Extensive aerosol and trace gas measurements were conducted at Ny-Ålesund (Svalbard) before and after arctic sunrise in 2001 (NICE Dark and Light intensive campaigns) in order to study the possible role of aerosols in the renoxification mechanism. This study reports aerosol physical measurements over a continuous 3-month period. Arctic and sub-arctic airmasses dominated the measurement period and were characterised by low number (N ~ 275 and 590 cm-3; respectively) and surface area (S ~ 39 and 28 µm2cm-3) concentrations (measured range d = 14 740 nm) except for two arctic haze events with high concentrations in springtime (N ~ 1140 cm-3 and S ~ 125 µm2 cm-3). Excluding these events, aerosol volatility measurements indicated no significant variation in the volatile (~ 0.40), semi-volatile (~ 0.32) or refractory (~ 0.28) volume fractions which are commonly attributed to H2SO4, (NH4)2SO4)/NH4HSO4, and soot/dust/sea-salt aerosol. No significant correlation was found between aerosol physical parameters and HONO mixing ratios from denuder measurements suggesting that airborne particles in the marine arctic boundary layer do not participate in renoxification.
Overview of Aerosol Microphysics at Arctic Sunrise: Measurements during the NICE ReNOxification Study
H J Beine
2004
Abstract
Extensive aerosol and trace gas measurements were conducted at Ny-Ålesund (Svalbard) before and after arctic sunrise in 2001 (NICE Dark and Light intensive campaigns) in order to study the possible role of aerosols in the renoxification mechanism. This study reports aerosol physical measurements over a continuous 3-month period. Arctic and sub-arctic airmasses dominated the measurement period and were characterised by low number (N ~ 275 and 590 cm-3; respectively) and surface area (S ~ 39 and 28 µm2cm-3) concentrations (measured range d = 14 740 nm) except for two arctic haze events with high concentrations in springtime (N ~ 1140 cm-3 and S ~ 125 µm2 cm-3). Excluding these events, aerosol volatility measurements indicated no significant variation in the volatile (~ 0.40), semi-volatile (~ 0.32) or refractory (~ 0.28) volume fractions which are commonly attributed to H2SO4, (NH4)2SO4)/NH4HSO4, and soot/dust/sea-salt aerosol. No significant correlation was found between aerosol physical parameters and HONO mixing ratios from denuder measurements suggesting that airborne particles in the marine arctic boundary layer do not participate in renoxification.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
