New-particle formation in connection with a nocturnal low-level jet: Observations and modeling results

Details New-particle formation in connection with a nocturnal low-level jet: Observations and modeling results New-particle formation in connection with a nocturnal low-level jet: Observations and modeling results

Aug 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007georl..3416822s&link_type=abstract

Geophysical Research Letters, Volume 34, Issue 16, CiteID L16822

Physics

2

Atmospheric Composition And Structure: Aerosols And Particles (0345, 4801, 4906), Atmospheric Composition And Structure: Cloud Physics And Chemistry, Atmospheric Composition And Structure: Pressure, Density, And Temperature

Scientific paper

Tethered-balloon borne observations show a correlation between a significant peak of ultrafine particle concentration and increased SO2 advected by a nocturnal low-level jet. The maximum of ultrafine particles is found at the lower edge of the jet in a region where the advected SO2 is mixed with colder and more humid air masses from below the jet. Model results corroborate that kinetic nucleation is the key mechanism for this nucleation event.

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