to a ~56 cm decline (σ=33 cm) recorded by four in situ gauging stations.
River flow directions and WSS are correctly inferred following filtering and
reach-averaging of AirSWOT data, but ~10 km reaches are essential to retrieve them.
July AirSWOT observations suggest steeper WSS down an alternate flow course
(Embarras River-Mamawi Creek distributary) of the Athabasca River, consistent
with field surveys conducted the following year. This signifies potential for
the Athabasca River to avulse northward into Mamawi Lake, with transformative
impacts on flooding, sedimentation, ecology, and human activities in the PAD.
Although AirSWOT differs from SWOT, we conclude SWOT Ka-band InSAR observations
may detect water level changes and avulsion potentials in other low-gradient
deltas globally. |
doi_str_mv | 10.1080/2150704X.2023.2280464 |
format | article |
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2023 the Surface Water and Ocean Topography (SWOT) satellite mission will release
unprecedented high-resolution measurements of water surface elevation (WSE) and
water surface slope (WSS) globally. SWOT's exciting Ka-band near-nadir
wide-swath interferometric radar (InSAR) technology could transform studies of surface
water hydrology, but remains highly experimental. We examine Airborne SWOT
(AirSWOT) data acquired twice over Canada's Peace-Athabasca Delta (PAD), a
large, low-gradient, ecologically important riverine wetland complex. While
noisy and susceptible to "dark water" (low-return) data losses, spatially
averaged AirSWOT WSE observations reveal a broad-scale water-level decline of ~44
cmn (σ =271 cm) between 9 July and 13 August 2017, similar to a ~56 cm decline (σ=33 cm) recorded by four in situ gauging stations.
River flow directions and WSS are correctly inferred following filtering and
reach-averaging of AirSWOT data, but ~10 km reaches are essential to retrieve them.
July AirSWOT observations suggest steeper WSS down an alternate flow course
(Embarras River-Mamawi Creek distributary) of the Athabasca River, consistent
with field surveys conducted the following year. This signifies potential for
the Athabasca River to avulse northward into Mamawi Lake, with transformative
impacts on flooding, sedimentation, ecology, and human activities in the PAD.
Although AirSWOT differs from SWOT, we conclude SWOT Ka-band InSAR observations
may detect water level changes and avulsion potentials in other low-gradient
deltas globally.</description><identifier>ISSN: 2150-704X</identifier><identifier>EISSN: 2150-7058</identifier><identifier>DOI: 10.1080/2150704X.2023.2280464</identifier><language>eng</language><publisher>Abingdon: Taylor & Francis</publisher><subject>AirSWOT ; Avulsion ; Coastal inlets ; Data acquisition ; Data loss ; Discharge measurement ; Extremely high frequencies ; Gaging stations ; Hydrology ; Interferometric synthetic aperture radar ; Lakes ; Radar ; radar remote sensing ; river avulsion ; River flow ; Rivers ; Stream discharge ; Surface water ; SWOT ; Water level fluctuations ; Water levels ; Water surface slope ; wetlands</subject><ispartof>Remote sensing letters, 2023-12, Vol.14 (12), p.1238-1250</ispartof><rights>2023 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group. 2023</rights><rights>2023 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group. This work is licensed under the Creative Commons Attribution – Non-Commercial – No Derivatives License http://creativecommons.org/licenses/by-nc-nd/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c385t-4f070d9c892dd2eedeb0529ca53991c80a46509261dfbee412b0f41f389de6823</citedby><cites>FETCH-LOGICAL-c385t-4f070d9c892dd2eedeb0529ca53991c80a46509261dfbee412b0f41f389de6823</cites><orcidid>0000-0002-4748-2938 ; 0000-0001-6866-5904 ; 0000-0003-2352-546X ; 0000-0002-0613-3838 ; 0000-0001-9786-2747 ; 0000-0002-3525-6220</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Smith, Laurence C.</creatorcontrib><creatorcontrib>Fayne, Jessica V.</creatorcontrib><creatorcontrib>Wang, Bo</creatorcontrib><creatorcontrib>Kyzivat, Ethan D.</creatorcontrib><creatorcontrib>Gleason, Colin J.</creatorcontrib><creatorcontrib>Harlan, Merritt E.</creatorcontrib><creatorcontrib>Langhorst, Theodore</creatorcontrib><creatorcontrib>Feng, Dongmei</creatorcontrib><creatorcontrib>Pavelsky, Tamlin M.</creatorcontrib><creatorcontrib>Peters, Daniel L.</creatorcontrib><title>Peace-Athabasca Delta water surface elevations and slopes mapped from AirSWOT Ka-band InSAR</title><title>Remote sensing letters</title><description>In late
2023 the Surface Water and Ocean Topography (SWOT) satellite mission will release
unprecedented high-resolution measurements of water surface elevation (WSE) and
water surface slope (WSS) globally. SWOT's exciting Ka-band near-nadir
wide-swath interferometric radar (InSAR) technology could transform studies of surface
water hydrology, but remains highly experimental. We examine Airborne SWOT
(AirSWOT) data acquired twice over Canada's Peace-Athabasca Delta (PAD), a
large, low-gradient, ecologically important riverine wetland complex. While
noisy and susceptible to "dark water" (low-return) data losses, spatially
averaged AirSWOT WSE observations reveal a broad-scale water-level decline of ~44
cmn (σ =271 cm) between 9 July and 13 August 2017, similar to a ~56 cm decline (σ=33 cm) recorded by four in situ gauging stations.
