I just have come back from this year's fall meeting of the American Geophysical Union (AGU) in San Francisco. The meeting was very interesting and productive (and exhausting) for me. The amount of exciting science from the whole range of geosciences, presented by many enthusiastic researchers at the AGU, is always overwhelming. I wish I would have been able to suck in more from all the information provided in the oral and poster sessions.
I, together with my collaborators Carlos Pérez García-Pando and Ron Miller, had following poster presentation on "Predicting the Mineral Composition of Dust Aerosols: Evaluation and Implications" in the session "Aerosol Comparisons between Observations and Models".
The abstract of the poster states:
"Soil dust aerosols in Earth system models are typically assumed to have globally uniform properties. However, important climate processes related to dust depend on the aerosol mineral and chemical composition, which varies regionally. Such processes include aerosol radiative forcing, transport of bioavailable iron that catalyzes marine photosynthesis, heterogeneous chemistry, ice nucleation, and cloud condensation.
We have implemented a new version of the soil dust aerosol scheme in the NASA GISS Earth System ModelE that takes into account the mineral composition of the dust particles. Dust aerosols are represented as an external mixture of minerals such as illite, kaolinite, smectite, carbonates, quartz, feldspar and gypsum, as well as iron oxides and accretions of iron oxides with each of these minerals.
We present a new publically available compilation of measurements of mineral fractions derived from ca. 50 references from the literature. This compilation is used to evaluate our new model of mineral and elemental composition within ModelE. We discuss the challenges of comparing simulated mineral fractions to measurements, which often come from field campaigns and ship cruises of limited duration. Despite uncertainties of the measurements, we show the importance of estimating the undisturbed size distribution of the parent soil prior to wet sieving, along with the modification of this size distribution during emission.
In particular, our new model reproduces measurements showing greater amount of aerosols at silt sizes (whose diameters exceed 2 μm) including significant amounts of clay mineral aerosols (like illite) at silt sizes. Our model also reduces the systematic overestimation of quartz, while allowing iron to be transported farther from its source as impurities than in its pure, crystalline form."
The two papers where the details of the results from three years of research can be found have just been submitted to Atmos. Chem. Phys. Discuss. Let's see how they are going to do in the review process.
Update 03/07/2015: Our two discussion papers have been published at Atmospheric Chemistry and Physics Discussions now and can be found here:
http://www.atmos-chem-phys-discuss.net/15/3493/2015/acpd-15-3493-2015.html
http://www.atmos-chem-phys-discuss.net/15/3577/2015/acpd-15-3577-2015.html
I, together with my collaborators Carlos Pérez García-Pando and Ron Miller, had following poster presentation on "Predicting the Mineral Composition of Dust Aerosols: Evaluation and Implications" in the session "Aerosol Comparisons between Observations and Models".
The abstract of the poster states:
"Soil dust aerosols in Earth system models are typically assumed to have globally uniform properties. However, important climate processes related to dust depend on the aerosol mineral and chemical composition, which varies regionally. Such processes include aerosol radiative forcing, transport of bioavailable iron that catalyzes marine photosynthesis, heterogeneous chemistry, ice nucleation, and cloud condensation.
We have implemented a new version of the soil dust aerosol scheme in the NASA GISS Earth System ModelE that takes into account the mineral composition of the dust particles. Dust aerosols are represented as an external mixture of minerals such as illite, kaolinite, smectite, carbonates, quartz, feldspar and gypsum, as well as iron oxides and accretions of iron oxides with each of these minerals.
We present a new publically available compilation of measurements of mineral fractions derived from ca. 50 references from the literature. This compilation is used to evaluate our new model of mineral and elemental composition within ModelE. We discuss the challenges of comparing simulated mineral fractions to measurements, which often come from field campaigns and ship cruises of limited duration. Despite uncertainties of the measurements, we show the importance of estimating the undisturbed size distribution of the parent soil prior to wet sieving, along with the modification of this size distribution during emission.
In particular, our new model reproduces measurements showing greater amount of aerosols at silt sizes (whose diameters exceed 2 μm) including significant amounts of clay mineral aerosols (like illite) at silt sizes. Our model also reduces the systematic overestimation of quartz, while allowing iron to be transported farther from its source as impurities than in its pure, crystalline form."
The two papers where the details of the results from three years of research can be found have just been submitted to Atmos. Chem. Phys. Discuss. Let's see how they are going to do in the review process.
Update 03/07/2015: Our two discussion papers have been published at Atmospheric Chemistry and Physics Discussions now and can be found here:
http://www.atmos-chem-phys-discuss.net/15/3493/2015/acpd-15-3493-2015.html
http://www.atmos-chem-phys-discuss.net/15/3577/2015/acpd-15-3577-2015.html