Hit from both sides: tracking industrial and volcanic plumes in Mexico City with surface measurements and OMI SO2 retrievals during the MILAGRO field campaign

被引:74
作者
de Foy, B. [1 ]
Krotkov, N. A. [2 ]
Bei, N. [3 ,4 ]
Herndon, S. C. [5 ]
Huey, L. G. [6 ]
Martinez, A. -P.
Ruiz-Suarez, L. G. [7 ]
Wood, E. C. [5 ]
Zavala, M. [3 ,4 ]
Molina, L. T. [3 ,4 ]
机构
[1] St Louis Univ, Dept Earth & Atmospher Sci, St Louis, MO 63103 USA
[2] Univ Maryland, Goddard Earth Sci & Technol Ctr, College Pk, MD 20742 USA
[3] Molina Ctr Energy & Environm, La Jolla, CA USA
[4] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA USA
[5] Aerodyne Res Inc, Billerica, MA 01821 USA
[6] Georgia Inst Technol, Atlanta, GA 30332 USA
[7] Univ Nacl Autonoma Mexico, Ctr Ciencias Atmosfera, Mexico City 04510, DF, Mexico
基金
美国国家科学基金会;
关键词
AIR-POLLUTION; POPOCATEPETL VOLCANO; AEROSOL COMPOSITION; FLUX RADIATION; NORTH-AMERICA; EMISSIONS; BASIN; PARTICLES; EVOLUTION; QUALITY;
D O I
10.5194/acp-9-9599-2009
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Large sulfur dioxide plumes were measured in the Mexico City Metropolitan Area (MCMA) during the MILAGRO field campaign. This paper seeks to identify the sources of these plumes and the meteorological processes that affect their dispersion in a complex mountain basin. Surface measurements of SO2 and winds are analysed in combination with radar wind profiler data to identify transport directions. Satellite retrievals of vertical SO2 columns from the Ozone Monitoring Instrument (OMI) reveal the dispersion from both the Tula industrial complex and the Popocatepetl volcano. Oversampling the OMI swath data to a fine grid (3 by 3 km) and averaging over the field campaign yielded a high resolution image of the average plume transport. Numerical simulations are used to identify possible transport scenarios. The analysis suggests that both Tula and Popocatepetl contribute to SO2 levels in the MCMA, sometimes on the same day due to strong vertical wind shear. During the field campaign, model estimates suggest that the volcano accounts for about one tenth of the SO2 in the MCMA, with a roughly equal split for the rest between urban sources and the Tula industrial complex. The evaluation of simulations with known sources and pollutants suggests that the combination of observations and meteorological models will be useful in identifying sources and transport processes of other plumes observed during MILAGRO.
引用
收藏
页码:9599 / 9617
页数:19
相关论文
共 62 条
[1]  
[Anonymous], 2004, DISTINGUISHED DISSER
[2]   Physical and chemical properties of the regional mixed layer of Mexico's Megapolis [J].
Baumgardner, D. ;
Grutter, M. ;
Allan, J. ;
Ochoa, C. ;
Rappenglueck, B. ;
Russell, L. M. ;
Arnott, P. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2009, 9 (15) :5711-5727
[3]   On the evolution of aerosol properties at a mountain site above Mexico City [J].
Baumgardner, D ;
Raga, GB ;
Kok, G ;
Ogren, J ;
Rosas, I ;
Báez, A ;
Novakov, T .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D17) :22243-22253
[4]  
Bossert JE, 1997, J APPL METEOROL, V36, P119, DOI 10.1175/1520-0450(1997)036<0119:AIOFRA>2.0.CO
[5]  
2
[6]   Geostatistical solutions for super-resolution land cover mapping [J].
Boucher, Alexandre ;
Kyriakidis, Phaedon C. ;
Cronkite-Ratcliff, Collin .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2008, 46 (01) :272-283
[7]   Sulfur dioxide emissions from Peruvian copper smelters detected by the Ozone Monitoring Instrument [J].
Carn, S. A. ;
Krueger, A. J. ;
Krotkov, N. A. ;
Yang, K. ;
Levelt, P. F. .
GEOPHYSICAL RESEARCH LETTERS, 2007, 34 (09)
[8]   Spatial differences in outdoor PM10 mass and aerosol composition in Mexico City [J].
Chow, JC ;
Watson, JG ;
Edgerton, SA ;
Vega, E ;
Ortiz, E .
JOURNAL OF THE AIR & WASTE MANAGEMENT ASSOCIATION, 2002, 52 (04) :423-434
[9]  
*COM AMB METR, 2008, INV EM ZON METR VALL
[10]   Retrieval of aerosol single scattering albedo at ultraviolet wavelengths at the T1 site during MILAGRO [J].
Corr, C. A. ;
Krotkov, N. ;
Madronich, S. ;
Slusser, J. R. ;
Holben, B. ;
Gao, W. ;
Flynn, J. ;
Lefer, B. ;
Kreidenweis, S. M. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2009, 9 (15) :5813-5827