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作 者:Claire M.WRIGHT Amy C.BLASER Paul M.TREITZ Neal A.SCOTT
机构地区:[1]Department of Geography and Planning,Queen’s University,Kingston,Ontario,Canada,K7L 3N6
出 处:《Advances in Polar Science》2021年第1期1-19,共19页极地科学进展(英文版)
基 金:ArcticNet NCE,the Natural Sciences and Engineering Research Council,Natural Resources Canada(Polar Continental Shelf Program);the Northern Scientific Training Program,and Queen’s University。
摘 要:Wet sedge meadows are the most productive plant communities in the High Arctic.However,the controls on carbon dioxide(CO_(2))exchange processes within wet sedge communities-and the scale at which they operate-are poorly understood.Here,the factors controlling CO_(2)exchange of wet sedge meadows experiencing different moisture regimes are examined.Environmental data are used to create predictive models of CO_(2)exchange on multiple temporal scales.Automated chamber systems recorded CO_(2)fluxes at 30-minute intervals at wet sedge sites in the Canadian High Arctic from June to August in 2014 and 2015.Static chambers were also deployed over a larger spatial extent in 2014.Our results show that wet sedge communities were strong CO_(2)sinks during the growing season(−7.67 to−44.36 g C·m^(−2)).CO_(2)exchange rates in wetter and drier areas within wet sedge meadows differed significantly(Wilcoxon,p<0.001),suggesting that soil moisture regimes within vegetation types influence net CO_(2)balance.Random Forest models explained a significant amount of the variability in CO_(2)flux rates over time(R2=0.46 to 0.90).The models showed that the drivers of CO_(2)exchange in these communities vary temporally.Variable moisture regimes indirectly influenced CO_(2)fluxes given that they exhibit different vegetation and temperature-response characteristics.We suggest that the response of a single vegetation type to environmental changes may vary depending on microenvironment variability within that community.
关 键 词:High Arctic carbon dioxide exchange wet sedge soil moisture
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