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

• Published in: Global change biology Vol. 30; no. 1; pp. e17087 - n/a
• Main Authors: Hermesdorf, Lena, Liu, Yijing, Michelsen, Anders, Westergaard‐Nielsen, Andreas, Mortensen, Louise Hindborg, Jepsen, Malte Skov, Sigsgaard, Charlotte, Elberling, Bo
• Format: Journal Article
• Language: English
• Published: England Blackwell Publishing Ltd 01.01.2024
• Subjects: Air temperature; Arctic Regions; Carbon dioxide; Carbon Dioxide - chemistry; Carbon dioxide exchange; climate change; CO2; Daytime; Ecosystem; ecosystem respiration; Ecosystems; Factorial design; Greenland; gross ecosystem photosynthesis; Growing season; NDVI; net ecosystem exchange; Normalized difference vegetative index; Photosynthesis; Precipitation; Seasons; Snow; Snow accumulation; Snow cover; Snow depth; Soil - chemistry; Summer; Taiga & tundra; Temperature; Tundra; Vegetation index; warming; Winter; Winter precipitation; Arctic Regions; net ecosystem exchange; ecosystem respiration; gross ecosystem photosynthesis; snow; CO2; warming; NDVI; Greenland; climate change
• DOI: 10.1111/gcb.17087
• ISSN: 1354-1013

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. We investigated the short‐term and long‐term effects of increased snow depth (snow fences) and warming (open top chambers) and their combination in a factorial design on all key components of the daytime carbon dioxide (CO2) in an arctic, well‐drained tundra ecosystem. Overall, the study highlights the complexity of a faster response from respiration processes, and a slower and complex plant response.