Environmental Research Letters (Jan 2021)

Soil respiration strongly offsets carbon uptake in Alaska and Northwest Canada

  • Jennifer D Watts,
  • Susan M Natali,
  • Christina Minions,
  • Dave Risk,
  • Kyle Arndt,
  • Donatella Zona,
  • Eugénie S Euskirchen,
  • Adrian V Rocha,
  • Oliver Sonnentag,
  • Manuel Helbig,
  • Aram Kalhori,
  • Walt Oechel,
  • Hiroki Ikawa,
  • Masahito Ueyama,
  • Rikie Suzuki,
  • Hideki Kobayashi,
  • Gerardo Celis,
  • Edward A G Schuur,
  • Elyn Humphreys,
  • Yongwon Kim,
  • Bang-Yong Lee,
  • Scott Goetz,
  • Nima Madani,
  • Luke D Schiferl,
  • Roisin Commane,
  • John S Kimball,
  • Zhihua Liu,
  • Margaret S Torn,
  • Stefano Potter,
  • Jonathan A Wang,
  • M Torre Jorgenson,
  • Jingfeng Xiao,
  • Xing Li,
  • Colin Edgar

DOI
https://doi.org/10.1088/1748-9326/ac1222
Journal volume & issue
Vol. 16, no. 8
p. 084051

Abstract

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Soil respiration (i.e. from soils and roots) provides one of the largest global fluxes of carbon dioxide (CO _2 ) to the atmosphere and is likely to increase with warming, yet the magnitude of soil respiration from rapidly thawing Arctic-boreal regions is not well understood. To address this knowledge gap, we first compiled a new CO _2 flux database for permafrost-affected tundra and boreal ecosystems in Alaska and Northwest Canada. We then used the CO _2 database, multi-sensor satellite imagery, and random forest models to assess the regional magnitude of soil respiration. The flux database includes a new Soil Respiration Station network of chamber-based fluxes, and fluxes from eddy covariance towers. Our site-level data, spanning September 2016 to August 2017, revealed that the largest soil respiration emissions occurred during the summer (June–August) and that summer fluxes were higher in boreal sites (1.87 ± 0.67 g CO _2 –C m ^−2 d ^−1 ) relative to tundra (0.94 ± 0.4 g CO _2 –C m ^−2 d ^−1 ). We also observed considerable emissions (boreal: 0.24 ± 0.2 g CO _2 –C m ^−2 d ^−1 ; tundra: 0.18 ± 0.16 g CO _2 –C m ^−2 d ^−1 ) from soils during the winter (November–March) despite frozen surface conditions. Our model estimates indicated an annual region-wide loss from soil respiration of 591 ± 120 Tg CO _2 –C during the 2016–2017 period. Summer months contributed to 58% of the regional soil respiration, winter months contributed to 15%, and the shoulder months contributed to 27%. In total, soil respiration offset 54% of annual gross primary productivity (GPP) across the study domain. We also found that in tundra environments, transitional tundra/boreal ecotones, and in landscapes recently affected by fire, soil respiration often exceeded GPP, resulting in a net annual source of CO _2 to the atmosphere. As this region continues to warm, soil respiration may increasingly offset GPP, further amplifying global climate change.

Keywords