Increased CO 2 loss from vegetated drained lake tundra ecosystems due to flooding

Tundra ecosystems are especially sensitive to climate change, which is particularly rapid in high northern latitudes resulting in significant alterations in temperature and soil moisture. Numerous studies have demonstrated that soil drying increases the respiration loss from wet Arctic tundra. And,...

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Published in:Global Biogeochemical Cycles
Main Authors: Zona, Donatella, Lipson, David A., Paw U, Kyaw T., Oberbauer, Steve F., Olivas, Paulo, Gioli, Beniamino, Oechel, Walter C.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2012
Subjects:
Online Access:https://oro.open.ac.uk/38776/
https://oro.open.ac.uk/38776/1/oechel%201.pdf
https://doi.org/10.1029/2011GB004037
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spelling ftopenunivgb:oai:oro.open.ac.uk:38776 2023-06-11T04:08:55+02:00 Increased CO 2 loss from vegetated drained lake tundra ecosystems due to flooding Zona, Donatella Lipson, David A. Paw U, Kyaw T. Oberbauer, Steve F. Olivas, Paulo Gioli, Beniamino Oechel, Walter C. 2012 application/pdf https://oro.open.ac.uk/38776/ https://oro.open.ac.uk/38776/1/oechel%201.pdf https://doi.org/10.1029/2011GB004037 unknown https://oro.open.ac.uk/38776/1/oechel%201.pdf Zona, Donatella; Lipson, David A.; Paw U, Kyaw T.; Oberbauer, Steve F.; Olivas, Paulo; Gioli, Beniamino and Oechel, Walter C. <http://oro.open.ac.uk/view/person/wco5.html> (2012). Increased CO2 loss from vegetated drained lake tundra ecosystems due to flooding. Global Biogeochemical Cycles, 26(2), article no. GB2004. Journal Item Public PeerReviewed 2012 ftopenunivgb https://doi.org/10.1029/2011GB004037 2023-05-28T05:50:34Z Tundra ecosystems are especially sensitive to climate change, which is particularly rapid in high northern latitudes resulting in significant alterations in temperature and soil moisture. Numerous studies have demonstrated that soil drying increases the respiration loss from wet Arctic tundra. And, warming and drying of tundra soils are assumed to increase CO 2 emissions from the Arctic. However, in this water table manipulation experiment (i.e., flooding experiment), we show that flooding of wet tundra can also lead to increased CO 2 loss. Standing water increased heat conduction into the soil, leading to higher soil temperature, deeper thaw and, surprisingly, to higher CO 2 loss in the most anaerobic of the experimental areas. The study site is located in a drained lake basin, and the soils are characterized by wetter conditions than upland tundra. In experimentally flooded areas, high wind speeds (greater than ~4 m s −1 ) increased CO 2 emission rates, sometimes overwhelming the photosynthetic uptake, even during daytime. This suggests that CO 2 efflux from C rich soils and surface waters can be limited by surface exchange processes. The comparison of the CO 2 and CH 4 emission in an anaerobic soil incubation experiment showed that in this ecosystem, CO 2 production is an order of magnitude higher than CH 4 production. Future increases in surface water ponding, linked to surface subsidence and thermokarst erosion, and concomitant increases in soil warming, can increase net C efflux from these arctic ecosystems. Article in Journal/Newspaper Arctic Climate change Thermokarst Tundra The Open University: Open Research Online (ORO) Arctic Global Biogeochemical Cycles 26 2 n/a n/a
institution Open Polar
collection The Open University: Open Research Online (ORO)
op_collection_id ftopenunivgb
language unknown
description Tundra ecosystems are especially sensitive to climate change, which is particularly rapid in high northern latitudes resulting in significant alterations in temperature and soil moisture. Numerous studies have demonstrated that soil drying increases the respiration loss from wet Arctic tundra. And, warming and drying of tundra soils are assumed to increase CO 2 emissions from the Arctic. However, in this water table manipulation experiment (i.e., flooding experiment), we show that flooding of wet tundra can also lead to increased CO 2 loss. Standing water increased heat conduction into the soil, leading to higher soil temperature, deeper thaw and, surprisingly, to higher CO 2 loss in the most anaerobic of the experimental areas. The study site is located in a drained lake basin, and the soils are characterized by wetter conditions than upland tundra. In experimentally flooded areas, high wind speeds (greater than ~4 m s −1 ) increased CO 2 emission rates, sometimes overwhelming the photosynthetic uptake, even during daytime. This suggests that CO 2 efflux from C rich soils and surface waters can be limited by surface exchange processes. The comparison of the CO 2 and CH 4 emission in an anaerobic soil incubation experiment showed that in this ecosystem, CO 2 production is an order of magnitude higher than CH 4 production. Future increases in surface water ponding, linked to surface subsidence and thermokarst erosion, and concomitant increases in soil warming, can increase net C efflux from these arctic ecosystems.
format Article in Journal/Newspaper
author Zona, Donatella
Lipson, David A.
Paw U, Kyaw T.
Oberbauer, Steve F.
Olivas, Paulo
Gioli, Beniamino
Oechel, Walter C.
spellingShingle Zona, Donatella
Lipson, David A.
Paw U, Kyaw T.
Oberbauer, Steve F.
Olivas, Paulo
Gioli, Beniamino
Oechel, Walter C.
Increased CO 2 loss from vegetated drained lake tundra ecosystems due to flooding
author_facet Zona, Donatella
Lipson, David A.
Paw U, Kyaw T.
Oberbauer, Steve F.
Olivas, Paulo
Gioli, Beniamino
Oechel, Walter C.
author_sort Zona, Donatella
title Increased CO 2 loss from vegetated drained lake tundra ecosystems due to flooding
title_short Increased CO 2 loss from vegetated drained lake tundra ecosystems due to flooding
title_full Increased CO 2 loss from vegetated drained lake tundra ecosystems due to flooding
title_fullStr Increased CO 2 loss from vegetated drained lake tundra ecosystems due to flooding
title_full_unstemmed Increased CO 2 loss from vegetated drained lake tundra ecosystems due to flooding
title_sort increased co 2 loss from vegetated drained lake tundra ecosystems due to flooding
publishDate 2012
url https://oro.open.ac.uk/38776/
https://oro.open.ac.uk/38776/1/oechel%201.pdf
https://doi.org/10.1029/2011GB004037
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Thermokarst
Tundra
genre_facet Arctic
Climate change
Thermokarst
Tundra
op_relation https://oro.open.ac.uk/38776/1/oechel%201.pdf
Zona, Donatella; Lipson, David A.; Paw U, Kyaw T.; Oberbauer, Steve F.; Olivas, Paulo; Gioli, Beniamino and Oechel, Walter C. <http://oro.open.ac.uk/view/person/wco5.html> (2012). Increased CO2 loss from vegetated drained lake tundra ecosystems due to flooding. Global Biogeochemical Cycles, 26(2), article no. GB2004.
op_doi https://doi.org/10.1029/2011GB004037
container_title Global Biogeochemical Cycles
container_volume 26
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