Chemical data assimilation estimates of continental US ozone and nitrogen budgets during the Intercontinental Chemical Transport Experiment-North America

被引:87
作者
Pierce, Robert B. [1 ]
Schaack, Todd
Al-Saadi, Jassim A.
Fairlie, T. Duncan
Kittaka, Chieko
Lingenfelser, Gretchen
Natarajan, Murali
Olson, Jennifer
Soja, Amber
Zapotocny, Tom
Lenzen, Allen
Stobie, James
Johnson, Donald
Avery, Melody A.
Sachse, Glen W.
Thompson, Anne
Cohen, Ron
Dibb, Jack E.
Crawford, Jim
Rault, Didier
Martin, Randall
Szykman, Jim
Fishman, Jack
机构
[1] NASA, Langley Res Ctr, Hampton, VA 23681 USA
[2] Univ Wisconsin, Ctr Space Sci & Engn, Madison, WI 53706 USA
[3] Sci Applicat Int Corp, Washington, DC 20591 USA
[4] Penn State Univ, Dept Meteorol, University Pk, PA 16802 USA
[5] Univ Calif Berkeley, Dept Chem, Berkeley, CA 94720 USA
[6] Univ New Hampshire, Dept Earth Sci, Durham, NH 03824 USA
[7] Dalhousie Univ, Dept Phys & Atmospher Sci, Halifax, NS B3H 4R2, Canada
[8] US EPA, Raleigh, NC USA
关键词
D O I
10.1029/2006JD007722
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] Global ozone analyses, based on assimilation of stratospheric profile and ozone column measurements, and NOy predictions from the Real-time Air Quality Modeling System (RAQMS) are used to estimate the ozone and NOy budget over the continental United States during the July - August 2004 Intercontinental Chemical Transport Experiment - North America (INTEX-A). Comparison with aircraft, satellite, surface, and ozonesonde measurements collected during INTEX-A show that RAQMS captures the main features of the global and continental U. S. distribution of tropospheric ozone, carbon monoxide, and NOy with reasonable fidelity. Assimilation of stratospheric profile and column ozone measurements is shown to have a positive impact on the RAQMS upper tropospheric/lower stratosphere ozone analyses, particularly during the period when SAGE III limb scattering measurements were available. Eulerian ozone and NOy budgets during INTEX-A show that the majority of the continental U. S. export occurs in the upper troposphere/ lower stratosphere poleward of the tropopause break, a consequence of convergence of tropospheric and stratospheric air in this region. Continental U. S. photochemically produced ozone was found to be a minor component of the total ozone export, which was dominated by stratospheric ozone during INTEX-A. The unusually low photochemical ozone export is attributed to anomalously cold surface temperatures during the latter half of the INTEX-A mission, which resulted in net ozone loss during the first 2 weeks of August. Eulerian NOy budgets are shown to be very consistent with previously published estimates. The NOy export efficiency was estimated to be 24%, with NOx + PAN accounting for 54% of the total NOy export during INTEX-A.
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