Short-term variations in atmospheric CO2 at Ny-Ålesund, Spitsbergen, during spring and summer

Results from the continuous measurements of atmospheric carbon dioxide performed at Ny-Ålesund, Spitsbergen are presented. The results are discussed with an emphasis on day-today variations during spring and early summer. During all years studied, significant negative anomalies (“dips”), lasting for...

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Main Authors: Engardt, Magnuz, Holmén, Kim, Heintzenberg, Jost
Format: Article in Journal/Newspaper
Language:English
Published: Milton Park : Taylor & Francis 2017
Subjects:
550
Online Access:https://doi.org/10.34657/1262
https://oa.tib.eu/renate/handle/123456789/430
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record_format openpolar
spelling ftleibnizopen:oai:oai.leibnizopen.de:QnXfXIkBdbrxVwz6UP9X 2023-07-30T04:05:27+02:00 Short-term variations in atmospheric CO2 at Ny-Ålesund, Spitsbergen, during spring and summer Engardt, Magnuz Holmén, Kim Heintzenberg, Jost 2017 application/pdf https://doi.org/10.34657/1262 https://oa.tib.eu/renate/handle/123456789/430 eng eng Milton Park : Taylor & Francis CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/ Tellus B: Chemical and Physical Meteorology, Volume 48, Issue 1, Page 33-43 air back trajectory atmospheric carbon dioxide carbon dioxide sink surface water variation 550 article Text 2017 ftleibnizopen https://doi.org/10.34657/1262 2023-07-16T23:25:14Z Results from the continuous measurements of atmospheric carbon dioxide performed at Ny-Ålesund, Spitsbergen are presented. The results are discussed with an emphasis on day-today variations during spring and early summer. During all years studied, significant negative anomalies (“dips”), lasting for several days, have been observed in the data from late May through July. The timing coincides with a draw down of dissolved carbon dioxide and nutrients in the surface waters of the North Atlantic observed by others. By using 3-dimensional trajectories, we follow the history of the air arriving in Ny-Ålesund, and show that the air, depleted in CO2 , had been in contact with these waters. Combining the trajectories with a box model yields a simple Lagrangian model, and we demonstrate that the timing and magnitude of the dips are consistent with the degree of CO2 saturation of the sea during April to mid-June. In late June and July, the model indicates that a significant portion of the dips must have other causes, e.g., CO2 uptake in the terrestrial biosphere further south. publishedVersion Article in Journal/Newspaper North Atlantic Ny Ålesund Ny-Ålesund Spitsbergen LeibnizOpen (The Leibniz Association) Ny-Ålesund
institution Open Polar
collection LeibnizOpen (The Leibniz Association)
op_collection_id ftleibnizopen
language English
topic air back trajectory
atmospheric carbon dioxide
carbon dioxide sink
surface water
variation
550
spellingShingle air back trajectory
atmospheric carbon dioxide
carbon dioxide sink
surface water
variation
550
Engardt, Magnuz
Holmén, Kim
Heintzenberg, Jost
Short-term variations in atmospheric CO2 at Ny-Ålesund, Spitsbergen, during spring and summer
topic_facet air back trajectory
atmospheric carbon dioxide
carbon dioxide sink
surface water
variation
550
description Results from the continuous measurements of atmospheric carbon dioxide performed at Ny-Ålesund, Spitsbergen are presented. The results are discussed with an emphasis on day-today variations during spring and early summer. During all years studied, significant negative anomalies (“dips”), lasting for several days, have been observed in the data from late May through July. The timing coincides with a draw down of dissolved carbon dioxide and nutrients in the surface waters of the North Atlantic observed by others. By using 3-dimensional trajectories, we follow the history of the air arriving in Ny-Ålesund, and show that the air, depleted in CO2 , had been in contact with these waters. Combining the trajectories with a box model yields a simple Lagrangian model, and we demonstrate that the timing and magnitude of the dips are consistent with the degree of CO2 saturation of the sea during April to mid-June. In late June and July, the model indicates that a significant portion of the dips must have other causes, e.g., CO2 uptake in the terrestrial biosphere further south. publishedVersion
format Article in Journal/Newspaper
author Engardt, Magnuz
Holmén, Kim
Heintzenberg, Jost
author_facet Engardt, Magnuz
Holmén, Kim
Heintzenberg, Jost
author_sort Engardt, Magnuz
title Short-term variations in atmospheric CO2 at Ny-Ålesund, Spitsbergen, during spring and summer
title_short Short-term variations in atmospheric CO2 at Ny-Ålesund, Spitsbergen, during spring and summer
title_full Short-term variations in atmospheric CO2 at Ny-Ålesund, Spitsbergen, during spring and summer
title_fullStr Short-term variations in atmospheric CO2 at Ny-Ålesund, Spitsbergen, during spring and summer
title_full_unstemmed Short-term variations in atmospheric CO2 at Ny-Ålesund, Spitsbergen, during spring and summer
title_sort short-term variations in atmospheric co2 at ny-ålesund, spitsbergen, during spring and summer
publisher Milton Park : Taylor & Francis
publishDate 2017
url https://doi.org/10.34657/1262
https://oa.tib.eu/renate/handle/123456789/430
geographic Ny-Ålesund
geographic_facet Ny-Ålesund
genre North Atlantic
Ny Ålesund
Ny-Ålesund
Spitsbergen
genre_facet North Atlantic
Ny Ålesund
Ny-Ålesund
Spitsbergen
op_source Tellus B: Chemical and Physical Meteorology, Volume 48, Issue 1, Page 33-43
op_rights CC BY 4.0 Unported
https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.34657/1262
_version_ 1772817365179826176