Modeling CO 2 emissions from A rctic lakes: Model development and site‐level study

Tan, Zeli; Zhuang, Qianlai; Shurpali, Narasinha J.; Marushchak, Maija E.; Biasi, Christina; Eugster, Werner; Walter Anthony, Katey

doi:10.1002/2017MS001028

Title: Modeling CO ₂ emissions from A rctic lakes: Model development and site‐level study

Journal Article · Thu Sep 14 00:00:00 EDT 2017 · Journal of Advances in Modeling Earth Systems

DOI:https://doi.org/10.1002/2017MS001028· OSTI ID:1390343

^[1];

^[2];

^[3]; Marushchak, Maija E. ^[3];

^[3];

^[4]; Walter Anthony, Katey ^[5]

Department of Earth, Atmospheric, and Planetary Sciences Purdue University West Lafayette Indiana USA, Now at Pacific Northwest National Laboratory Richland Washington USA
Department of Earth, Atmospheric, and Planetary Sciences Purdue University West Lafayette Indiana USA, Department of Agronomy Purdue University West Lafayette Indiana USA
Department of Environmental and Biological Science University of Eastern Finland Kuopio Finland
Department of Environmental Systems Science ETH Zurich Zurich Switzerland
Water and Environmental Research Center, University of Alaska Fairbanks Fairbanks Alaska USA

Abstract Recent studies indicated that Arctic lakes play an important role in receiving, processing, and storing organic carbon exported from terrestrial ecosystems. To quantify the contribution of Arctic lakes to the global carbon cycle, we developed a one‐dimensional process‐based Arctic Lake Biogeochemistry Model (ALBM) that explicitly simulates the dynamics of organic and inorganic carbon in Arctic lakes. By realistically modeling water mixing, carbon biogeochemistry, and permafrost carbon loading, the model can reproduce the seasonal variability of CO ₂ fluxes from the study Arctic lakes. The simulated area‐weighted CO ₂ fluxes from yedoma thermokarst lakes, nonyedoma thermokarst lakes, and glacial lakes are 29.5, 13.0, and 21.4 g C m ⁻² yr ⁻¹ , respectively, close to the observed values (31.2, 17.2, and 16.5 ± 7.7 g C m ⁻² yr ⁻¹ , respectively). The simulations show that the high CO ₂ fluxes from yedoma thermokarst lakes are stimulated by the biomineralization of mobilized labile organic carbon from thawing yedoma permafrost. The simulations also imply that the relative contribution of glacial lakes to the global carbon cycle could be the largest because of their much larger surface area and high biomineralization and carbon loading. According to the model, sunlight‐induced organic carbon degradation is more important for shallow nonyedoma thermokarst lakes but its overall contribution to the global carbon cycle could be limited. Overall, the ALBM can simulate the whole‐lake carbon balance of Arctic lakes, a difficult task for field and laboratory experiments and other biogeochemistry models.

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Research Organization:: Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)

Sponsoring Organization:: USDOE Office of Science (SC), Biological and Environmental Research (BER)

Grant/Contract Number:: DE‐FG02‐08ER64599; AC05-076RL01830; FG02-08ER64599; AC02-05CH11231

OSTI ID:: 1390343

Alternate ID(s):: OSTI ID: 1390344; OSTI ID: 1413514

Report Number(s):: PNNL-SA-129018

Journal Information:: Journal of Advances in Modeling Earth Systems, Journal Name: Journal of Advances in Modeling Earth Systems Vol. 9 Journal Issue: 5; ISSN 1942-2466

Publisher:: American Geophysical Union (AGU)Copyright Statement

Country of Publication:: United States

Language:: English

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Cited by: 29 works

Citation information provided by
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