Articles | Volume 17, issue 20
https://doi.org/10.5194/acp-17-12779-2017
https://doi.org/10.5194/acp-17-12779-2017
Research article
 | 
26 Oct 2017
Research article |  | 26 Oct 2017

Do contemporary (1980–2015) emissions determine the elemental carbon deposition trend at Holtedahlfonna glacier, Svalbard?

Meri M. Ruppel, Joana Soares, Jean-Charles Gallet, Elisabeth Isaksson, Tõnu Martma, Jonas Svensson, Jack Kohler, Christina A. Pedersen, Sirkku Manninen, Atte Korhola, and Johan Ström

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Increase in elemental carbon values between 1970 and 2004 observed in a 300-year ice core from Holtedahlfonna (Svalbard)
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Cited articles

AMAP: The Impact of Black Carbon on Arctic Climate (2011). Arctic Monitoring and Assessment Programme (AMAP), Oslo, Norway, 72 pp., 2011.
Beaudon, E., Arppe, L., Jonsell, U., Martma, T., Möller, M., Pohjola, V. A., Scherer, D., and Moore, J. C.: Spatial and temporal variability of net accumulation from shallow cores from Vestfonna ice cap (Nordaustlandet, Svalbard), Geogr. Ann. A, 93, 287–299, https://doi.org/10.1111/j.1468-0459.2011.00439.x, 2011.
Beaudon, E., Moore, J. C., Martma, T., Pohjola, V. A., van der Wal, R. S. W., Kohler, J., and Isaksson, E.: Lomonosovfonna and Holtedahlfonna ice cores reveal east–west disparities of Spitsbergen environment since 1700 AD, J. Glaciol., 59, 1069–1083, https://doi.org/10.3189/2013JoG12J203, 2013.
Birch, M. E. and Cary, R. A.: Elemental carbon-based method for monitoring occupational exposures, to particulate diesel exhaust, Aerosol Sci. Tech., 25, 221–241, 1996.
Bond, T. C., Bhardwaj, E., Dong, R., Jogani, R., Jung, S., Roden, C., Streets, D. G., and Trautmann, N. M.: Historical emissions of black and organic carbon aerosol from energy-related combustion, 1850–2000, Global Biogeochem. Cy., 21, GB2018, https://doi.org/10.1029/2006GB002840, 2007.
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Short summary
Black carbon (BC) deposition enhances Arctic warming and melting. We present Svalbard ice core BC data from 2005 to 2015, comparing the results with chemical transport model data. The ice core and modelled BC deposition trends clearly deviate from measured and observed atmospheric concentration trends, and thus meteorological processes such as precipitation and scavenging efficiency seem to have a stronger influence on the BC deposition trend than BC emission or atmospheric concentration trends.
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