Ice-nucleating particles near two major dust source regions

0562232 - ÚVGZ 2023 RIV DE eng J - Článek v odborném periodiku
Beall, Ch. M. - Hill, T. C. J. - DeMott, P. J. - Koneman, T. - Pikridas, M. - Drewnick, F. - Harder, H. - Pohlker, Ch. - Lelieveld, J. - Weber, B. - Iakovides, M. - Prokeš, Roman - Sciare, J. - Andreae, M. O. - Stokes, M. D. - Prather, K. A.
Ice-nucleating particles near two major dust source regions.
Atmospheric Chemistry and Physics. Roč. 22, č. 18 (2022), s. 12607-12627. ISSN 1680-7316. E-ISSN 1680-7324
Institucionální podpora: RVO:86652079
Klíčová slova: sea spray aerosol * mineral dust * ship-borne measurements * arabian peninsula * active-sites * mixing state * saharan dust * marine air * nuclei * mediterranean sea
Obor OECD: Meteorology and atmospheric sciences
Impakt faktor: 6.3, rok: 2022
Způsob publikování: Open access
https://acp.copernicus.org/articles/22/12607/2022/

Mineral dust and sea spray aerosol represent important sources of ice-nucleating particles (INPs), the minor fraction of aerosol particles able to trigger cloud ice crystal formation and, consequently, influence multiple climate-relevant cloud properties including lifetime, radiative properties and precipitation initiation efficiency. Mineral dust is considered the dominant INP source in many parts of the world due to its ice nucleation efficiency and its sheer abundance, with global emission rates of up to 4700 Tg a(-1). However, INPs emitted from the ocean surface in sea spray aerosol frequently dominate INP populations in remote marine environments, including parts of the Southern Ocean where cloud-resolving model simulations have demonstrated that cloud radiative properties are likely strongly controlled by INPs. Here we report INP concentrations measured in aerosol and seawater samples during Air Quality and Climate Change in the Arabian Basin (AQABA), a shipborne campaign that spanned the Red Sea, Gulf of Aden, Arabian Sea, Arabian Gulf and part of the Mediterranean. In aerosol samples collected within a few hundred kilometers of the first and second ranked sources of dust globally, the Sahara and Arabian Peninsula, INP concentrations ranged from 0.2 to 11 L-1 at20 degrees C with observed ice-active surface site densities (n(s)) 1-3 orders of magnitude below levels predicted by mineral dust INP parameterizations. Over half of the samples (at least 14 of 26) were collected during dust storms with average dust mass concentrations between 150 and 490 mu g m(-3) (PM10), as simulated by the Modern-Era Retrospective analysis for Research and Application, version 2 (MERRA-2). The impacts of heat and peroxide treatments indicate that organics dominated the observed ice nucleation (IN) activity at temperatures >=15 degrees C with proteinaceous (heat-labile) INPs frequently observed at high freezing temperatures > 10 degrees C. INP concentrations in seawater samples ranged between 3 and 46 mL(-1) at19 degrees C, demonstrating the relatively low INP source potential of seawater in the region as compared to seawater from multiple other regions reported previously. Overall, our results demonstrate that despite proximity to the Sahara and the Arabian Peninsula and the dominance of mineral dust in the aerosol sampled, existing mineral dust parameterizations alone would not skillfully represent the near-surface n(s) in the observed temperature regime (-6 to25 degrees C). Future efforts to develop or improve representations of dust INPs at modest supercooling (>=15 degrees C) would benefit from a characterization of the specific organic species associated with dust INPs. More generally, an improved understanding of the organic species associated with increased IN activity and their variability across dust source regions would directly inform efforts to determine whether n(s)-based parameterizations are appropriate for faithful representation of dust INPs in this sensitive temperature regime, whether region-specific parameterizations are required, or whether an alternative to the n(s) approach is necessary.
Trvalý link: https://hdl.handle.net/11104/0334910