Abstract The northern permafrost region has been projected to shift from a net sink to a net source of carbon under global warming. However, estimates of the contemporary net greenhouse gas (GHG) balance and budgets of the permafrost region remain highly uncertain. Here, we construct the first comprehensive bottom‐up budgets of CO2, CH4, and N2O across the terrestrial permafrost region using databases of more than 1000 in situ flux measurements and a land cover‐based ecosystem flux upscaling approach for the period 2000–2020. Estimates indicate that the permafrost region emitted a mean annual flux of 12 (−606, 661) Tg CO2–C yr−1, 38 (22, 53) Tg CH4–C yr−1, and 0.67 (0.07, 1.3) Tg N2O–N yr−1to the atmosphere throughout the period. Thus, the region was a net source of CH4and N2O, while the CO2balance was near neutral within its large uncertainties. Undisturbed terrestrial ecosystems had a CO2sink of −340 (−836, 156) Tg CO2–C yr−1. Vertical emissions from fire disturbances and inland waters largely offset the sink in vegetated ecosystems. When including lateral fluxes for a complete GHG budget, the permafrost region was a net source of C and N, releasing 144 (−506, 826) Tg C yr−1and 3 (2, 5) Tg N yr−1. Large uncertainty ranges in these estimates point to a need for further expansion of monitoring networks, continued data synthesis efforts, and better integration of field observations, remote sensing data, and ecosystem models to constrain the contemporary net GHG budgets of the permafrost region and track their future trajectory.
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Lateral Dissolved Organic Carbon Losses Represent ∼10% of Upland Tundra Carbon Losses and Include Seasonal Permafrost Contributions
Abstract We investigated lateral dissolved organic carbon (DOC) fluxes from lower‐order streams in upland tundra underlain by permafrost to assess their contribution to carbon (C) sink or source strength. The study site, located in Healy, Alaska, is within the Panguingue Creek watershed (66 km2), where permafrost acts as a confining layer for soil pore water. We examined how seasonal hydrology affects DOC export to understand lateral C flux contributions to the site's net ecosystem C balance. Previous estimates of vertical gas exchange (net CO2uptake and release) indicated a loss of 52.5 g C m−2 yr−1and methane was estimated to lead to an additional loss of 6.4 ± 0.20 CO2‐equivalent (g CO2–C m−2 yr−1) suggesting the site is a net C source. We found that a second‐order stream exported an additional 5.0 g DOC m−2 yr−1laterally, which is approximately 10% of the vertical CO2loss, reinforcing the site's source status. Accounting for CO2, CH4, and DOC, total C losses were estimated to be 64 g C m−2 yr−1. Further, we found that shoulder seasons played a key role in C export, with the spring freshet alone accounting for 59% of total DOC flux. Seasonality also influenced DOC age, with older, permafrost‐derived DOC exported primarily during spring and fall. These findings underscore the significance of lateral pathways in permafrost C budgets and highlight DOC as a critical, seasonally variable component of C loss.
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- Award ID(s):
- 2224776
- PAR ID:
- 10665522
- Publisher / Repository:
- American Geophysical Union
- Date Published:
- Journal Name:
- Journal of Geophysical Research: Biogeosciences
- Volume:
- 130
- Issue:
- 11
- ISSN:
- 2169-8953
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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