Bedoukian   RussellIPM   RussellIPM   Piezoelectric Micro-Sprayer


Home
Animal Taxa
Plant Taxa
Semiochemicals
Floral Compounds
Semiochemical Detail
Semiochemicals & Taxa
Synthesis
Control
Invasive spp.
References

Abstract

Guide

Alphascents
Pherobio
InsectScience
E-Econex
Counterpart-Semiochemicals
Print
Email to a Friend
Kindly Donate for The Pherobase

« Previous AbstractIsotopes of volatile organic compounds: an emerging approach for studying atmospheric budgets and chemistry    Next AbstractBiomarker Discovery and Utility in Necrotizing Enterocolitis »

Proc Natl Acad Sci U S A


Title:Biogenic carbon and anthropogenic pollutants combine to form a cooling haze over the southeastern United States
Author(s):Goldstein AH; Koven CD; Heald CL; Fung IY;
Address:"Department of Environmental Science, Policy, and Management, University of California, Berkeley, CA 94720, USA. ahg@nature.berkeley"
Journal Title:Proc Natl Acad Sci U S A
Year:2009
Volume:20090518
Issue:22
Page Number:8835 - 8840
DOI: 10.1073/pnas.0904128106
ISSN/ISBN:1091-6490 (Electronic) 0027-8424 (Print) 0027-8424 (Linking)
Abstract:"Remote sensing data over North America document the ubiquity of secondary aerosols resulting from a combination of primary biogenic and anthropogenic emissions. The spatial and temporal distribution of aerosol optical thickness (AOT) over the southeastern United States cannot be explained by anthropogenic aerosols alone, but is consistent with the spatial distribution, seasonal distribution, and temperature dependence of natural biogenic volatile organic compound (BVOC) emissions. These patterns, together with observations of organic aerosol in this region being dominated by modern (14)C and BVOC oxidation products with summer maxima, indicate nonfossil fuel origins and strongly suggest that the dominant summer AOT signal is caused by secondary aerosol formed from BVOC oxidation. A link between anthropogenic and biogenic emissions forming secondary aerosols that dominate the regional AOT is supported by reports of chemicals in aerosols formed by BVOC oxidation in a NO(x)- and sulfate-rich environment. Even though ground-based measurements from the IMPROVE network suggest higher sulfate than organic concentrations near the surface in this region, we infer that much of the secondary organic aerosol in the Southeast must occur above the surface layer, consistent with reported observations of the organic fraction of the total aerosol increasing with height and models of the expected vertical distribution of secondary organic aerosols from isoprene oxidation. The observed AOT is large enough in summer to provide regional cooling; thus we conclude that this secondary aerosol source is climatically relevant with significant potential for a regional negative climate feedback as BVOC emissions increase with temperature"
Keywords:Aerosols/*chemistry Air Pollutants/*chemistry Carbon/*chemistry *Climatic Processes *Cold Temperature Environmental Monitoring United States Volatile Organic Compounds/*chemistry;
Notes:"MedlineGoldstein, Allen H Koven, Charles D Heald, Colette L Fung, Inez Y eng Research Support, U.S. Gov't, Non-P.H.S. 2009/05/20 Proc Natl Acad Sci U S A. 2009 Jun 2; 106(22):8835-40. doi: 10.1073/pnas.0904128106. Epub 2009 May 18"

 
Back to top
 
Citation: El-Sayed AM 2024. The Pherobase: Database of Pheromones and Semiochemicals. <http://www.pherobase.com>.
© 2003-2024 The Pherobase - Extensive Database of Pheromones and Semiochemicals. Ashraf M. El-Sayed.
Page created on 22-11-2024