Long-term changes in the daytime growing season carbon dioxide exchange following increased temperature and snow cover in arctic tundra

© 2023 John Wiley & Sons Ltd.

Détails bibliographiques
Publié dans:Global change biology. - 1999. - 30(2024), 1 vom: 26. Jan., Seite e17087
Auteur principal: Hermesdorf, Lena (Auteur)
Autres auteurs: Liu, Yijing, Michelsen, Anders, Westergaard-Nielsen, Andreas, Mortensen, Louise Hindborg, Jepsen, Malte Skov, Sigsgaard, Charlotte, Elberling, Bo
Format: Article en ligne
Langue:English
Publié: 2024
Accès à la collection:Global change biology
Sujets:Journal Article CO2 Greenland NDVI climate change ecosystem respiration gross ecosystem photosynthesis net ecosystem exchange snow warming plus... Carbon Dioxide 142M471B3J Soil
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520 |a Increasing temperatures and winter precipitation can influence the carbon (C) exchange rates in arctic ecosystems. Feedbacks can be both positive and negative, but the net effects are unclear and expected to vary strongly across the Arctic. There is a lack of understanding of the combined effects of increased summer warming and winter precipitation on the C balance in these ecosystems. Here we assess the short-term (1-3 years) and long-term (5-8 years) effects of increased snow depth (snow fences) (on average + 70 cm) and warming (open top chambers; 1-3°C increase) and the combination in a factorial design on all key components of the daytime carbon dioxide (CO2 ) fluxes in a wide-spread heath tundra ecosystem in West Greenland. The warming treatment increased ecosystem respiration (ER) on a short- and long-term basis, while gross ecosystem photosynthesis (GEP) was only increased in the long term. Despite the difference in the timing of responses of ER and GEP to the warming treatment, the net ecosystem exchange (NEE) of CO2 was unaffected in the short term and in the long term. Although the structural equation model (SEM) indicates a direct relationship between seasonal accumulated snow depth and ER and GEP, there were no significant effects of the snow addition treatment on ER or GEP measured over the summer period. The combination of warming and snow addition turned the plots into net daytime CO2 sources during the growing season. Interestingly, despite no significant changes in air temperature during the snow-free time during the experiment, control plots as well as warming plots revealed significantly higher ER and GEP in the long term compared to the short term. This was in line with the satellite-derived time-integrated normalized difference vegetation index of the study area, suggesting that more factors than air temperature are drivers for changes in arctic tundra ecosystems 
650 4 |a Journal Article 
650 4 |a CO2 
650 4 |a Greenland 
650 4 |a NDVI 
650 4 |a climate change 
650 4 |a ecosystem respiration 
650 4 |a gross ecosystem photosynthesis 
650 4 |a net ecosystem exchange 
650 4 |a snow 
650 4 |a warming 
650 7 |a Carbon Dioxide  |2 NLM 
650 7 |a 142M471B3J  |2 NLM 
650 7 |a Soil  |2 NLM 
700 1 |a Liu, Yijing  |e verfasserin  |4 aut 
700 1 |a Michelsen, Anders  |e verfasserin  |4 aut 
700 1 |a Westergaard-Nielsen, Andreas  |e verfasserin  |4 aut 
700 1 |a Mortensen, Louise Hindborg  |e verfasserin  |4 aut 
700 1 |a Jepsen, Malte Skov  |e verfasserin  |4 aut 
700 1 |a Sigsgaard, Charlotte  |e verfasserin  |4 aut 
700 1 |a Elberling, Bo  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Global change biology  |d 1999  |g 30(2024), 1 vom: 26. Jan., Seite e17087  |w (DE-627)NLM098239996  |x 1365-2486  |7 nnas 
773 1 8 |g volume:30  |g year:2024  |g number:1  |g day:26  |g month:01  |g pages:e17087 
856 4 0 |u http://dx.doi.org/10.1111/gcb.17087  |3 Volltext 
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