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Total Aquatic Carbon Emissions Across the Boreal Biome of Québec Driven by Watershed Slope
Inland waters emit large amounts of CO2 and CH4 to the atmosphere, partially offsetting the sequestration of carbon in terrestrial ecosystems. However, the incorporation of inland waters into landscape carbon budgets remains challenging, hampered by a lack of studies that consider both carbon gases...
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Published in: | Journal of geophysical research. Biogeosciences 2021-01, Vol.126 (1), p.n/a |
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description | Inland waters emit large amounts of CO2 and CH4 to the atmosphere, partially offsetting the sequestration of carbon in terrestrial ecosystems. However, the incorporation of inland waters into landscape carbon budgets remains challenging, hampered by a lack of studies that consider both carbon gases and the variety of aquatic systems (streams, rivers, and lakes). Here we develop a whole‐network assessment of total aquatic carbon emissions for a set of large watersheds in boreal Québec, Canada. Expressed per unit watershed area, our estimates of total (CO2 + CH4) aquatic carbon emissions range between 11 and 38 g C m−2 yr−1 and cannot be predicted from the size of the watershed or the total surface area of aquatic systems. Rather, we show that total aquatic emissions vary across the boreal landscape of Québec as a function of the average slope of the watershed, which indirectly accounts for the configuration of aquatic networks, the physical forcing that influences gas exchange in fluvial systems, and the potential amount of soil carbon reaching aquatic systems. Total aquatic carbon emissions in boreal Québec are of the same range and magnitude of variation than other components of the boreal carbon budget and could offset terrestrial net ecosystem productivity by as much as 38%.
Plain Language Summary
Inland waters are natural emitters of greenhouse gases to the atmosphere, partially offsetting the CO2 uptake by agricultural, forest, and wetland ecosystems. Nevertheless, the role of inland waters is rarely incorporated into regional greenhouse gas inventories. One of the main reasons is that there are very few estimates that integrate CO2 emissions from streams, rivers, and lakes at the large scale, and even fewer that in addition consider methane. Here we present the first assessment of total aquatic carbon emissions at the regional scale, which we developed for the boreal biome of Québec, Canada, and explore how these aquatic emissions vary across this northern landscape. We show that total aquatic carbon emissions covary nonlinearly with the average slope of the watershed, such that maximal emissions occur both in the flattest and steepest landscapes. We further demonstrate that aquatic emissions could offset terrestrial carbon sinks by as much as 38%, and provide simple tools to incorporate inland waters into regional greenhouse gas inventories.
Key Points
We have modeled CO2 and CH4 emissions from streams, rivers, and lakes across boreal Québec, Canada |
doi_str_mv | 10.1029/2020JG005863 |
format | article |
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Plain Language Summary
Inland waters are natural emitters of greenhouse gases to the atmosphere, partially offsetting the CO2 uptake by agricultural, forest, and wetland ecosystems. Nevertheless, the role of inland waters is rarely incorporated into regional greenhouse gas inventories. One of the main reasons is that there are very few estimates that integrate CO2 emissions from streams, rivers, and lakes at the large scale, and even fewer that in addition consider methane. Here we present the first assessment of total aquatic carbon emissions at the regional scale, which we developed for the boreal biome of Québec, Canada, and explore how these aquatic emissions vary across this northern landscape. We show that total aquatic carbon emissions covary nonlinearly with the average slope of the watershed, such that maximal emissions occur both in the flattest and steepest landscapes. We further demonstrate that aquatic emissions could offset terrestrial carbon sinks by as much as 38%, and provide simple tools to incorporate inland waters into regional greenhouse gas inventories.
