Spatial and Temporal Patterns in Atmospheric Deposition of Dissolved Organic Carbon

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.

[1]  W. McDowell,et al.  Nitrogen wet deposition stoichiometry: the role of organic nitrogen, seasonality, and snow , 2022, Biogeochemistry.

[2]  G. González,et al.  African dust deposition in Puerto Rico: Analysis of a 20-year rainfall chemistry record and comparison with models , 2019, Atmospheric Environment.

[3]  J. D. Hanwell.  Atmospheric Processes , 2019 .

[4]  G. Likens,et al.  Nitrogen oligotrophication in northern hardwood forests , 2018, Biogeochemistry.

[5]  C. Heald,et al.  A Global Assessment of Dissolved Organic Carbon in Precipitation , 2017 .

[6]  Matthew P. Miller,et al.  Variability of dissolved organic carbon in precipitation during storms at the Shale Hills Critical Zone Observatory , 2017 .

[7]  E. Boyer,et al.  Atmospheric deposition of organic carbon via precipitation , 2016 .

[8]  P. Raymond,et al.  Spatial Variation in the Origin of Dissolved Organic Carbon in Snow on the Juneau Icefield, Southeast Alaska. , 2015, Environmental science & technology.

[9]  K. Bishop,et al.  Organic Matter in Rain : An Overlooked Influence on Mercury Deposition , 2015 .

[10]  Renjian Zhang,et al.  Significant influence of fungi on coarse carbonaceous and potassium aerosols in a tropical rainforest , 2015 .

[11]  Wolfgang Knorr,et al.  Global data set of biogenic VOC emissions calculated by the MEGAN model over the last 30 years , 2014 .

[12]  J. Neirynck,et al.  Impact of air-borne or canopy-derived dissolved organic carbon (DOC) on forest soil solution DOC in Flanders, Belgium , 2014 .

[13]  A. Ballantyne,et al.  Increasing Ca2+ deposition in the western US: The role of mineral aerosols , 2013 .

[14]  Julia A. Jones,et al.  Trends in cation, nitrogen, sulfate and hydrogen ion concentrations in precipitation in the United States and Europe from 1978 to 2010: a new look at an old problem , 2013, Biogeochemistry.

[15]  J. Randerson,et al.  Global burned area and biomass burning emissions from small fires , 2012 .

[16]  N. Mahowald,et al.  Atmospheric fluxes of organic N and P to the global ocean , 2012 .

[17]  T. Burt,et al.  The multi-annual nitrogen budget of a peat-covered catchment--changing from sink to source? , 2012, The Science of the total environment.

[18]  S. Martin,et al.  Biogenic Potassium Salt Particles as Seeds for Secondary Organic Aerosol in the Amazon , 2012, Science.

[19]  S. K. Schmidt,et al.  Atmospheric deposition as a source of carbon and nutrients to an alpine catchment of the Colorado Rocky Mountains , 2012 .

[20]  A. Marchetto,et al.  The role of forest type in the variability of DOC in atmospheric deposition at forest plots in Italy , 2012, Environmental Monitoring and Assessment.

[21]  R. Jaenicke,et al.  Primary biological aerosol particles in the atmosphere: a review , 2012 .

[22]  S. Ghan,et al.  Global Distribution and Climate Forcing of Marine Organic Aerosol: 1. Model Improvements and Evaluation , 2011 .

[23]  W. McDowell,et al.  Long‐term patterns and short‐term dynamics of stream solutes and suspended sediment in a rapidly weathering tropical watershed , 2011 .

[24]  J. Randerson,et al.  Global fire emissions and the contribution of deforestation, savanna, forest, agricultural, and peat fires (1997-2009) , 2010 .

[25]  S. K. Akagi,et al.  Emission factors for open and domestic biomass burning for use in atmospheric models , 2010 .

[26]  Yuesi Wang,et al.  Study on dissolved organic carbon in precipitation in Northern China. , 2010 .

[27]  A. Moffat,et al.  Chemical fluxes in time through forest ecosystems in the UK - soil response to pollution recovery. , 2010, Environmental pollution.

[28]  J. Kirchner,et al.  Concentration–discharge relationships reflect chemostatic characteristics of US catchments , 2009 .

[29]  W. Wilcke,et al.  Amazonian biomass burning‐derived acid and nutrient deposition in the north Andean montane forest of Ecuador , 2008 .

[30]  C. Duarte,et al.  Atmospheric deposition of organic and black carbon to the global oceans , 2008 .

[31]  R. Nogueira,et al.  Dissolved organic carbon in rainwater from areas heavily impacted by sugar cane burning , 2008 .

[32]  A. Guenther,et al.  The tropical forest and fire emissions experiment: laboratory fire measurements and synthesis of campaign data , 2008 .

[33]  M. Andreae,et al.  Contribution of fungi to primary biogenic aerosols in the atmosphere: wet and dry discharged spores, carbohydrates, and inorganic ions , 2007 .

[34]  A. Goldstein,et al.  Known and Unexplored Organic Constituents in the Earth's Atmosphere , 2007 .

[35]  J. Willey,et al.  Carbon isotopic characterization of dissolved organic carbon in rainwater: Terrestrial and marine influences , 2006 .

[36]  J. Willey,et al.  Changing chemical composition of precipitation in Wilmington, North Carolina, U.S.A.: implications for the Continental U.S.A. , 2006, Environmental science & technology.

