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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Online Access: | https://doi.org/10.34657/1262 https://oa.tib.eu/renate/handle/123456789/430 |
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ftleibnizopen:oai:oai.leibnizopen.de:_9-Om4YBdbrxVwz60GBT 2023-05-15T17:33:26+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/ CC-BY 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 2023-03-01T07:46:46Z 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_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.34657/1262 |
_version_ |
1766131942694060032 |