Key Points
We have modeled CO2 and CH4 emissions from streams, rivers, and lakes across boreal Québec, Canada
Normalized by watershed area, total aquatic carbon emissions are unrelated to percent water coverage but covary with watershed average slope
Total aquatic carbon emissions could offset terrestrial carbon uptake by as much as 38%</description><identifier>ISSN: 2169-8953</identifier><identifier>EISSN: 2169-8961</identifier><identifier>DOI: 10.1029/2020JG005863</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Agricultural ecosystems ; Aquatic ecosystems ; Aquatic environment ; aquatic network ; Atmosphere ; Carbon ; Carbon dioxide ; Carbon dioxide emissions ; Carbon footprint ; Carbon sequestration ; Carbon sinks ; Creeks & streams ; Ecosystems ; Emission inventories ; Emissions ; Emitters ; Farm buildings ; Gas exchange ; Gases ; Greenhouse effect ; Greenhouse gases ; Inland waters ; Inventories ; Lakes ; Landscape ; Methane ; Regional development ; Rivers ; Soil ; Streams ; Terrestrial ecosystems ; Uptake ; Watersheds</subject><ispartof>Journal of geophysical research. Biogeosciences, 2021-01, Vol.126 (1), p.n/a</ispartof><rights>2020. American Geophysical Union. All Rights Reserved.</rights><rights>2021. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3507-66c8ee9cf447125b424c5ba63f25f751640a8772eac1dc895c24b748f13944443</citedby><cites>FETCH-LOGICAL-c3507-66c8ee9cf447125b424c5ba63f25f751640a8772eac1dc895c24b748f13944443</cites><orcidid>0000-0002-1696-4934 ; 0000-0003-4708-9332</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>Casas‐Ruiz, Joan P.</creatorcontrib><creatorcontrib>Hutchins, Ryan H. S.</creatorcontrib><creatorcontrib>Giorgio, Paul A.</creatorcontrib><title>Total Aquatic Carbon Emissions Across the Boreal Biome of Québec Driven by Watershed Slope</title><title>Journal of geophysical research. Biogeosciences</title><description>Inland waters emit large amounts of CO2 and CH4 to the atmosphere, partially offsetting the sequestration of carbon in terrestrial ecosystems. However, the incorporation of inland waters into landscape carbon budgets remains challenging, hampered by a lack of studies that consider both carbon gases and the variety of aquatic systems (streams, rivers, and lakes). Here we develop a whole‐network assessment of total aquatic carbon emissions for a set of large watersheds in boreal Québec, Canada. Expressed per unit watershed area, our estimates of total (CO2 + CH4) aquatic carbon emissions range between 11 and 38 g C m−2 yr−1 and cannot be predicted from the size of the watershed or the total surface area of aquatic systems. Rather, we show that total aquatic emissions vary across the boreal landscape of Québec as a function of the average slope of the watershed, which indirectly accounts for the configuration of aquatic networks, the physical forcing that influences gas exchange in fluvial systems, and the potential amount of soil carbon reaching aquatic systems. Total aquatic carbon emissions in boreal Québec are of the same range and magnitude of variation than other components of the boreal carbon budget and could offset terrestrial net ecosystem productivity by as much as 38%.
Plain Language Summary
Inland waters are natural emitters of greenhouse gases to the atmosphere, partially offsetting the CO2 uptake by agricultural, forest, and wetland ecosystems. Nevertheless, the role of inland waters is rarely incorporated into regional greenhouse gas inventories. One of the main reasons is that there are very few estimates that integrate CO2 emissions from streams, rivers, and lakes at the large scale, and even fewer that in addition consider methane. Here we present the first assessment of total aquatic carbon emissions at the regional scale, which we developed for the boreal biome of Québec, Canada, and explore how these aquatic emissions vary across this northern landscape. We show that total aquatic carbon emissions covary nonlinearly with the average slope of the watershed, such that maximal emissions occur both in the flattest and steepest landscapes. We further demonstrate that aquatic emissions could offset terrestrial carbon sinks by as much as 38%, and provide simple tools to incorporate inland waters into regional greenhouse gas inventories.