River flow directions and WSS are correctly inferred following filtering and
reach-averaging of AirSWOT data, but ~10 km reaches are essential to retrieve them.
July AirSWOT observations suggest steeper WSS down an alternate flow course
(Embarras River-Mamawi Creek distributary) of the Athabasca River, consistent
with field surveys conducted the following year. This signifies potential for
the Athabasca River to avulse northward into Mamawi Lake, with transformative
impacts on flooding, sedimentation, ecology, and human activities in the PAD.
Although AirSWOT differs from SWOT, we conclude SWOT Ka-band InSAR observations
may detect water level changes and avulsion potentials in other low-gradient
deltas globally.</description><subject>AirSWOT</subject><subject>Avulsion</subject><subject>Coastal inlets</subject><subject>Data acquisition</subject><subject>Data loss</subject><subject>Discharge measurement</subject><subject>Extremely high frequencies</subject><subject>Gaging stations</subject><subject>Hydrology</subject><subject>Interferometric synthetic aperture radar</subject><subject>Lakes</subject><subject>Radar</subject><subject>radar remote sensing</subject><subject>river avulsion</subject><subject>River flow</subject><subject>Rivers</subject><subject>Stream discharge</subject><subject>Surface water</subject><subject>SWOT</subject><subject>Water level fluctuations</subject><subject>Water levels</subject><subject>Water surface slope</subject><subject>wetlands</subject><issn>2150-704X</issn><issn>2150-7058</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>0YH</sourceid><recordid>eNp9kE1Lw0AQhoMoWLQ_QVjwnDq72aSbm6V-YqHiBwoelkl2FlPSbNxNLf33prR6dC4zzLzzDvNE0RmHEQcFF4KnMAb5PhIgkpEQCmQmD6LBth-PIVWHf7V8P46GISygj4RLNVaD6OORsKR40n1igaFEdkV1h2yNHXkWVt72U0Y1fWNXuSYwbAwLtWspsCW2LRlmvVuySeWf3-Yv7AHjYiu5b54nT6fRkcU60HCfT6LXm-uX6V08m9_eTyezuExU2sXS9g-YvFS5MEYQGSogFXmJaZLnvFSAMkshFxk3tiCSXBRgJbeJyg1lSiQn0fnOt_Xua0Wh0wu38k1_UoscknEmIYVele5UpXcheLK69dUS_UZz0FuU-hel3qLUe5T93uVur2qs80tcO18b3eGmdt56bMoq6OR_ix_As3lR</recordid><startdate>20231202</startdate><enddate>20231202</enddate><creator>Smith, Laurence C.</creator><creator>Fayne, Jessica V.</creator><creator>Wang, Bo</creator><creator>Kyzivat, Ethan D.</creator><creator>Gleason, Colin J.</creator><creator>Harlan, Merritt E.</creator><creator>Langhorst, Theodore</creator><creator>Feng, Dongmei</creator><creator>Pavelsky, Tamlin M.</creator><creator>Peters, Daniel L.</creator><general>Taylor & Francis</general><general>Taylor & Francis Ltd</general><scope>0YH</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><orcidid>https://orcid.org/0000-0002-4748-2938</orcidid><orcidid>https://orcid.org/0000-0001-6866-5904</orcidid><orcidid>https://orcid.org/0000-0003-2352-546X</orcidid><orcidid>https://orcid.org/0000-0002-0613-3838</orcidid><orcidid>https://orcid.org/0000-0001-9786-2747</orcidid><orcidid>https://orcid.org/0000-0002-3525-6220</orcidid></search><sort><creationdate>20231202</creationdate><title>Peace-Athabasca Delta water surface elevations and slopes mapped from AirSWOT Ka-band InSAR</title><author>Smith, Laurence C. ; Fayne, Jessica V. ; Wang, Bo ; Kyzivat, Ethan D. ; Gleason, Colin J. ; Harlan, Merritt E. ; Langhorst, Theodore ; Feng, Dongmei ; Pavelsky, Tamlin M. ; Peters, Daniel L.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c385t-4f070d9c892dd2eedeb0529ca53991c80a46509261dfbee412b0f41f389de6823</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>AirSWOT</topic><topic>Avulsion</topic><topic>Coastal inlets</topic><topic>Data acquisition</topic><topic>Data loss</topic><topic>Discharge measurement</topic><topic>Extremely high frequencies</topic><topic>Gaging stations</topic><topic>Hydrology</topic><topic>Interferometric synthetic aperture radar</topic><topic>Lakes</topic><topic>Radar</topic><topic>radar remote sensing</topic><topic>river avulsion</topic><topic>River flow</topic><topic>Rivers</topic><topic>Stream discharge</topic><topic>Surface water</topic><topic>SWOT</topic><topic>Water level fluctuations</topic><topic>Water levels</topic><topic>Water surface slope</topic><topic>wetlands</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Smith, Laurence C.