Welcome to the new version of CaltechAUTHORS. Login is currently restricted to library staff. If you notice any issues, please email coda@library.caltech.edu
Published October 14, 2013 | Supplemental Material + Published
Journal Article Open

Los Angeles Basin airborne organic aerosol characterization during CalNex

Abstract

We report airborne organic aerosol (OA) measurements over Los Angeles carried out in May 2010 as part of the CalNex field campaign. The principal platform for the airborne data reported here was the CIRPAS Twin Otter (TO); airborne data from NOAA WP-3D aircraft and Pasadena CalNex ground-site data acquired during simultaneous TO flybys are also presented. Aerodyne aerosol mass spectrometer measurements constitute the main source of data analyzed. The increase in organic aerosol oxidation from west to east in the basin was sensitive to OA mass loading, with a greater spatial trend in O:C associated with lower mass concentration. Three positive matrix factorization (PMF) components (hydrocarbon-like organic aerosol (HOA), semi-volatile oxidized organic aerosol (SVOOA), and low volatility oxidized organic aerosol (LVOOA)) were resolved for the one flight that exhibited the largest variability in estimated O:C ratio. Comparison of the PMF factors with two optical modes of refractory black carbon (rBC)-containing aerosol revealed that the coating of thinly coated rBC-containing aerosol, dominant in the downtown region, is likely composed of HOA, whereas more thickly coated rBC-containing aerosol, dominant in the Banning pass outflow, is composed of SVOOA and LVOOA. The correlation of water-soluble organic mass to oxidized organic aerosol (OOA) is higher in the outflows than in the basin due to the higher mass fraction of OOA/OA in the outflows. By comparison, the average OA concentration over Mexico City MILAGRO (Megacity Initiative: Local and Global Research Observations) campaign was ∼7 times higher than the airborne average during CalNex.

Additional Information

© 2013 American Geophysical Union. Received 12 March 2013; revised 13 September 2013; accepted 16 September 2013; published 14 October 2013. This work was supported by NOAA grant NA09OAR4310128. The authors would like to acknowledge the Center for Interdisciplinary Remotely-Piloted Aircraft Studies (CIRPAS) crew at the Naval Postgraduate School in Monterey, California for their support during CalNex. The authors would also like to acknowledge B. L. Lefer for use of the PBLH data from the CalNex Pasadena ground-site and W. T. Morgan for the use of their data in Figure 11. P.L.H. and J.L.J. thank CARB 08-319/11-305 and DOE (BER/ASR) DE-SC0006035/DE-FG02-11ER65293, as well as a CIRES Visiting Fellowship to P.L.H.

Attached Files

Published - jgrd50853.pdf

Supplemental Material - AMSvsDMAVol.pdf

Supplemental Material - LocationofIntercomparison.pdf

Supplemental Material - MSfpeakvary.pdf

Supplemental Material - OtoCvsLong.pdf

Supplemental Material - QContributions.pdf

Supplemental Material - ReadMeFileCravenCalNex.docx

Supplemental Material - SupplementalMaterialRRR.pdf

Supplemental Material - TSfpeakvary.pdf

Supplemental Material - ThreeFactorTs.pdf

Supplemental Material - VolumeTS.pdf

Files

AMSvsDMAVol.pdf
Files (4.8 MB)
Name Size Download all
md5:9ec446bb8e11650d1a7a265d7d37c953
90.3 kB Download
md5:368378a254fe3efeea1cf60063d2a157
77.4 kB Preview Download
md5:13cd923aa011a82c7a78cf2aeca16d33
62.4 kB Preview Download
md5:e739ce430713f30feba8c27cd8c408e7
38.6 kB Preview Download
md5:f3ad4c3f5ae013f2006869a398be1651
91.6 kB Preview Download
md5:f7f8a22d5272138f97cba5632bb8d1fb
17.8 kB Preview Download
md5:4ce2abc80939f3808dc6f22b8b41e3a8
530.2 kB Preview Download
md5:42357f69edf8e5e36a5f61c2f910c0f5
22.7 kB Preview Download
md5:711ce47b28b9e39e502a522a4facbd69
5.8 kB Preview Download
md5:5f65f79881fa9982f2aebbb4ec3ae05e
59.5 kB Preview Download
md5:71dd8199105135995e40090a686e4f18
3.9 MB Preview Download

Additional details

Created:
August 22, 2023
Modified:
October 26, 2023