How significantly does coagulational scavenging limit atmospheric particle production?
Open Access
- 27 October 2001
- journal article
- research article
- Published by American Geophysical Union (AGU)
- Vol. 106 (D20), 24119-24125
- https://doi.org/10.1029/2001jd000322
Abstract
No abstract availableKeywords
This publication has 28 references indexed in Scilit:
- Secondary organics and atmospheric cloud condensation nuclei productionPublished by American Geophysical Union (AGU) ,2000
- Ultrafine aerosol formation via ion‐mediated nucleationGeophysical Research Letters, 2000
- Ternary nucleation of H2SO4, NH3, and H2O in the atmosphereJournal of Geophysical Research: Atmospheres, 1999
- Secondary Organic Aerosol Formation vs Primary Organic Aerosol Emission: In Situ Evidence for the Chemical Coupling between Monoterpene Acidic Photooxidation Products and New Particle Formation over ForestsEnvironmental Science & Technology, 1999
- New Particle Formation in the Remote Troposphere: A Comparison of Observations at Various SitesGeophysical Research Letters, 1999
- Airborne aerosol measurements in the tropopause region and the dependence of new particle formation on preexisting particle number concentrationPublished by American Geophysical Union (AGU) ,1998
- The potential for atmospheric mixing processes to enhance the binary nucleation ratePublished by American Geophysical Union (AGU) ,1998
- New particle formation at a remote continental site: Assessing the contributions of SO2 and organic precursorsJournal of Geophysical Research: Atmospheres, 1997
- Carbon dioxide and methane in continental Europe: a climatology, and 222Radon-based emission estimatesTellus B: Chemical and Physical Meteorology, 1996
- Size distribution of Antarctic submicron aerosolsTellus B: Chemical and Physical Meteorology, 1993