Loading…

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...

Full description

Saved in:
Bibliographic Details
Published in:Remote sensing letters 2023-12, Vol.14 (12), p.1238-1250
Main Authors: 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.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c385t-4f070d9c892dd2eedeb0529ca53991c80a46509261dfbee412b0f41f389de6823
cites cdi_FETCH-LOGICAL-c385t-4f070d9c892dd2eedeb0529ca53991c80a46509261dfbee412b0f41f389de6823
container_end_page 1250
container_issue 12
container_start_page 1238
container_title Remote sensing letters
container_volume 14
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
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_crossref_primary_10_1080_2150704X_2023_2280464</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2903764050</sourcerecordid><originalsourceid>FETCH-LOGICAL-c385t-4f070d9c892dd2eedeb0529ca53991c80a46509261dfbee412b0f41f389de6823</originalsourceid><addsrcrecordid>eNp9kE1Lw0AQhoMoWLQ_QVjwnDq72aSbm6V-YqHiBwoelkl2FlPSbNxNLf33prR6dC4zzLzzDvNE0RmHEQcFF4KnMAb5PhIgkpEQCmQmD6LBth-PIVWHf7V8P46GISygj4RLNVaD6OORsKR40n1igaFEdkV1h2yNHXkWVt72U0Y1fWNXuSYwbAwLtWspsCW2LRlmvVuySeWf3-Yv7AHjYiu5b54nT6fRkcU60HCfT6LXm-uX6V08m9_eTyezuExU2sXS9g-YvFS5MEYQGSogFXmJaZLnvFSAMkshFxk3tiCSXBRgJbeJyg1lSiQn0fnOt_Xua0Wh0wu38k1_UoscknEmIYVele5UpXcheLK69dUS_UZz0FuU-hel3qLUe5T93uVur2qs80tcO18b3eGmdt56bMoq6OR_ix_As3lR</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2903764050</pqid></control><display><type>article</type><title>Peace-Athabasca Delta water surface elevations and slopes mapped from AirSWOT Ka-band InSAR</title><source>Taylor and Francis Science and Technology Collection</source><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.</creator><creatorcontrib>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.</creatorcontrib><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><identifier>ISSN: 2150-704X</identifier><identifier>EISSN: 2150-7058</identifier><identifier>DOI: 10.1080/2150704X.2023.2280464</identifier><language>eng</language><publisher>Abingdon: Taylor &amp; 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 &amp; Francis Group. 2023</rights><rights>2023 The Author(s). Published by Informa UK Limited, trading as Taylor &amp; 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 &amp; Francis</general><general>Taylor &amp; 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 &amp; 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 &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science &amp; 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 &amp; 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>
fulltext fulltext
identifier ISSN: 2150-704X
ispartof Remote sensing letters, 2023-12, Vol.14 (12), p.1238-1250
issn 2150-704X
2150-7058
language eng
recordid cdi_crossref_primary_10_1080_2150704X_2023_2280464
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
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-06T11%3A30%3A14IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Peace-Athabasca%20Delta%20water%20surface%20elevations%20and%20slopes%20mapped%20from%20AirSWOT%20Ka-band%20InSAR&rft.jtitle=Remote%20sensing%20letters&rft.au=Smith,%20Laurence%20C.&rft.date=2023-12-02&rft.volume=14&rft.issue=12&rft.spage=1238&rft.epage=1250&rft.pages=1238-1250&rft.issn=2150-704X&rft.eissn=2150-7058&rft_id=info:doi/10.1080/2150704X.2023.2280464&rft_dat=%3Cproquest_cross%3E2903764050%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c385t-4f070d9c892dd2eedeb0529ca53991c80a46509261dfbee412b0f41f389de6823%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2903764050&rft_id=info:pmid/&rfr_iscdi=true