Key Points
We have modeled CO2 and CH4 emissions from streams, rivers, and lakes across boreal Québec, Canada
Normalized by watershed area, total aquatic carbon emissions are unrelated to percent water coverage but covary with watershed average slope
Total aquatic carbon emissions could offset terrestrial carbon uptake by as much as 38%</description><subject>Agricultural ecosystems</subject><subject>Aquatic ecosystems</subject><subject>Aquatic environment</subject><subject>aquatic network</subject><subject>Atmosphere</subject><subject>Carbon</subject><subject>Carbon dioxide</subject><subject>Carbon dioxide emissions</subject><subject>Carbon footprint</subject><subject>Carbon sequestration</subject><subject>Carbon sinks</subject><subject>Creeks & streams</subject><subject>Ecosystems</subject><subject>Emission inventories</subject><subject>Emissions</subject><subject>Emitters</subject><subject>Farm buildings</subject><subject>Gas exchange</subject><subject>Gases</subject><subject>Greenhouse effect</subject><subject>Greenhouse gases</subject><subject>Inland waters</subject><subject>Inventories</subject><subject>Lakes</subject><subject>Landscape</subject><subject>Methane</subject><subject>Regional development</subject><subject>Rivers</subject><subject>Soil</subject><subject>Streams</subject><subject>Terrestrial ecosystems</subject><subject>Uptake</subject><subject>Watersheds</subject><issn>2169-8953</issn><issn>2169-8961</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp9kM1KAzEUhYMoWGp3PkDAraP5mySzbGsdLQVRKy5cDJk0oVOmkzaZUfpIPocvZrQirjybezl83Ms5AJxidIERyS4JImiaI5RKTg9Aj2CeJTLj-PB3T-kxGISwQlEyWhj3wMvctaqGw22n2krDsfKla-BkXYVQuSbAofYuBNguDRw5byI6qtzaQGfhfffxXhoNr3z1ahpY7uCzao0PS7OAj7XbmBNwZFUdzOBn9sHT9WQ-vklmd_nteDhLNE2RSDjX0phMW8YEJmnJCNNpqTi1JLUixZwhJYUgRmm80DGGJqwUTFpMMxZF--Bsf3fj3bYzoS1WrvNNfFkQJpFENONZpM731Hcib2yx8dVa-V2BUfHVYPG3wYjTPf5W1Wb3L1tM84ecYCEF_QT66HBN</recordid><startdate>202101</startdate><enddate>202101</enddate><creator>Casas‐Ruiz, Joan P.</creator><creator>Hutchins, Ryan H. S.</creator><creator>Giorgio, Paul A.</creator><general>Blackwell Publishing Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0002-1696-4934</orcidid><orcidid>https://orcid.org/0000-0003-4708-9332</orcidid></search><sort><creationdate>202101</creationdate><title>Total Aquatic Carbon Emissions Across the Boreal Biome of Québec Driven by Watershed Slope</title><author>Casas‐Ruiz, Joan P. ; Hutchins, Ryan H. S. ; Giorgio, Paul A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3507-66c8ee9cf447125b424c5ba63f25f751640a8772eac1dc895c24b748f13944443</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Agricultural ecosystems</topic><topic>Aquatic ecosystems</topic><topic>Aquatic environment</topic><topic>aquatic network</topic><topic>Atmosphere</topic><topic>Carbon</topic><topic>Carbon dioxide</topic><topic>Carbon dioxide emissions</topic><topic>Carbon footprint</topic><topic>Carbon sequestration</topic><topic>Carbon sinks</topic><topic>Creeks & streams</topic><topic>Ecosystems</topic><topic>Emission inventories</topic><topic>Emissions</topic><topic>Emitters</topic><topic>Farm buildings</topic><topic>Gas exchange</topic><topic>Gases</topic><topic>Greenhouse effect</topic><topic>Greenhouse gases</topic><topic>Inland waters</topic><topic>Inventories</topic><topic>Lakes</topic><topic>Landscape</topic><topic>Methane</topic><topic>Regional development</topic><topic>Rivers</topic><topic>Soil</topic><topic>Streams</topic><topic>Terrestrial ecosystems</topic><topic>Uptake</topic><topic>Watersheds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Casas‐Ruiz, Joan P.</creatorcontrib><creatorcontrib>Hutchins, Ryan H. S.</creatorcontrib><creatorcontrib>Giorgio, Paul A.</creatorcontrib><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of geophysical research. Biogeosciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Casas‐Ruiz, Joan P.</au><au>Hutchins, Ryan H. S.