Mass analysis of charged aerosol particles in NLC and PMSE during the ECOMA/MASS campaign

Author
Robertson, Scott
Horányi, Mihály
Knappmiller, Scott
Sternovsky, Zoltan
Holzworth, Robert H.
Shimogawa, Michelle M.
Friedrich, Martin
Torkar, Klaus
Gumbel, Jörg
Megner, Linda
Baumgarten, Gerd
Latteck, Ralph
Rapp, Markus
Hoppe, Ulf-Peter
Hervig, Mark E.
Date Issued
2009
Permalink
http://hdl.handle.net/20.500.12242/756
https://publications.ffi.no/123456789/756
DOI
10.5194/angeo-27-1213-2009
Collection
Articles
Description
Robertson, Scott; Horányi, Mihály; Knappmiller, Scott; Sternovsky, Zoltan; Holzworth, Robert H.; Shimogawa, Michelle M.; Friedrich, Martin; Torkar, Klaus; Gumbel, Jörg; Megner, Linda; Baumgarten, Gerd; Latteck, Ralph; Rapp, Markus; Hoppe, Ulf-Peter; Hervig, Mark E.. Mass analysis of charged aerosol particles in NLC and PMSE during the ECOMA/MASS campaign. Annales Geophysicae 2009 ;Volum 27.(3) s. 1213-1232
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Abstract
MASS (Mesospheric Aerosol Sampling Spectrometer) is a multichannel mass spectrometer for charged aerosol particles, which was flown from the Andoya Rocket Range, Norway, through NLC and PMSE on 3 August 2007 and through PMSE on 6 August 2007. The eight-channel analyzers provided for the first time simultaneous measurements of the charge density residing on aerosol particles in four mass ranges, corresponding to ice particles with radii <0.5 nm (including ions), 0.5-1 nm, 1-2 nm, and >3 nm (approximately). Positive and negative particles were recorded on separate channels. Faraday rotation measurements provided electron density and a means of checking charge density measurements made by the spectrometer. Additional complementary measurements were made by rocket-borne dust impact detectors, electric field booms, a photometer and ground-based radar and lidar. The MASS data from the first flight showed negative charge number densities of 1500 3000 cm(-3) for particles with radii >3 nm from 83-88 km approximately coincident with PMSE observed by the ALWIN radar and NLC observed by the ALOMAR lidar. For particles in the 1-2 nm range, number densities of positive and negative charge were similar in magnitude (similar to 2000 cm(-3)) and for smaller particles, 0.5-1 nm in radius, positive charge was dominant. The occurrence of positive charge on the aerosol particles of the smallest size and predominately negative charge on the particles of largest size suggests that nucleation occurs on positive condensation nuclei and is followed by collection of negative charge during subsequent growth to larger size. Faraday rotation measurements show a bite-out in electron density that increases the time for positive aerosol particles to be neutralized and charged negatively. The larger particles (>3 nm) are observed throughout the NLC region, 83-88 km, and the smaller particles are observed primarily at the high end of the range, 86-88 km. The second flight into PMSE alone at 84-88 km, found only small number densities (similar to 500 cm(-3)) of particles >3 nm in a narrow altitude range, 86.5-87.5 km. Both positive (similar to 2000 cm(-3)) and negative (similar to 4500 cm(-3)) particles with radii 1-2 nm were detected from 85-87.5 km.
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