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      Optimized method for black carbon analysis in ice and snow using the Single Particle Soot Photometer

      , , , , , ,
      Atmospheric Measurement Techniques
      Copernicus GmbH

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          Abstract

          <p><strong>Abstract.</strong> In this study we attempt to optimize the method for measuring black carbon (BC) in snow and ice using a Single Particle Soot Photometer (SP2). Beside the previously applied ultrasonic (CETAC) and Collison-type nebulizers we introduce a jet (Apex Q) nebulizer to aerosolize the aqueous sample for SP2 analysis. Both CETAC and Apex Q require small sample volumes (a few milliliters) which makes them suitable for ice core analysis. The Apex Q shows the least size-dependent nebulizing efficiency in the BC particle diameter range of 100–1000 nm. The CETAC has the advantage that air and liquid flows can be monitored continuously. All nebulizer-types require a calibration with BC standards for the determination of the BC mass concentration in unknown aqueous samples. We found Aquadag to be a suitable material for preparing calibration standards. Further, we studied the influence of different treatments for fresh discrete snow and ice samples as well as the effect of storage. The results show that samples are best kept frozen until analysis. Once melted, they should be sonicated for 25 min, immediately analyzed while being stirred and not be refrozen.</p>

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          Present-day climate forcing and response from black carbon in snow

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            20th-century industrial black carbon emissions altered Arctic climate forcing.

            Black carbon (BC) from biomass and fossil fuel combustion alters chemical and physical properties of the atmosphere and snow albedo, yet little is known about its emission or deposition histories. Measurements of BC, vanillic acid, and non-sea-salt sulfur in ice cores indicate that sources and concentrations of BC in Greenland precipitation varied greatly since 1788 as a result of boreal forest fires and industrial activities. Beginning about 1850, industrial emissions resulted in a sevenfold increase in ice-core BC concentrations, with most change occurring in winter. BC concentrations after about 1951 were lower but increasing. At its maximum from 1906 to 1910, estimated surface climate forcing in early summer from BC in Arctic snow was about 3 watts per square meter, which is eight times the typical preindustrial forcing value.
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              Single-particle measurements of midlatitude black carbon and light-scattering aerosols from the boundary layer to the lower stratosphere

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                Author and article information

                Journal
                Atmospheric Measurement Techniques
                Atmos. Meas. Tech.
                Copernicus GmbH
                1867-8548
                2014
                August 21 2014
                : 7
                : 8
                : 2667-2681
                Article
                10.5194/amt-7-2667-2014
                a44fa9d5-d3e0-4302-859b-fb1d8c52c137
                © 2014

                https://creativecommons.org/licenses/by/3.0/

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