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Peatland Heterogeneity Impacts on Regional Carbon Flux and Its Radiative Effect Within a Boreal Landscape

Kou, Dan ; Virtanen, Tarmo ; Treat, Claire C. ; Tuovinen, Juha Pekka ; Räsänen, Aleksi ; Juutinen, Sari ; Mikola, Juha ; Aurela, Mika ; Heiskanen, Lauri and Heikkilä, Maija , et al. (2022) In Journal of Geophysical Research: Biogeosciences 127(9).
Abstract

Peatlands, with high spatial variability in ecotypes and microforms, constitute a significant part of the boreal landscape and play an important role in the global carbon (C) cycle. However, the effects of this peatland heterogeneity within the boreal landscape are rarely quantified. Here, we use field-based measurements, high-resolution land cover classification, and biogeochemical and atmospheric models to estimate the atmosphere-ecosystem C fluxes and the corresponding radiative effect (RE) for a boreal landscape (Kaamanen) in northern Finland. Our result shows that the Kaamanen catchment currently functioned as a sink of carbon dioxide (CO2) and a source of methane (CH4). Peatlands (26% of the area) contributed... (More)

Peatlands, with high spatial variability in ecotypes and microforms, constitute a significant part of the boreal landscape and play an important role in the global carbon (C) cycle. However, the effects of this peatland heterogeneity within the boreal landscape are rarely quantified. Here, we use field-based measurements, high-resolution land cover classification, and biogeochemical and atmospheric models to estimate the atmosphere-ecosystem C fluxes and the corresponding radiative effect (RE) for a boreal landscape (Kaamanen) in northern Finland. Our result shows that the Kaamanen catchment currently functioned as a sink of carbon dioxide (CO2) and a source of methane (CH4). Peatlands (26% of the area) contributed 22% of the total CO2 uptake and 89% of CH4 emissions; forests (61%) accounted for 78% of CO2 uptake and offset 6% of CH4 emissions; water bodies (13%) offset 7% of CO2 uptake and contributed 11% of CH4 emissions. The heterogeneity of peatlands accounted for 11%, 88%, and 75% of the area-weighted variability (deviation from the area-weighted mean among different land cover types (LCTs) within the catchment) in CO2 flux, CH4 flux, and the combined RE of CO2 and CH4 exchanges over the 25-year time horizon, respectively. Aggregating peatland LCTs or misclassifying them as nonpeatland LCTs can significantly (p < 0.05) bias the regional CH4 exchange and RE estimates, while differentiating between drier noninundated and wetter inundated peatlands can effectively reduce the bias. Current land cover products lack such details in peatland heterogeneity, which would be needed to better constrain boreal C budgets and global C-climate feedbacks.

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@article{dafb5236-7e81-489b-8eed-6f08a3a999fa,
  abstract     = {{<p>Peatlands, with high spatial variability in ecotypes and microforms, constitute a significant part of the boreal landscape and play an important role in the global carbon (C) cycle. However, the effects of this peatland heterogeneity within the boreal landscape are rarely quantified. Here, we use field-based measurements, high-resolution land cover classification, and biogeochemical and atmospheric models to estimate the atmosphere-ecosystem C fluxes and the corresponding radiative effect (RE) for a boreal landscape (Kaamanen) in northern Finland. Our result shows that the Kaamanen catchment currently functioned as a sink of carbon dioxide (CO<sub>2</sub>) and a source of methane (CH<sub>4</sub>). Peatlands (26% of the area) contributed 22% of the total CO<sub>2</sub> uptake and 89% of CH<sub>4</sub> emissions; forests (61%) accounted for 78% of CO<sub>2</sub> uptake and offset 6% of CH<sub>4</sub> emissions; water bodies (13%) offset 7% of CO<sub>2</sub> uptake and contributed 11% of CH<sub>4</sub> emissions. The heterogeneity of peatlands accounted for 11%, 88%, and 75% of the area-weighted variability (deviation from the area-weighted mean among different land cover types (LCTs) within the catchment) in CO<sub>2</sub> flux, CH<sub>4</sub> flux, and the combined RE of CO<sub>2</sub> and CH<sub>4</sub> exchanges over the 25-year time horizon, respectively. Aggregating peatland LCTs or misclassifying them as nonpeatland LCTs can significantly (p &lt; 0.05) bias the regional CH<sub>4</sub> exchange and RE estimates, while differentiating between drier noninundated and wetter inundated peatlands can effectively reduce the bias. Current land cover products lack such details in peatland heterogeneity, which would be needed to better constrain boreal C budgets and global C-climate feedbacks.</p>}},
  author       = {{Kou, Dan and Virtanen, Tarmo and Treat, Claire C. and Tuovinen, Juha Pekka and Räsänen, Aleksi and Juutinen, Sari and Mikola, Juha and Aurela, Mika and Heiskanen, Lauri and Heikkilä, Maija and Weckström, Jan and Juselius, Teemu and Piilo, Sanna R. and Deng, Jia and Zhang, Yu and Chaudhary, Nitin and Huang, Conghong and Väliranta, Minna and Biasi, Christina and Liu, Xiangyu and Guo, Mingyang and Zhuang, Qianlai and Korhola, Atte and Shurpali, Narasinha J.}},
  issn         = {{2169-8953}},
  keywords     = {{boreal; carbon; heterogeneity; landscape; peatland; radiative effect}},
  language     = {{eng}},
  number       = {{9}},
  publisher    = {{Wiley}},
  series       = {{Journal of Geophysical Research: Biogeosciences}},
  title        = {{Peatland Heterogeneity Impacts on Regional Carbon Flux and Its Radiative Effect Within a Boreal Landscape}},
  url          = {{http://dx.doi.org/10.1029/2021JG006774}},
  doi          = {{10.1029/2021JG006774}},
  volume       = {{127}},
  year         = {{2022}},
}