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231225s2021 xx |||||o 00| ||eng c |
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|a 10.1029/2021gl096520
|2 doi
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|a eng
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|a Hilario, Miguel Ricardo A
|e verfasserin
|4 aut
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|a Particulate Oxalate-To-Sulfate Ratio as an Aqueous Processing Marker
|b Similarity Across Field Campaigns and Limitations
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|c 2021
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|a Text
|b txt
|2 rdacontent
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|a ƒaComputermedien
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|2 rdamedia
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|a ƒa Online-Ressource
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|a Date Revised 16.02.2022
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|a published: Print-Electronic
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|a figshare: 10.6084/m9.figshare.11861859.v2
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|a Citation Status PubMed-not-MEDLINE
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|a Leveraging aerosol data from multiple airborne and surface-based field campaigns encompassing diverse environmental conditions, we calculate statistics of the oxalate-sulfate mass ratio (median: 0.0217; 95% confidence interval: 0.0154-0.0296; R = 0.76; N = 2,948). Ground-based measurements of the oxalate-sulfate ratio fall within our 95% confidence interval, suggesting the range is robust within the mixed layer for the submicrometer particle size range. We demonstrate that dust and biomass burning emissions can separately bias this ratio toward higher values by at least one order of magnitude. In the absence of these confounding factors, the 95% confidence interval of the ratio may be used to estimate the relative extent of aqueous processing by comparing inferred oxalate concentrations between air masses, with the assumption that sulfate primarily originates from aqueous processing
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|a Journal Article
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|a Crosbie, Ewan
|e verfasserin
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|a Bañaga, Paola Angela
|e verfasserin
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|a Betito, Grace
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|a Braun, Rachel A
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|a Cambaliza, Maria Obiminda
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|a Corral, Andrea F
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|a Cruz, Melliza Templonuevo
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|a Dibb, Jack E
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|a Lorenzo, Genevieve Rose
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|a MacDonald, Alexander B
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|a Robinson, Claire E
|e verfasserin
|4 aut
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|a Shook, Michael A
|e verfasserin
|4 aut
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|a Simpas, James Bernard
|e verfasserin
|4 aut
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|a Stahl, Connor
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|a Winstead, Edward
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|a Ziemba, Luke D
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|a Sorooshian, Armin
|e verfasserin
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| 773 |
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|i Enthalten in
|t Geophysical research letters
|d 1984
|g 48(2021), 23 vom: 16. Dez.
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|u http://dx.doi.org/10.1029/2021gl096520
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