</creatorcontrib><creatorcontrib>Fayne, Jessica V.</creatorcontrib><creatorcontrib>Wang, Bo</creatorcontrib><creatorcontrib>Kyzivat, Ethan D.</creatorcontrib><creatorcontrib>Gleason, Colin J.</creatorcontrib><creatorcontrib>Harlan, Merritt E.</creatorcontrib><creatorcontrib>Langhorst, Theodore</creatorcontrib><creatorcontrib>Feng, Dongmei</creatorcontrib><creatorcontrib>Pavelsky, Tamlin M.</creatorcontrib><creatorcontrib>Peters, Daniel L.</creatorcontrib><collection>Taylor & Francis_OA刊</collection><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Remote sensing letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Smith, Laurence C.</au><au>Fayne, Jessica V.</au><au>Wang, Bo</au><au>Kyzivat, Ethan D.</au><au>Gleason, Colin J.</au><au>Harlan, Merritt E.</au><au>Langhorst, Theodore</au><au>Feng, Dongmei</au><au>Pavelsky, Tamlin M.</au><au>Peters, Daniel L.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Peace-Athabasca Delta water surface elevations and slopes mapped from AirSWOT Ka-band InSAR</atitle><jtitle>Remote sensing letters</jtitle><date>2023-12-02</date><risdate>2023</risdate><volume>14</volume><issue>12</issue><spage>1238</spage><epage>1250</epage><pages>1238-1250</pages><issn>2150-704X</issn><eissn>2150-7058</eissn><abstract>In late
2023 the Surface Water and Ocean Topography (SWOT) satellite mission will release
unprecedented high-resolution measurements of water surface elevation (WSE) and
water surface slope (WSS) globally. SWOT's exciting Ka-band near-nadir
wide-swath interferometric radar (InSAR) technology could transform studies of surface
water hydrology, but remains highly experimental. We examine Airborne SWOT
(AirSWOT) data acquired twice over Canada's Peace-Athabasca Delta (PAD), a
large, low-gradient, ecologically important riverine wetland complex. While
noisy and susceptible to "dark water" (low-return) data losses, spatially
averaged AirSWOT WSE observations reveal a broad-scale water-level decline of ~44
cmn (σ =271 cm) between 9 July and 13 August 2017, similar to a ~56 cm decline (σ=33 cm) recorded by four in situ gauging stations.
River flow directions and WSS are correctly inferred following filtering and
reach-averaging of AirSWOT data, but ~10 km reaches are essential to retrieve them.
July AirSWOT observations suggest steeper WSS down an alternate flow course
(Embarras River-Mamawi Creek distributary) of the Athabasca River, consistent
with field surveys conducted the following year. This signifies potential for
the Athabasca River to avulse northward into Mamawi Lake, with transformative
impacts on flooding, sedimentation, ecology, and human activities in the PAD.
Although AirSWOT differs from SWOT, we conclude SWOT Ka-band InSAR observations
may detect water level changes and avulsion potentials in other low-gradient
deltas globally.</abstract><cop>Abingdon</cop><pub>Taylor & Francis</pub><doi>10.1080/2150704X.2023.2280464</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0002-4748-2938</orcidid><orcidid>https://orcid.org/0000-0001-6866-5904</orcidid><orcidid>https://orcid.org/0000-0003-2352-546X</orcidid><orcidid>https://orcid.org/0000-0002-0613-3838</orcidid><orcidid>https://orcid.org/0000-0001-9786-2747</orcidid><orcidid>https://orcid.org/0000-0002-3525-6220</orcidid><oa>free_for_read</oa></addata></record> |
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source | Taylor and Francis Science and Technology Collection |
subjects | AirSWOT Avulsion Coastal inlets Data acquisition Data loss Discharge measurement Extremely high frequencies Gaging stations Hydrology Interferometric synthetic aperture radar Lakes Radar radar remote sensing river avulsion River flow Rivers Stream discharge Surface water SWOT Water level fluctuations Water levels Water surface slope wetlands |
title | Peace-Athabasca Delta water surface elevations and slopes mapped from AirSWOT Ka-band InSAR |
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