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Chasing pre-industrial aerosols

Project description

Hypotheses on how pre-industrial aerosols can form in pristine environments

Models are critical to testing hypotheses and predicting outcomes. Models of climate change attempt to explain past events and predict future ones using data related to man-made and natural climate drivers. Aerosol particles result from both human activity and natural emissions. Significant uncertainty exists regarding their net effect on climate. One way to distinguish them is to look at pre-industrial environments when only natural aerosol emissions were present. The EU-funded CHAPAs project is studying aerosols in pristine environments like the Arctic and Siberia as a proxy. Environmental measurements and laboratory experiments will help scientists quantify the ways in which new aerosol particles form and grow, pointing to pre-industrial aerosol nucleation mechanisms that could enhance the accuracy of climate models.

Objective

Aerosol particles affect the climate by scattering incoming radiation and by acting as cloud condensation nuclei; however, their net effect remains of highest uncertainty, specifically when quantifying their relationship to anthropogenic greenhouse gases. It has been estimated that 45% of the variance of aerosol forcing arises from uncertainties in natural emissions. This highlight the importance of understanding pristine preindustrial-like environments, with natural aerosols only. One of the great challenges in understanding preindustrial aerosols and their sources resides in identifying the processes by which new particles form and grow from oxidized vapours.
We recently presented in Science the ground-breaking observation of purely organic nucleation. The existence of this mechanism was confirmed by laboratory experiments where we show that highly oxygenated molecules are able to form new particles independent of H2SO4. This finding sheds the light into the preindustrial era where the anthropogenic emissions were almost absent and H2SO4 concentration was rather minimal.
The aim of my project is to provide unprecedented data to resolve the preindustrial nucleation mechanism. I will organize intensive long-term measurements in pristine preindustrial-like environments like the Arctic and Siberia. Using state-of-the-art chemical ionization mass spectrometry, I will retrieve the chemical cluster composition and the vapours concentration. Additionally, I am planning short intensive measurements at high altitude above the oceans. Finally, these measurements will be complemented by laboratory experiments needed to probe the observed mechanism and retrieve a parametrization that can be used in global modelling.
The outcome of these field campaigns combined with laboratory experiments will provide extraordinary results in understanding pre-industrial aerosol formation, which will set the baseline for estimations of the impact of present and future aerosol on climate.

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Topic(s)

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ERC-STG - Starting Grant

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Call for proposal

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(opens in new window) ERC-2019-STG

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Host institution

HELSINGIN YLIOPISTO
Net EU contribution

Net EU financial contribution. The sum of money that the participant receives, deducted by the EU contribution to its linked third party. It considers the distribution of the EU financial contribution between direct beneficiaries of the project and other types of participants, like third-party participants.

€ 1 999 704,00
Address
FABIANINKATU 33
00014 HELSINGIN YLIOPISTO
Finland

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Activity type
Higher or Secondary Education Establishments
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Total cost

The total costs incurred by this organisation to participate in the project, including direct and indirect costs. This amount is a subset of the overall project budget.

€ 1 999 704,00

Beneficiaries (1)

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