[37]  E. Davidson,et al.  Dissolved rainfall inputs and streamwater outputs in an undisturbed watershed on highly weathered soils in the Brazilian cerrado , 2006 .

[38]  G. Guggenberger,et al.  Dissolved organic carbon and nitrogen in precipitation, throughfall, soil solution, and stream water of the tropical highlands in northern Thailand , 2005 .

[39]  P. Raymond.  The composition and transport of organic carbon in rainfall: Insights from the natural (13C and 14C) isotopes of carbon , 2005 .

[40]  J. Lamarque,et al.  Tropospheric ozone evolution between 1890 and 1990 , 2005 .

[41]  L. Barrie,et al.  Temporal and spatial variabilities of atmospheric polychlorinated biphenyls (PCBs), organochlorine (OC) pesticides and polycyclic aromatic hydrocarbons (PAHs) in the Canadian Arctic: results from a decade of monitoring. , 2005, The Science of the total environment.

[42]  N. Mahowald,et al.  Global Iron Connections Between Desert Dust, Ocean Biogeochemistry, and Climate , 2005, Science.

[43]  R. Jaenicke.  Abundance of Cellular Material and Proteins in the Atmosphere , 2005, Science.

[44]  Yang Yu-sheng,et al.  Dissolved organic carbon and nitrogen in precipitation, throughfall and stemflow fromSchima superba andCunninghamia lanceolata plantations in subtropical China , 2005, Journal of Forestry Research.

[45]  T. Eck,et al.  A review of biomass burning emissions part III: intensive optical properties of biomass burning particles , 2004 .

[46]  Eric A. Davidson,et al.  NUTRIENT LOSS AND REDISTRIBUTION AFTER FOREST CLEARING ON A HIGHLY WEATHERED SOIL IN AMAZONIA , 2004 .

[47]  Gregory S. Okin,et al.  Impact of desert dust on the biogeochemistry of phosphorus in terrestrial ecosystems , 2004 .

[48]  W. Wilcke,et al.  Water and element input into native, agri- and silvicultural ecosystems of the Brazilian savanna , 2004 .

[49]  S. Lindow,et al.  Microbiology of the Phyllosphere , 2003, Applied and Environmental Microbiology.

[50]  J. Laclau,et al.  Nutrient cycling in a clonal stand of Eucalyptus and an adjacent savanna ecosystem in Congo : 1. Chemical composition of rainfall, throughfall and stemflow solutions , 2003 .

[51]  Chiung-Pin Liu,et al.  Dissolved organic carbon in precipitation, throughfall, stemflow, soil solution, and stream water at the Guandaushi subtropical forest in Taiwan , 2003 .

[52]  G. B. Avery,et al.  Dissolved organic carbon and organic acids in coastal New Zealand rainwater , 2002 .

[53]  M. Andreae,et al.  Emission of trace gases and aerosols from biomass burning , 2001 .

[54]  W. McDowell,et al.  Dissolved organic nitrogen budgets for upland, forested ecosystems in New England , 2000 .

[55]  J. Willey,et al.  Rainwater dissolved organic carbon: Concentrations and global flux , 2000 .

[56]  H. L. Allen,et al.  Three decades of observed soil acidification in the Calhoun Experimental Forest: Has acid rain made a difference? , 1998 .

[57]  W. McDowell,et al.  Seasonal variation of tropical precipitation chemistry: La Selva, Costa Rica , 1997 .

[58]  C. N. Hewitt,et al.  A global model of natural volatile organic compound emissions , 1995 .

[59]  I. Fung,et al.  Modeling of mineral dust in the atmosphere: Sources, transport, and optical thickness , 1994 .

[60]  Andrew G. Dickson,et al.  Handbook of methods for the analysis of the various parameters of the carbon dioxide system in sea water. Version 2 , 1994 .

[61]  Stephen D. Piccot,et al.  A global inventory of volatile organic compound emissions from anthropogenic sources , 1992 .

[62]  N. Peters,et al.  Use of multivariate analysis for determining sources of solutes found in wet atmospheric deposition in the United States , 1989 .

[63]  R. Harriss,et al.  Formic and acetic acid over the central Amazon region, Brazil: 1. Dry season , 1988 .

[64]  W. McDowell,et al.  Origin, Composition, and Flux of Dissolved Organic Carbon in the Hubbard Brook Valley , 1988 .

[65]  G. Likens,et al.  Chemistry of precipitation from a remote, terrestrial site in Australia , 1987 .

[66]  G. Likens,et al.  The composition of precipitation in remote areas of the world , 1982 .

[67]  J. Mulder,et al.  Dissolved Organic Carbon Concentrations in Throughfall and Soil Waters at Level II Monitoring Plots in Norway: Short- and Long-Term Variations , 2010 .

[68]  W. Wilcke,et al.  Water and element input into native, agri- and silvicultural ecosystems of the Brazilian savanna , 2005 .

[69]  J. Galloway.  The global nitrogen cycle: changes and consequences , 1998 .

[70]  P. Paatero,et al.  Source identification of bulk wet deposition in Finland by positive matrix factorization , 1995 .

[71]  I. Beverland,et al.  On the interpretation of event and sub-event rainfall chemistry. , 1992, Environmental pollution.

[72]  W. Schlesinger.  Biogeochemistry: An Analysis of Global Change , 1991 .

[73]  P. Doskey,et al.  Atmospheric deposition of macronutrients by pollen at a semi-remote site in northern Wisconsin , 1989 .

[74]  R. Forthofer,et al.  Rank Correlation Methods , 1981 .