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000010074 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000010074 1001_ $$0P:(DE-HGF)0$$aSnider, J.R.$$b0
000010074 245__ $$aIntercomparison of cloud condensation nuclei and hygroscopic fraction the LACIS Experiment in November (LExNo)
000010074 260__ $$aWashington, DC$$bUnion$$c2010
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000010074 440_0 $$06393$$aJournal of Geophysical Research D: Atmospheres$$v115$$x0148-0227
000010074 500__ $$aSeveral LExNo participants (G. Frank, A. Kiendler-Scharr, A. Kristensson, T. F. Mentel, D. Rose, J. Snider, and S. Walter) thank Atmospheric Composition Change: a European Network (ACCENT) for travel support. M. Bilde thanks the Nordic Center of Excellence, Research Unit BACCI, and Danish Natural Science Research Council for financial support. As a whole, the LExNo group thanks Simon Clegg. LExNo was hosted by the research group in Leipzig; their efforts were essential for bringing the study to fruition. The work of three reviewers is also acknowledged.
000010074 520__ $$aFour cloud condensation nuclei (CCN) instruments were used to sample size-selected particles prepared at the Leipzig Aerosol Cloud Interaction Simulator facility. Included were two Wyoming static diffusion CCN instruments, the continuous flow instrument built by Droplet Measurement Technologies, and the continuous flow Leipzig instrument. The aerosols were composed of ammonium sulfate, levoglucosan, levoglucosan and soot, and ammonium hydrogen sulfate and soot. Comparisons are made among critical supersaturation values from the CCN instruments and derived from measurements made with a humidified tandem differential mobility system. The comparison is quite encouraging: with few exceptions the reported critical supersaturations agree within known experimental uncertainty limits. Also reported are CCN- and hygroscopicity-based estimates of the soot particles' solute fraction. Relative differences between these are as large as 40%, but an error analysis demonstrates that agreement within experimental uncertainty is achieved. We also analyze data from the Droplet Measurement Technologies and the two Wyoming static diffusion instruments for evidence of size distribution broadening and investigate levoglucosan particle growth kinetics in the Wyoming CCN instrument.
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000010074 7001_ $$0P:(DE-HGF)0$$aWex, H.$$b1
000010074 7001_ $$0P:(DE-HGF)0$$aRose, D.$$b2
000010074 7001_ $$0P:(DE-HGF)0$$aKristensson, A.$$b3
000010074 7001_ $$0P:(DE-HGF)0$$aStratmann, F.$$b4
000010074 7001_ $$0P:(DE-HGF)0$$aHenning, T.$$b5
000010074 7001_ $$0P:(DE-HGF)0$$aHenning, S.$$b6
000010074 7001_ $$0P:(DE-HGF)0$$aKiselev, A.$$b7
000010074 7001_ $$0P:(DE-HGF)0$$aBilde, M.$$b8
000010074 7001_ $$0P:(DE-HGF)0$$aBurkhart, M.$$b9
000010074 7001_ $$0P:(DE-HGF)0$$aDusek, U.$$b10
000010074 7001_ $$0P:(DE-HGF)0$$aFrank, G.P.$$b11
000010074 7001_ $$0P:(DE-Juel1)4528$$aKiendler-Scharr, A.$$b12$$uFZJ
000010074 7001_ $$0P:(DE-Juel1)16346$$aMentel, T. F.$$b13$$uFZJ
000010074 7001_ $$0P:(DE-HGF)0$$aPetters, M.D.$$b14
000010074 7001_ $$0P:(DE-HGF)0$$aPöschl, U.$$b15
000010074 773__ $$0PERI:(DE-600)2016800-7 $$a10.1029/2009JD012618$$gVol. 115, p. D11205$$pD11205$$q115<D11205$$tJournal of geophysical research / Atmospheres  $$tJournal of Geophysical Research$$v115$$x0148-0227$$y2010
000010074 8567_ $$uhttp://dx.doi.org/10.1029/2009JD012618
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