Daniel Liptzin
Spatial and Temporal Patterns in Atmospheric Deposition of Dissolved Organic Carbon
Liptzin, Daniel; Boy, Jens; Campbell, John L.; Clarke, Nicholas; Laclau, Jean‐Paul; Godoy, Roberto; Johnson, Sherri L.; Kaiser, Klaus; Likens, Gene E.; Karlsson, Gunilla Pihl; Markewitz, Daniel; Rogora, Michela; Sebestyen, Stephen D.; Shanley, James B.; Vanguelova, Elena; Verstraeten, Arne; Wilcke, Wolfgang; Worrall, Fred; McDowell, William H.
Authors
Jens Boy
John L. Campbell
Nicholas Clarke
Jean‐Paul Laclau
Roberto Godoy
Sherri L. Johnson
Klaus Kaiser
Gene E. Likens
Gunilla Pihl Karlsson
Daniel Markewitz
Michela Rogora
Stephen D. Sebestyen
James B. Shanley
Elena Vanguelova
Arne Verstraeten
Wolfgang Wilcke
Professor Fred Worrall fred.worrall@durham.ac.uk
Professor
William H. McDowell
Abstract
Atmospheric deposition of dissolved organic carbon (DOC) to terrestrial ecosystems is a small, but rarely studied component of the global carbon (C) cycle. Emissions of volatile organic compounds (VOC) and organic particulates are the sources of atmospheric C and deposition represents a major pathway for the removal of organic C from the atmosphere. Here, we evaluate the spatial and temporal patterns of DOC deposition using 70 data sets at least one year in length ranging from 40° south to 66° north latitude. Globally, the median DOC concentration in bulk deposition was 1.7 mg L−1. The DOC concentrations were significantly higher in tropical (<25°) latitudes compared to temperate (>25°) latitudes. DOC deposition was significantly higher in the tropics because of both higher DOC concentrations and precipitation. Using the global median or latitudinal specific DOC concentrations leads to a calculated global deposition of 202 or 295 Tg C yr−1 respectively. Many sites exhibited seasonal variability in DOC concentration. At temperate sites, DOC concentrations were higher during the growing season; at tropical sites, DOC concentrations were higher during the dry season. Thirteen of the thirty-four long-term (>10 years) data sets showed significant declines in DOC concentration over time with the others showing no significant change. Based on the magnitude and timing of the various sources of organic C to the atmosphere, biogenic VOCs likely explain the latitudinal pattern and the seasonal pattern at temperate latitudes while decreases in anthropogenic emissions are the most likely explanation for the declines in DOC concentration.
Citation
Liptzin, D., Boy, J., Campbell, J. L., Clarke, N., Laclau, J., Godoy, R., …McDowell, W. H. (2022). Spatial and Temporal Patterns in Atmospheric Deposition of Dissolved Organic Carbon. Global Biogeochemical Cycles, 36(10), https://doi.org/10.1029/2022gb007393
Journal Article Type | Article |
---|---|
Acceptance Date | Oct 11, 2022 |
Online Publication Date | Oct 17, 2022 |
Publication Date | 2022 |
Deposit Date | Feb 6, 2023 |
Publicly Available Date | Feb 6, 2023 |
Journal | Global Biogeochemical Cycles |
Print ISSN | 0886-6236 |
Electronic ISSN | 1944-9224 |
Publisher | American Geophysical Union |
Peer Reviewed | Peer Reviewed |
Volume | 36 |
Issue | 10 |
DOI | https://doi.org/10.1029/2022gb007393 |
Public URL | https://durham-repository.worktribe.com/output/1179917 |
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Copyright Statement
This is an open access article under the terms of the Creative Commons Attribution-NonCommercial License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes.
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