Articles | Volume 15, issue 11
https://doi.org/10.5194/acp-15-6247-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-6247-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Sources, transport and deposition of iron in the global atmosphere
Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China
Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University, Beijing, China
Laboratoire des Sciences du Climat et de l'Environnement, CEA CNRS UVSQ, Gif-sur-Yvette, France
Y. Balkanski
Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China
Laboratoire des Sciences du Climat et de l'Environnement, CEA CNRS UVSQ, Gif-sur-Yvette, France
O. Boucher
Laboratoire de Météorologie Dynamique, IPSL/CNRS, Université Pierre et Marie Curie, Paris, France
Laboratoire des Sciences du Climat et de l'Environnement, CEA CNRS UVSQ, Gif-sur-Yvette, France
A. Chappell
CSIRO Land & Water National Research Flagship, G.P.O. Box 1666, Canberra, ACT 2601, Australia
Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China
Laboratoire des Sciences du Climat et de l'Environnement, CEA CNRS UVSQ, Gif-sur-Yvette, France
D. Hauglustaine
Laboratoire des Sciences du Climat et de l'Environnement, CEA CNRS UVSQ, Gif-sur-Yvette, France
J. Peñuelas
CSIC, Global Ecology Unit CREAF-CEAB-UAB, Cerdanyola del Vallès, 08193 Catalonia, Spain
CREAF, Cerdanyola del Vallès, 08193 Catalonia, Spain
S. Tao
Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China
Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University, Beijing, China
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- Up in Smoke: Most Aerosolized Fe From Biomass Burning Does Not Derive From Foliage L. Tegler et al. 10.1029/2023GB007796
- Climate engineering by mimicking natural dust climate control: the iron salt aerosol method F. Oeste et al. 10.5194/esd-8-1-2017
- Improved methodologies for Earth system modelling of atmospheric soluble iron and observation comparisons using the Mechanism of Intermediate complexity for Modelling Iron (MIMI v1.0) D. Hamilton et al. 10.5194/gmd-12-3835-2019
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- What Controls Springtime Fine Dust Variability in the Western United States? Investigating the 2002–2015 Increase in Fine Dust in the U.S. Southwest P. Achakulwisut et al. 10.1002/2017JD027208
- Perspective on identifying and characterizing the processes controlling iron speciation and residence time at the atmosphere-ocean interface N. Meskhidze et al. 10.1016/j.marchem.2019.103704
- Emission of primary microplastics in mainland China: Invisible but not negligible T. Wang et al. 10.1016/j.watres.2019.06.042
- Magnetic mineral constraint on lead isotope variations of coal fly ash and its implications for source discrimination Z. Zhu et al. 10.1016/j.scitotenv.2019.136320
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- Atmospheric Wet Iron, Molybdenum, and Vanadium Deposition in Chinese Terrestrial Ecosystems Y. Chen et al. 10.1021/acs.est.2c03213
- Pre‐Industrial, Present and Future Atmospheric Soluble Iron Deposition and the Role of Aerosol Acidity and Oxalate Under CMIP6 Emissions E. Bergas‐Massó et al. 10.1029/2022EF003353
- Chemical analysis of trace metal contamination in the air of industrial area of Gajraula (U.P), India A. Kumar et al. 10.1016/j.jksus.2019.10.008
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Saved (final revised paper)
Saved (final revised paper)
Saved (preprint)
Latest update: 13 Dec 2024
Short summary
This study makes a first attempt to estimate the temporal trend of Fe emissions from anthropogenic and natural combustion sources from 1960 to 2007 and the emissions of Fe from mineral dust based on a recent mineralogical database. The new emission inventory is introduced into a global aerosol model. The simulated total Fe and soluble Fe concentrations in surface air as well as the deposition of total Fe are evaluated by observations over major continental and oceanic regions globally.
This study makes a first attempt to estimate the temporal trend of Fe emissions from...
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Final-revised paper
Preprint