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Nitrate postdeposition processes in Svalbard surface snow
Author(s) -
Björkman Mats P.,
Vega Carmen P.,
Kühnel Rafael,
Spataro Francesca,
Ianniello Antonietta,
Esposito Giulio,
Kaiser Jan,
Marca Alina,
Hodson Andy,
Isaksson Elisabeth,
Roberts Tjarda J.
Publication year - 2014
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2013jd021234
Subject(s) - snow , snowpack , nitrate , reactive nitrogen , atmospheric sciences , ozone , deposition (geology) , environmental science , environmental chemistry , nitrogen , chemistry , meteorology , geology , geography , structural basin , organic chemistry , paleontology
The snowpack acts as a sink for atmospheric reactive nitrogen, but several postdeposition pathways have been reported to alter the concentration and isotopic composition of snow nitrate with implications for atmospheric boundary layer chemistry, ice core records, and terrestrial ecology following snow melt. Careful daily sampling of surface snow during winter (11–15 February 2010) and springtime (9 April to 5 May 2010) near Ny‐Ålesund, Svalbard reveals a complex pattern of processes within the snowpack. Dry deposition was found to dominate over postdeposition losses, with a net nitrate deposition rate of (0.6 ± 0.2) µmol m −2 d −1 to homogeneous surface snow. At Ny‐Ålesund, such surface dry deposition can either solely result from long‐range atmospheric transport of oxidized nitrogen or include the redeposition of photolytic/bacterial emission originating from deeper snow layers. Our data further confirm that polar basin air masses bring 15 N‐depleted nitrate to Svalbard, while high nitrate δ ( 18 O) values only occur in connection with ozone‐depleted air, and show that these signatures are reflected in the deposited nitrate. Such ozone‐depleted air is attributed to active halogen chemistry in the air masses advected to the site. However, here the Ny‐Ålesund surface snow was shown to have an active role in the halogen dynamics for this region, as indicated by declining bromide concentrations and increasing nitrate δ ( 18 O), during high BrO (low‐ozone) events. The data also indicate that the snowpack BrO‐NO x cycling continued in postevent periods, when ambient ozone and BrO levels recovered.