Tropospheric ozone determined from aura OMI and MLS: Evaluation of measurements and comparison with the Global Modeling Initiative's Chemical Transport Model

被引:280
作者
Ziemke, J. R. [1 ]
Chandra, S.
Duncan, B. N.
Froidevaux, L.
Bhartia, P. K.
Levelt, P. F.
Waters, J. W.
机构
[1] Univ Maryland Baltimore Cty, Catonsville, MD 21228 USA
[2] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[3] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[4] Royal Netherlands Meteorol Inst, NL-3730 AE De Bilt, Netherlands
关键词
D O I
10.1029/2006JD007089
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[ 1] Ozone measurements from the OMI and MLS instruments on board the Aura satellite are used for deriving global distributions of tropospheric column ozone (TCO). TCO is determined using the tropospheric ozone residual method which involves subtracting measurements of MLS stratospheric column ozone (SCO) from OMI total column ozone after adjusting for intercalibration differences of the two instruments using the convective-cloud differential method. The derived TCO field, which covers one complete year of mostly continuous daily measurements from late August 2004 through August 2005, is used for studying the regional and global pollution on a timescale of a few days to months. The seasonal and zonal characteristics of the observed TCO fields are also compared with TCO fields derived from the Global Modeling Initiative's Chemical Transport Model. The model and observations show interesting similarities with respect to zonal and seasonal variations. However, there are notable differences, particularly over the vast region of the Saharan desert.
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相关论文
共 63 条
[1]   Global modeling of tropospheric chemistry with assimilated meteorology: Model description and evaluation [J].
Bey, I ;
Jacob, DJ ;
Yantosca, RM ;
Logan, JA ;
Field, BD ;
Fiore, AM ;
Li, QB ;
Liu, HGY ;
Mickley, LJ ;
Schultz, MG .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D19) :23073-23095
[2]   Fast-J2: Accurate simulation of stratospheric photolysis in global chemical models [J].
Bian, HS ;
Prather, MJ .
JOURNAL OF ATMOSPHERIC CHEMISTRY, 2002, 41 (03) :281-296
[3]  
BLOOM S, 2005, TECH REP SER GLOBAL, V26
[4]   Elevated ozone in the troposphere over the Atlantic and Pacific oceans in the Northern Hemisphere [J].
Chandra, S ;
Ziemke, JR ;
Tie, XX ;
Brasseur, G .
GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (23) :1-4
[5]   Tropospheric ozone at tropical and middle latitudes derived from TOMS/MLS residual: Comparison with a global model [J].
Chandra, S ;
Ziemke, JR ;
Martin, RV .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D9)
[6]   Tropical tropospheric ozone: Implications for dynamics and biomass burning [J].
Chandra, S ;
Ziemke, JR ;
Bhartia, PK ;
Martin, RV .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2002, 107 (D14) :ACH3-1
[7]  
Chin M, 2002, J ATMOS SCI, V59, P461, DOI 10.1175/1520-0469(2002)059<0461:TAOTFT>2.0.CO
[8]  
2
[9]   Sensitivity of Global Modeling Initiative chemistry and transport model simulations of radon-222 and lead-210 to input meteorological data [J].
Considine, DB ;
Bergmann, DJ ;
Liu, H .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2005, 5 :3389-3406
[10]   A polar stratospheric cloud parameterization for the global modeling initiative three-dimensional model and its response to stratospheric aircraft [J].
Considine, DB ;
Douglass, AR ;
Connell, PS ;
Kinnison, DE ;
Rotman, DA .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D3) :3955-3973