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Variability in Trends and Indicators of CO 2 Exchange Across Arctic Wetlands
Author(s) -
Coffer Megan M.,
Hestir Erin L.
Publication year - 2019
Publication title -
journal of geophysical research: biogeosciences
Language(s) - English
Resource type - Journals
eISSN - 2169-8961
pISSN - 2169-8953
DOI - 10.1029/2018jg004775
Subject(s) - environmental science , wetland , primary production , carbon sink , evapotranspiration , ecosystem respiration , arctic , sink (geography) , climate change , ecosystem , carbon cycle , atmospheric sciences , precipitation , climatology , ecology , geography , meteorology , cartography , geology , biology
Arctic wetlands store nearly half of the world's soil organic carbon and are crucial to the global carbon cycle. However, most Earth system models fail to account for wetlands given heterogeneity and uncertainty surrounding the response of different wetland types to climate change. We analyzed summer (June–August) carbon dioxide (CO 2 ) exchange, meteorological conditions, and ecological conditions at four Arctic wetlands. Micrometeorological flux tower data were used to assess CO 2 exchange and meteorological conditions across 7 to 9 years of data. Climate data were used to assess meteorological conditions across 30 years of data. Satellite data described ecological conditions. Each site acted as a CO 2 sink, but strength varied, ranging from −49 to −93 g C/m 2 per summer. A trend analysis was used to investigate how CO 2 balance and surrounding conditions may have changed. CO 2 exchange significantly changed at one site, becoming a stronger sink. Changes in meteorological conditions were variable across sites with the exception of air temperature which, when considering significant trends, unanimously increased across sites. Ecological conditions suggested increased vegetation cover regardless of statistical significance at all sites. A conditional random forest algorithm was used to evaluate drivers of CO 2 exchange. Cumulative precipitation and evapotranspiration were the main drivers of net ecosystem exchange and gross primary productivity, while ecosystem respiration was primarily driven by air temperature, suggesting that projected changes in temperature and precipitation patterns will influence the carbon balance of Arctic wetlands. Variability across sites emphasizes the need for long‐term observations across wetland types and climatic gradients.