K. Torseth et al., Processes affecting deposition of oxidised nitrogen and associated speciesin the coastal areas of Norway, ATMOS ENVIR, 34(2), 2000, pp. 207-217
Measurement data on air, precipitation and canopy throughfall chemistry fro
m a network of sites have been combined to study scavenging and deposition
processes, with particular emphasis on the oxidised nitrogen species. High
deposition rates of oxidised nitrogen occur in coastal areas of SW Norway.
These are partly caused by high precipitation rates, partly also because a
large fraction of the oxidised nitrogen is present as nitrate in large part
icles, which are rapidly removed by both wet and dry deposition processes.
High wind speeds near the coast result in high concentrations of sea-salt p
articles in the air and high deposition rates of both nitrate and sea-salt
particles, particularly in coniferous forest stands. HNO3 contributes on av
erage only about 10-20% to the sum of aerosol nitrate and HNO3 (sNO(3)). St
ill, the combined dry deposition velocity of sNO(3) to these forest stands
may be between 4 and 6 cm s(-1) on average. (C) 1999 Elsevier Science Ltd.
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