Staff Publications

Staff Publications

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    'Staff publications' is the digital repository of Wageningen University & Research

    'Staff publications' contains references to publications authored by Wageningen University staff from 1976 onward.

    Publications authored by the staff of the Research Institutes are available from 1995 onwards.

    Full text documents are added when available. The database is updated daily and currently holds about 240,000 items, of which 72,000 in open access.

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Record number 419467
Title Sources, distribution, and acidity of sulfate–ammonium aerosol in the Arctic in winter–spring
Author(s) Fisher, J.A.; Jacob, D.J.; Wang, Q.; Bahreini, R.; Carouge, C.C.; Cubison, M.J.; Dibb, J.E.; Diehl, T.; Jiminez, J.L.; Leibensperger, E.M.; Lu, Z.; Meinders, M.B.J.; Pye, H.O.T.; Quinn, P.K.; Sharma, S.; Streets, D.G.; Donkelaar, A. van; Yantosca, R.M.
Source Atmospheric Environment 45 (2011)39. - ISSN 1352-2310 - p. 7301 - 7318.
DOI http://dx.doi.org/10.1016/j.atmosenv.2011.08.030
Department(s) FBR Food Technology
Publication type Refereed Article in a scientific journal
Publication year 2011
Keyword(s) circulation model assessment - cloud resolving simulations - dry deposition - chemical-composition - asian pollution - ice nucleation - air-pollution - intex-b - atmospheric transport - ozone depletion
Abstract We use GEOS-Chem chemical transport model simulations of sulfate–ammonium aerosol data from the NASA ARCTAS and NOAA ARCPAC aircraft campaigns in the North American Arctic in April 2008, together with longer-term data from surface sites, to better understand aerosol sources in the Arctic in winter–spring and the implications for aerosol acidity. Arctic pollution is dominated by transport from mid-latitudes, and we test the relevant ammonia and sulfur dioxide emission inventories in the model by comparison with wet deposition flux data over the source continents. We find that a complicated mix of natural and anthropogenic sources with different vertical signatures is responsible for sulfate concentrations in the Arctic. East Asian pollution influence is weak in winter but becomes important in spring through transport in the free troposphere. European influence is important at all altitudes but never dominant. West Asia (non-Arctic Russia and Kazakhstan) is the largest contributor to Arctic sulfate in surface air in winter, reflecting a southward extension of the Arctic front over that region. Ammonium in Arctic spring mostly originates from anthropogenic sources in East Asia and Europe, with added contribution from boreal fires, resulting in a more neutralized aerosol in the free troposphere than at the surface. The ARCTAS and ARCPAC data indicate a median aerosol neutralization fraction [NH4+]/(2[SO42-] + [NO3-]) of 0.5 mol mol-1 below 2 km and 0.7 mol mol-1 above. We find that East Asian and European aerosol transported to the Arctic is mostly neutralized, whereas West Asian and North American aerosol is highly acidic. Growth of sulfur emissions in West Asia may be responsible for the observed increase in aerosol acidity at Barrow over the past decade. As global sulfur emissions decline over the next decades, increasing aerosol neutralization in the Arctic is expected, potentially accelerating Arctic warming through indirect radiative forcing and feedbacks.
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