Airborne observations of regional variation in fluorescent aerosol across the United States

被引:101
作者
Perring, A. E. [1 ,2 ]
Schwarz, J. P. [1 ,2 ]
Baumgardner, D. [3 ]
Hernandez, M. T. [4 ]
Spracklen, D. V. [5 ]
Heald, C. L. [6 ]
Gao, R. S. [1 ]
Kok, G. [3 ]
McMeeking, G. R. [3 ]
McQuaid, J. B. [5 ]
Fahey, D. W. [1 ]
机构
[1] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA
[2] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[3] Droplet Measurement Technol, Boulder, CO USA
[4] Univ Colorado, Dept Civil Environm & Architectural Engn, Boulder, CO 80309 USA
[5] Univ Leeds, Sch Earth & Environm, Leeds, W Yorkshire, England
[6] MIT, Dept Civil & Environm Engn, Boston, MA USA
基金
美国国家科学基金会;
关键词
bioaerosol; fluorescent aerosol; PBAP; biological particles; IN; CCN; PRIMARY BIOLOGICAL AEROSOL; HIGH-ELEVATION SITE; ICE NUCLEATION; DIFFERENT ECOSYSTEMS; SIZE DISTRIBUTIONS; GLOBAL ATMOSPHERE; FUNGAL SPORES; CLIMATE MODEL; MINERAL DUST; UV-APS;
D O I
10.1002/2014JD022495
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Airborne observations of fluorescent aerosol were made aboard an airship during CloudLab, a series of flights that took place in September and October of 2013 and covered a wideband of longitude across the continental U.S. between Florida and California and between 28 and 37N latitudes. Sampling occurred from near the surface to 1000m above the ground. A Wideband Integrated Bioaerosol Sensor (WIBS-4) measured average concentrations of supermicron fluorescent particles aloft (1 mu m to 10 mu m), revealing number concentrations ranging from 2.10.8 to 8.72.2x10(4) particles m(-3) and representing up to 24% of total supermicron particle number. We observed distinct variations in size distributions and fluorescent characteristics in different regions, and attribute these to geographically diverse bioaerosol. Fluorescent aerosol detected in the east is largely consistent with mold spores observed in a laboratory setting, while a shift to larger sizes associated with different fluorescent patterns is observed in the west. Fluorescent bioaerosol loadings in the desert west were as high as those near the Gulf of Mexico, suggesting that bioaerosol is a substantial component of supermicron aerosol both in humid and arid environments. The observations are compared to model fungal and bacterial loading predictions, and good agreement in both particle size and concentrations is observed in the east. In the west, the model underestimated observed concentrations by a factor between 2 and 4 and the prescribed particle sizes are smaller than the observed fluorescent aerosol. A classification scheme for use with WIBS data is also presented.
引用
收藏
页码:1153 / 1170
页数:18
相关论文
共 54 条
[1]   Molecular identification of potential pathogens in water and air of a hospital therapy pool [J].
Angenent, LT ;
Kelley, ST ;
St Amand, A ;
Pace, NR ;
Hernandez, MT .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2005, 102 (13) :4860-4865
[2]  
Blanchard C., 1970, SCIENCE, V170, P626
[3]   Seasonal variability in airborne bacterial communities at a high-elevation site [J].
Bowers, Robert M. ;
McCubbin, Ian B. ;
Hallar, Anna G. ;
Fierer, Noah .
ATMOSPHERIC ENVIRONMENT, 2012, 50 :41-49
[4]   Characterization of Airborne Microbial Communities at a High-Elevation Site and Their Potential To Act as Atmospheric Ice Nuclei [J].
Bowers, Robert M. ;
Lauber, Christian L. ;
Wiedinmyer, Christine ;
Hamady, Micah ;
Hallar, Anna G. ;
Fall, Ray ;
Knight, Rob ;
Fierer, Noah .
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 2009, 75 (15) :5121-5130
[5]   Ice nuclei in marine air: biogenic particles or dust? [J].
Burrows, S. M. ;
Hoose, C. ;
Poeschl, U. ;
Lawrence, M. G. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2013, 13 (01) :245-267
[6]   Bacteria in the global atmosphere - Part 1: Review and synthesis of literature data for different ecosystems [J].
Burrows, S. M. ;
Elbert, W. ;
Lawrence, M. G. ;
Poeschl, U. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2009, 9 (23) :9263-9280
[7]   Bacteria in the global atmosphere - Part 2: Modeling of emissions and transport between different ecosystems [J].
Burrows, S. M. ;
Butler, T. ;
Joeckel, P. ;
Tost, H. ;
Kerkweg, A. ;
Poeschl, U. ;
Lawrence, M. G. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2009, 9 (23) :9281-9297
[8]   Ubiquity of biological ice nucleators in snowfall [J].
Christner, Brent C. ;
Morris, Cindy E. ;
Foreman, Christine M. ;
Cai, Rongman ;
Sands, David C. .
SCIENCE, 2008, 319 (5867) :1214-1214
[9]   Ice formation and development in aged, wintertime cumulus over the UK: observations and modelling [J].
Crawford, I. ;
Bower, K. N. ;
Choularton, T. W. ;
Dearden, C. ;
Crosier, J. ;
Westbrook, C. ;
Capes, G. ;
Coe, H. ;
Connolly, P. J. ;
Dorsey, J. R. ;
Gallagher, M. W. ;
Williams, P. ;
Trembath, J. ;
Cui, Z. ;
Blyth, A. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2012, 12 (11) :4963-4985
[10]   Dust and Biological Aerosols from the Sahara and Asia Influence Precipitation in the Western U.S. [J].
Creamean, Jessie M. ;
Suski, Kaitlyn J. ;
Rosenfeld, Daniel ;
Cazorla, Alberto ;
DeMott, Paul J. ;
Sullivan, Ryan C. ;
White, Allen B. ;
Ralph, F. Martin ;
Minnis, Patrick ;
Comstock, Jennifer M. ;
Tomlinson, Jason M. ;
Prather, Kimberly A. .
SCIENCE, 2013, 339 (6127) :1572-1578