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Elemental and water-insoluble organic carbon in Svalbard snow: a synthesis of observations during 2007–2018
Abstrakt
Light-absorbing carbonaceous aerosols emitted by biomass or fossil fuel combustion can contribute to amplifying Arctic climate warming by lowering the albedo of snow. The Svalbard archipelago, being near to Europe and Russia, is particularly affected by these pollutants, and improved knowledge of their distribution in snow is needed to assess their impact. Here we present and synthesize new data obtained on Svalbard between 2007 and 2018, comprising measurements of elemental (EC) and water-insoluble organic carbon (WIOC) in snow from 37 separate sites. We used these data, combined with meteorological data and snowpack modeling, to investigate the variability of EC and WIOC deposition in Svalbard snow across latitude, longitude, elevation and time. Overall, EC concentrations (CECsnow) ranged from <1.0 to 266.6 ng g−1, while WIOC concentrations (CWIOCsnow) ranged from <1 to 9426 ng g−1, with the highest values observed near Ny-Ålesund. Calculated snowpack loadings (LECsnow, LWIOCsnow) on glaciers surveyed in spring 2016 were 0.1 to 2.6 mg m−2 and 2 to 173 mg m−2, respectively. The median CECsnow and the LECsnow on those glaciers were close to or lower than those found in earlier (2007–2009), comparable surveys. Both LECsnow and LWIOCsnow increased with elevation and snow accumulation, with dry deposition likely playing a minor role. Estimated area-averaged snowpack loads across Svalbard were 1.1 mg EC m−2 and 38.3 mg WIOC m−2 for the 2015–2016 winter. An ∼11-year long dataset of spring surface snow measurements from the central Brøgger Peninsula was used to quantify the interannual variability of EC and WIOC deposition in snow. In most years, CECsnow and CWIOCsnow at Ny-Ålesund (50 m a.s.l.) were 2–5 times higher than on the nearby Austre Brøggerbreen glacier (456 m a.s.l.), and the median EC/WIOC in Ny-Ålesund was 6 times higher, suggesting a possible influence of local EC emission from Ny-Ålesund. While no long-term trends between 2011 and 2018 were found, CECsnow and CWIOCsnow showed synchronous variations at Ny-Ålesund and Austre Brøggerbreen. When compared with data from other circum-Arctic sites obtained by comparable methods, the median CECsnow on Svalbard falls between that found in central Greenland (lowest) and those in continental sectors of European Arctic (northern Scandinavia, Russia and Siberia; highest), which is consistent with large-scale patterns of BC in snow reported by surveys based on other methods.
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Autorzy (13)
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Christian Zdanowicz
- Uppsala University
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Jean-Charles Gallet
- Norwegian Polar Institute
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Mats P. Björkman
- University of Gothenburg
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Catherine Larose
- Université de Lyon
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Thomas Schuler
- University of Oslo
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Andrea Spolaor
- Institute of Polar Sciences, ISP-CNR & Ca' Foscari University of Venice
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Elena Barbaro
- Institute of Polar Sciences, ISP-CNR & Ca' Foscari University of Venice
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Tõnu Martma
- Tallinn University of Technology
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Ward van Pelt
- Uppsala University
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Ulla Wideqvist
- Stockholm University
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Johan Ström
- Stockholm University
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Informacje szczegółowe
- Kategoria:
- Publikacja w czasopiśmie
- Typ:
- artykuły w czasopismach
- Opublikowano w:
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ATMOSPHERIC CHEMISTRY AND PHYSICS
nr 21,
strony 3035 - 3057,
ISSN: 1680-7316 - Język:
- angielski
- Rok wydania:
- 2021
- Opis bibliograficzny:
- Zdanowicz C., Gallet J., Björkman M. P., Larose C., Schuler T., Luks B., Koziol K., Spolaor A., Barbaro E., Martma T., van Pelt W., Wideqvist U., Ström J.: Elemental and water-insoluble organic carbon in Svalbard snow: a synthesis of observations during 2007–2018// ATMOSPHERIC CHEMISTRY AND PHYSICS -Vol. 21,iss. 4 (2021), s.3035-3057
- DOI:
- Cyfrowy identyfikator dokumentu elektronicznego (otwiera się w nowej karcie) 10.5194/acp-21-3035-2021
- Źródła finansowania:
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- The April 2016 survey on Svalbard was funded through a grant from the Svalbard Science Forum (RIS 10472) to Jean-Charles Gallet and others, and surface snow monitoring on Brøgger Peninsula was conducted by the Norwegian Polar Institute (NPI) with additional support from Svalbardmiljøfonds, the Swedish Research Council Formas project “Black and White” (grant 2006-00210 to Johan Ström and others), the Polish Ministry of Science and Higher Education (statutory activities 3841/E-41/S/2020), and the Institut Paul-Emile Victor (France). Planning and collaborative work between the study co-authors was facilitated by funds from the Swedish Strategic Research Area initiative “Biodiversity and Ecosystem services in a Changing Climate” through Gothenburg University, the Gothenburg Air and Climate Network and the International Arctic Science Committee.
- Weryfikacja:
- Politechnika Gdańska
wyświetlono 147 razy
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