Improving the Representation of Soluble Iron in Climate Models
- Columbia Univ., New York, NY (United States)
Mineral dust produced in the arid and semi-arid regions of the world is the dominant source of iron (Fe) in atmospheric aerosol inputs to the open ocean. The bioavailable Fe fraction of atmospheric dust is thought to regulate and occasionally limit the primary productivity in large oceanic regions, which influences the CO2 uptake from the atmosphere affecting the Earth’s climate. Because Fe bioavailability cannot be directly measured, it is assumed that the dissolved Fe or highly reactive Fe in the dust is bioavailable. The fraction of soluble Fe in dust is mainly controlled by: (1) the mineral composition of the soils and the emitted dust from the source areas; (2) the atmospheric processing that converts the Fe in Fe-bearing minerals into highly soluble forms of Fe. The project has mainly focused on constraining the mineral composition of dust aerosols (1), a previously neglected, yet a key issue to constrain the deposition of soluble iron. Deriving aerosol mineral composition requires global knowledge of the soil mineral content, which is available from poorly constrained global atlases. In addition, the mineral content of the emitted aerosol differs from that of the parent soil. Measurements of soil mineral fractions are based upon wet sedimentation (or ’wet sieving’) techniques that disturb the soil sample, breaking aggregates that are found in the original, undispersed soil that is subject to wind erosion. Wet sieving alters the soil size distribution, replacing aggregates that are potentially mobilized as aerosols with a collection of smaller particles. A major challenge is to derive the size-distributed mineral fractions of the emitted dust based upon their fractions measured from wet-sieved soils. Finally, representations of dust mineral composition need to account for mixtures of minerals. Examination of individual particles shows that iron, an element that is central to many climate processes, is often found as trace impurities of iron oxide attached to aggregates of other minerals. This is another challenge that has been tackled by the project. The project has produced a major step forward on our understanding of the key processes needed to predict the mineral composition of dust aerosols by connecting theory, modeling and observations. The project has produced novel semi-empirical and theoretical methods to estimate the emitted size distribution and mineral composition of dust aerosols. These methods account for soil aggregates that are potentially emitted from the original undisturbed soil but are destroyed during wet sieving. The methods construct the emitted size distribution of individual minerals building upon brittle fragmentation theory, reconstructions of wet-sieved soil mineral size distributions, and/or characteristic mineral size distributions estimated from observations at times of high concentration. Based on an unprecedented evaluation with a new global compilation of observations produced with the project support, we showed that the new methods remedy some key deficiencies compared to the previous state-of-the-art. This includes the correct representation of Fe-bearing phyllosilicates at silt sizes, where they are abundant according to observations. In addition, the quartz fraction of silt particles is in better agreement with measured values. In addition, we represent an additional class of iron oxide aerosol that is a small impurity embedded within other minerals, allowing it to travel farther than in its pure crystalline state. We assume that these impurities are least frequent in soils rich in iron oxides (as a result of the assumed effect of weathering that creates pure iron oxide crystals). The mineral composition of dust is also important to other interaction with climate - through shortwave absorption and radiative forcing, nucleation of cloud droplets and ice crystals, and the heterogeneous formation of sulfates and nitrates - and to its impacts upon human health. Despite the importance of mineral composition, models have typically assumed that soil dust aerosols have globally uniform composition. The results of this project will allow an improved estimation of the dust effects upon climate and health.
- Research Organization:
- The Trustees of Columbia University, New York, NY (United States)
- Sponsoring Organization:
- USDOE Office of Science (SC), Biological and Environmental Research (BER)
- DOE Contract Number:
- SC0006713
- OSTI ID:
- 1241294
- Report Number(s):
- DOE-COLU-06713-1
- Resource Relation:
- Related Information: Peer reviewed publications:1. Perlwitz, J. P.*, C. Perez Garcia-Pando*, and R. L. Miller*, 2015: Predicting the mineral composition of dust aerosols - Part 1: Representing key processes. Atmos. Chem. Phys., 15, 11593-11627, doi:10.5194/acp-15-11593-2015. (*Equal contribution) 2. Perlwitz, J. P., C. Perez Garcia-Pando, and R.L. Miller, 2015: Predicting the mineral composition of dust aerosols - Part 2: Model evaluation and identification of key processes with observations. Atmos. Chem. Phys., 15, 11629-11652, doi:10.5194/acp-15-11629-2015.3. Miller, R.L., et al, 2014: CMIP5 historical simulations (1850-2012) with GISS ModelE2. J. Adv. Model. Earth Syst., 6, no. 2, 441-477, doi:10.1002/2013MS000266.4. Perez Garcia-Pando, C., M. Stanton, P. Diggle, S. Trzaska, R.L. Miller, J.P. Perlwitz, J.M. Baldasano, E. Cuevas, P. Ceccato, P. Yaka, and M. Thomson, 2014: Soil dust aerosols and wind as predictors of seasonal meningitis incidence in Niger. Environ. Health Perspect., 122, no. 7, 679-686, doi:10.1289/ehp.1306640.5. Hickman, J.E., R.J. Scholes, T.S. Rosenstock, C. Perez Garcia-Pando, and J. Nyamangara, 2014: Assessing non-CO2 climate-forcing emissions and mitigation in sub-Saharan Africa. Curr. Opin. Environ. Sustain., 9-10, 65-72, doi:10.1016/j.cosust.2014.07.010.6. Schulz, M., J.M. Prospero, A.R. Baker, F. Dentener, L. Ickes, P.S. Liss, N.M. Mahowald, S. Nickovic, C. Perez, S. Rodríguez, M. Manmohan Sarin, I. Tegen, and R.A. Duce, 2012: The atmospheric transport and deposition of mineral dust to the ocean: Implications for research needs. Environ. Sci. Technol., 46, 10390-10404, doi:10.1021/es300073u.Book Chapters1. Miller, R.L., P. Knippertz, C. Perez Garcia-Pando, J.P. Perlwitz, and I. Tegen, 2014: Impact of dust radiative forcing upon climate. In Mineral Dust: A Key Player in the Earth System. P. Knippertz, and J.-B.W. Stuut, Eds. Springer, 327-357, doi:10.1007/978-94-017-8978-3_13.Datasets:We have made dataset available at http://data.giss.nasa.gov/mineralfrac/The global compilation of observations is also available in the Supporting Information of Perlwitz et al. (2015b).
- Country of Publication:
- United States
- Language:
- English
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