</au><au>Giorgio, Paul A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Total Aquatic Carbon Emissions Across the Boreal Biome of Québec Driven by Watershed Slope</atitle><jtitle>Journal of geophysical research. Biogeosciences</jtitle><date>2021-01</date><risdate>2021</risdate><volume>126</volume><issue>1</issue><epage>n/a</epage><issn>2169-8953</issn><eissn>2169-8961</eissn><abstract>Inland waters emit large amounts of CO2 and CH4 to the atmosphere, partially offsetting the sequestration of carbon in terrestrial ecosystems. However, the incorporation of inland waters into landscape carbon budgets remains challenging, hampered by a lack of studies that consider both carbon gases and the variety of aquatic systems (streams, rivers, and lakes). Here we develop a whole‐network assessment of total aquatic carbon emissions for a set of large watersheds in boreal Québec, Canada. Expressed per unit watershed area, our estimates of total (CO2 + CH4) aquatic carbon emissions range between 11 and 38 g C m−2 yr−1 and cannot be predicted from the size of the watershed or the total surface area of aquatic systems. Rather, we show that total aquatic emissions vary across the boreal landscape of Québec as a function of the average slope of the watershed, which indirectly accounts for the configuration of aquatic networks, the physical forcing that influences gas exchange in fluvial systems, and the potential amount of soil carbon reaching aquatic systems. Total aquatic carbon emissions in boreal Québec are of the same range and magnitude of variation than other components of the boreal carbon budget and could offset terrestrial net ecosystem productivity by as much as 38%.
Plain Language Summary
Inland waters are natural emitters of greenhouse gases to the atmosphere, partially offsetting the CO2 uptake by agricultural, forest, and wetland ecosystems. Nevertheless, the role of inland waters is rarely incorporated into regional greenhouse gas inventories. One of the main reasons is that there are very few estimates that integrate CO2 emissions from streams, rivers, and lakes at the large scale, and even fewer that in addition consider methane. Here we present the first assessment of total aquatic carbon emissions at the regional scale, which we developed for the boreal biome of Québec, Canada, and explore how these aquatic emissions vary across this northern landscape. We show that total aquatic carbon emissions covary nonlinearly with the average slope of the watershed, such that maximal emissions occur both in the flattest and steepest landscapes. We further demonstrate that aquatic emissions could offset terrestrial carbon sinks by as much as 38%, and provide simple tools to incorporate inland waters into regional greenhouse gas inventories.
Key Points
We have modeled CO2 and CH4 emissions from streams, rivers, and lakes across boreal Québec, Canada
Normalized by watershed area, total aquatic carbon emissions are unrelated to percent water coverage but covary with watershed average slope
Total aquatic carbon emissions could offset terrestrial carbon uptake by as much as 38%</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2020JG005863</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0002-1696-4934</orcidid><orcidid>https://orcid.org/0000-0003-4708-9332</orcidid></addata></record> |
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language | eng |
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source | Wiley; Alma/SFX Local Collection |
subjects | Agricultural ecosystems Aquatic ecosystems Aquatic environment aquatic network Atmosphere Carbon Carbon dioxide Carbon dioxide emissions Carbon footprint Carbon sequestration Carbon sinks Creeks & streams Ecosystems Emission inventories Emissions Emitters Farm buildings Gas exchange Gases Greenhouse effect Greenhouse gases Inland waters Inventories Lakes Landscape Methane Regional development Rivers Soil Streams Terrestrial ecosystems Uptake Watersheds |
title | Total Aquatic Carbon Emissions Across the Boreal Biome of Québec Driven by Watershed Slope |
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