Characteristics and effects of aerosols during blowing snow events in the central Arctic DOI Creative Commons
Nora Bergner, Benjamin Heutte, Ivo Beck

et al.

Elementa Science of the Anthropocene, Journal Year: 2025, Volume and Issue: 13(1)

Published: Jan. 1, 2025

Sea salt aerosol (SSaer) significantly impacts aerosol-radiation and aerosol-cloud interactions, sublimated blowing snow is hypothesized to be an important SSaer source in polar regions. Understanding other wind-sourced aerosols’ climate relevant properties needed, especially during winter when Arctic amplification greatest. However, most of our understanding comes from modeling studies, direct observations are sparse. Additionally, can originate multiple sources, making it difficult disentangle emission processes. Here, we present comprehensive events the Multidisciplinary drifting Observatory for Study Climate (MOSAiC) expedition central Arctic. High wind speed strongly enhances total number, submicron sodium chloride mass, cloud condensation nuclei concentrations, scattering coefficients. Generally, relative response enhancement strongest fall concentrations lowest. Blowing showed similar environmental across events, apart occasions with high age (>6 days since last snowfall). Coarse-mode number (>1 μm) better explained by variability averaged over 12-h air mass back trajectories arriving at MOSAiC site compared local, instantaneous speed, suggesting importance regional transport consideration history wind-driven production. These provide new insights into may help validate studies improve model parameterizations particularly indirect radiative forcing.

Language: Английский

Characteristics and effects of aerosols during blowing snow events in the central Arctic DOI Creative Commons
Nora Bergner, Benjamin Heutte, Ivo Beck

et al.

Elementa Science of the Anthropocene, Journal Year: 2025, Volume and Issue: 13(1)

Published: Jan. 1, 2025

Sea salt aerosol (SSaer) significantly impacts aerosol-radiation and aerosol-cloud interactions, sublimated blowing snow is hypothesized to be an important SSaer source in polar regions. Understanding other wind-sourced aerosols’ climate relevant properties needed, especially during winter when Arctic amplification greatest. However, most of our understanding comes from modeling studies, direct observations are sparse. Additionally, can originate multiple sources, making it difficult disentangle emission processes. Here, we present comprehensive events the Multidisciplinary drifting Observatory for Study Climate (MOSAiC) expedition central Arctic. High wind speed strongly enhances total number, submicron sodium chloride mass, cloud condensation nuclei concentrations, scattering coefficients. Generally, relative response enhancement strongest fall concentrations lowest. Blowing showed similar environmental across events, apart occasions with high age (>6 days since last snowfall). Coarse-mode number (>1 μm) better explained by variability averaged over 12-h air mass back trajectories arriving at MOSAiC site compared local, instantaneous speed, suggesting importance regional transport consideration history wind-driven production. These provide new insights into may help validate studies improve model parameterizations particularly indirect radiative forcing.

Language: Английский

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