Dried, closed-path eddy covariance method for measuring carbon dioxide flux over sea ice
The Arctic marine environment plays an important role in the global carbon cycle. However, there remain large uncertainties in how sea ice affects air–sea fluxes of carbon dioxide ( CO 2 ), partially due to disagreement between the two main methods (enclosure and eddy covariance) for measuring CO 2...
Published in: | Atmospheric Measurement Techniques |
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Language: | English |
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2019
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Online Access: | https://doi.org/10.5194/amt-11-6075-2018 https://amt.copernicus.org/articles/11/6075/2018/ |
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The Arctic marine environment plays an important role in the global carbon cycle. However, there remain large uncertainties in how sea ice affects air–sea fluxes of carbon dioxide ( CO 2 ), partially due to disagreement between the two main methods (enclosure and eddy covariance) for measuring CO 2 flux ( <math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msub><mi>F</mi><mrow><mi mathvariant="normal">CO</mi><msub><mi/><mn mathvariant="normal">2</mn></msub></mrow></msub></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="6b8cbfd9be1fe094f1cc39ba3389da73"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-11-6075-2018-ie00001.svg" width="23pt" height="14pt" src="amt-11-6075-2018-ie00001.png"/></svg:svg> ). The enclosure method has appeared to produce more credible <math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msub><mi>F</mi><mrow><mi mathvariant="normal">CO</mi><msub><mi/><mn mathvariant="normal">2</mn></msub></mrow></msub></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="647cda4c1184e3ee1e2e34e33689234d"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-11-6075-2018-ie00002.svg" width="23pt" height="14pt" src="amt-11-6075-2018-ie00002.png"/></svg:svg> than eddy covariance (EC), but is not suited for collecting long-term, ecosystem-scale flux datasets in such remote regions. Here we describe the design and performance of an EC system to measure <math xmlns="http://www.w3.org/1998/Math/MathML" id="M6" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msub><mi>F</mi><mrow><mi mathvariant="normal">CO</mi><msub><mi/><mn mathvariant="normal">2</mn></msub></mrow></msub></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="0632e7a6a53d08c3ed8efc4956b7f74c"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-11-6075-2018-ie00003.svg" width="23pt" height="14pt" src="amt-11-6075-2018-ie00003.png"/></svg:svg> over landfast sea ice that addresses the shortcomings of previous EC systems. The system was installed on a 10 m tower on Qikirtaarjuk Island – a small rock outcrop in Dease Strait located roughly 35 km west of Cambridge Bay, Nunavut, in the Canadian Arctic Archipelago. The system incorporates recent developments in the field of air–sea gas exchange by measuring atmospheric CO 2 using a closed-path infrared gas analyzer (IRGA) with a dried sample airstream, thus avoiding the known water vapor issues associated with using open-path IRGAs in low-flux environments. A description of the methods and the results from 4 months of continuous flux measurements from May through August 2017 are presented, highlighting the winter to summer transition from ice cover to open water. We show that the dried, closed-path EC system greatly reduces the magnitude of measured <math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msub><mi>F</mi><mrow><mi mathvariant="normal">CO</mi><msub><mi/><mn mathvariant="normal">2</mn></msub></mrow></msub></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="201812cb0124c03de581e702a3f1399b"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-11-6075-2018-ie00004.svg" width="23pt" height="14pt" src="amt-11-6075-2018-ie00004.png"/></svg:svg> compared to simultaneous open-path EC measurements, and for the first time reconciles EC and enclosure flux measurements over sea ice. This novel EC installation is capable of operating year-round on solar and wind power, and therefore promises to deliver new insights into the magnitude of CO 2 fluxes and their driving processes through the annual sea ice cycle. |
format |
Text |
author |
Butterworth, Brian J. Else, Brent G. T. |
spellingShingle |
Butterworth, Brian J. Else, Brent G. T. Dried, closed-path eddy covariance method for measuring carbon dioxide flux over sea ice |
author_facet |
Butterworth, Brian J. Else, Brent G. T. |
author_sort |
Butterworth, Brian J. |
title |
Dried, closed-path eddy covariance method for measuring carbon dioxide flux over sea ice |
title_short |
Dried, closed-path eddy covariance method for measuring carbon dioxide flux over sea ice |
title_full |
Dried, closed-path eddy covariance method for measuring carbon dioxide flux over sea ice |
title_fullStr |
Dried, closed-path eddy covariance method for measuring carbon dioxide flux over sea ice |
title_full_unstemmed |
Dried, closed-path eddy covariance method for measuring carbon dioxide flux over sea ice |
title_sort |
dried, closed-path eddy covariance method for measuring carbon dioxide flux over sea ice |
publishDate |
2019 |
url |
https://doi.org/10.5194/amt-11-6075-2018 https://amt.copernicus.org/articles/11/6075/2018/ |
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ENVELOPE(-105.130,-105.130,69.037,69.037) ENVELOPE(-107.502,-107.502,68.834,68.834) ENVELOPE(-115.020,-115.020,69.251,69.251) ENVELOPE(-45.592,-45.592,-60.702,-60.702) |
