Aircraft-Based Measurements of the Carbon Footprint of Indianapolis

被引:140
作者
Mays, Kelly L. [1 ]
Shepson, Paul B. [1 ,2 ]
Stirm, Brian H. [3 ]
Karion, Anna [4 ]
Sweeney, Colm [4 ]
Gurney, Kevin R. [1 ,5 ]
机构
[1] Purdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47907 USA
[2] Purdue Univ, Dept Chem, W Lafayette, IN 47906 USA
[3] Purdue Univ, Dept Aviat Technol, W Lafayette, IN 47907 USA
[4] Natl Ocean & Atmospher Adm, Boulder, CO 80305 USA
[5] Purdue Univ, Dept Agron, W Lafayette, IN 47907 USA
关键词
ATMOSPHERIC METHANE; CO2; FLUXES; URBAN; EMISSIONS; DIOXIDE; VARIABILITY; POLLUTANTS; TURBULENCE; AIRBORNE; FOSSIL;
D O I
10.1021/es901326b
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The quantification of greenhouse gas emissions requires high precision measurements made with high spatial resolution. Here we describe measurements of carbon dioxide (CO2) and methane (CH4) conducted using Purdue University's Airborne Laboratory for Atmospheric Research (ALAR), aimed at the quantification of the "footprints" for these greenhouse, gases for Indianapolis, IN. A cavity ring-down spectrometer measured atmospheric concentrations, and flask samples were obtained at various points for comparison. Coupled with pressure, temperature, and model-derived horizontal winds, these measurements allow for flux estimation. Long horizontal transacts were flown perpendicular to the wind downwind of the city. Emissions were calculated using the wind speed and the difference between the concentration,in the plume and the background concentration. A kriging method is applied to interpolate the measured values to a vertical plans traced out by the flight pattern within the mixed layer. Results show the urban plume is clearly distinguishable in the downwind concentrations for most-flights, Additionally, there is large variability in the measured day-to-day emissions fluxes as well as in the relative CH4 and CO2 fluxes. Uncertainties in the method are discussed, and its potential utility in determining sector-based emission factors is shown.
引用
收藏
页码:7816 / 7823
页数:8
相关论文
共 38 条
[1]  
ALKEZWEENY AJ, 1977, J APPL METEOROL, V16, P561, DOI 10.1175/1520-0450(1977)016<0561:AMOPOU>2.0.CO
[2]  
2
[3]  
BABBITT CW, 2003, J CLEAN PROD, V13, P903
[4]   Springtime transitions of NO2, CO, and O3 over North America: Model evaluation and analysis [J].
Choi, Yunsoo ;
Wang, Yuhang ;
Zeng, Tao ;
Cunnold, Derek ;
Yang, Eun-Su ;
Martin, Randall ;
Chance, Kelly ;
Thouret, Valerie ;
Edgerton, Eric .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2008, 113 (D20)
[5]  
Chu D., 2004, GLOBEC KRIGING SOFTW, V3rd edn
[6]   A SENSITIVE FAST-RESPONSE PROBE TO MEASURE TURBULENCE AND HEAT-FLUX FROM ANY AIRPLANE [J].
CRAWFORD, TL ;
DOBOSY, RJ .
BOUNDARY-LAYER METEOROLOGY, 1992, 59 (03) :257-278
[7]   Aircraft wind measurement considering lift-induced upwash [J].
Crawford, TL ;
Dobosy, RJ ;
Dumas, EJ .
BOUNDARY-LAYER METEOROLOGY, 1996, 80 (1-2) :79-94
[8]   A cavity ring-down analyzer for measuring atmospheric levels of methane, carbon dioxide, and water vapor [J].
Crosson, E. R. .
APPLIED PHYSICS B-LASERS AND OPTICS, 2008, 92 (03) :403-408
[9]  
Draxler R.R., 2010, HYSPLIT HYBRID SINGL
[10]  
*EM FACT INV GROUP, 1998, COMP AIR POLL EM FAC