geographic |
Arctic Cambridge Bay Canadian Arctic Archipelago Dease Strait Nunavut Qikirtaarjuk Island Small Rock |
geographic_facet |
Arctic Cambridge Bay Canadian Arctic Archipelago Dease Strait Nunavut Qikirtaarjuk Island Small Rock |
genre |
Arctic Archipelago Arctic Cambridge Bay Canadian Arctic Archipelago Nunavut Sea ice |
genre_facet |
Arctic Archipelago Arctic Cambridge Bay Canadian Arctic Archipelago Nunavut Sea ice |
op_source |
eISSN: 1867-8548 |
op_relation |
doi:10.5194/amt-11-6075-2018 https://amt.copernicus.org/articles/11/6075/2018/ |
op_doi |
https://doi.org/10.5194/amt-11-6075-2018 |
container_title |
Atmospheric Measurement Techniques |
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11 |
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11 |
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6075 |
op_container_end_page |
6090 |
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1766303160148688896 |
spelling |
ftcopernicus:oai:publications.copernicus.org:amt68878 2023-05-15T14:29:04+02:00 Dried, closed-path eddy covariance method for measuring carbon dioxide flux over sea ice Butterworth, Brian J. Else, Brent G. T. 2019-01-04 application/pdf https://doi.org/10.5194/amt-11-6075-2018 https://amt.copernicus.org/articles/11/6075/2018/ eng eng doi:10.5194/amt-11-6075-2018 https://amt.copernicus.org/articles/11/6075/2018/ eISSN: 1867-8548 Text 2019 ftcopernicus https://doi.org/10.5194/amt-11-6075-2018 2020-07-20T16:23:04Z The Arctic marine environment plays an important role in the global carbon cycle. However, there remain large uncertainties in how sea ice affects air–sea fluxes of carbon dioxide ( CO 2 ), partially due to disagreement between the two main methods (enclosure and eddy covariance) for measuring CO 2 flux ( <math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msub><mi>F</mi><mrow><mi mathvariant="normal">CO</mi><msub><mi/><mn mathvariant="normal">2</mn></msub></mrow></msub></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="6b8cbfd9be1fe094f1cc39ba3389da73"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-11-6075-2018-ie00001.svg" width="23pt" height="14pt" src="amt-11-6075-2018-ie00001.png"/></svg:svg> ). The enclosure method has appeared to produce more credible <math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msub><mi>F</mi><mrow><mi mathvariant="normal">CO</mi><msub><mi/><mn mathvariant="normal">2</mn></msub></mrow></msub></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="647cda4c1184e3ee1e2e34e33689234d"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-11-6075-2018-ie00002.svg" width="23pt" height="14pt" src="amt-11-6075-2018-ie00002.png"/></svg:svg> than eddy covariance (EC), but is not suited for collecting long-term, ecosystem-scale flux datasets in such remote regions. Here we describe the design and performance of an EC system to measure <math xmlns="http://www.w3.org/1998/Math/MathML" id="M6" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msub><mi>F</mi><mrow><mi mathvariant="normal">CO</mi><msub><mi/><mn mathvariant="normal">2</mn></msub></mrow></msub></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="0632e7a6a53d08c3ed8efc4956b7f74c"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-11-6075-2018-ie00003.svg" width="23pt" height="14pt" src="amt-11-6075-2018-ie00003.png"/></svg:svg> over landfast sea ice that addresses the shortcomings of previous EC systems. The system was installed on a 10 m tower on Qikirtaarjuk Island – a small rock outcrop in Dease Strait located roughly 35 km west of Cambridge Bay, Nunavut, in the Canadian Arctic Archipelago. The system incorporates recent developments in the field of air–sea gas exchange by measuring atmospheric CO 2 using a closed-path infrared gas analyzer (IRGA) with a dried sample airstream, thus avoiding the known water vapor issues associated with using open-path IRGAs in low-flux environments. A description of the methods and the results from 4 months of continuous flux measurements from May through August 2017 are presented, highlighting the winter to summer transition from ice cover to open water. We show that the dried, closed-path EC system greatly reduces the magnitude of measured <math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msub><mi>F</mi><mrow><mi mathvariant="normal">CO</mi><msub><mi/><mn mathvariant="normal">2</mn></msub></mrow></msub></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="201812cb0124c03de581e702a3f1399b"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-11-6075-2018-ie00004.svg" width="23pt" height="14pt" src="amt-11-6075-2018-ie00004.png"/></svg:svg> compared to simultaneous open-path EC measurements, and for the first time reconciles EC and enclosure flux measurements over sea ice. This novel EC installation is capable of operating year-round on solar and wind power, and therefore promises to deliver new insights into the magnitude of CO 2 fluxes and their driving processes through the annual sea ice cycle. Text Arctic Archipelago Arctic Cambridge Bay Canadian Arctic Archipelago Nunavut Sea ice Copernicus Publications: E-Journals Arctic Cambridge Bay ENVELOPE(-105.130,-105.130,69.037,69.037) Canadian Arctic Archipelago Dease Strait ENVELOPE(-107.502,-107.502,68.834,68.834) Nunavut Qikirtaarjuk Island ENVELOPE(-115.020,-115.020,69.251,69.251) Small Rock ENVELOPE(-45.592,-45.592,-60.702,-60.702) Atmospheric Measurement Techniques 11 11 6075 6090 |