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Volumn 301, Issue 5641, 2003, Pages 1886-1889

Particle formation by ion nucleation in the upper troposphere and lower stratosphere

Author keywords

[No Author keywords available]

Indexed keywords

ATMOSPHERIC AEROSOLS; CLOUDS; NUCLEATION; THERMODYNAMICS; TROPOSPHERE; UPPER ATMOSPHERE;

EID: 0141534329     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.1087236     Document Type: Article
Times cited : (218)

References (33)
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    • Materials and methods are available on Science Online.
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    • note
    • Fractional sun exposure is the integrated fraction of time in which an air parcel is exposed to sunlight at solar zenith angles (SZA) <95° over the preceding 5 days. SZA was computed from the time and position of the air parcel during backward trajectory calculations (20).
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    • note
    • H2SO4 to ∼40% of its measured value (table S1), the model simulated a very low number of ultrafine particles (fig. S3). These results are consistent with the sensitivity study (Fig. 3).
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  • 33
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    • note
    • We thank H. Harder, M. Martinez, J. Simpas, and W. H. Brune for providing OH measurements; M. J. Mahoney for tropopause heights; R. Herman and R. May for water vapor measurements; E. R. Lovejoy for providing IIN model calculations and comprehensive discussions; B. C. Daube and C. A. Brock for helpful comments on the manuscript; and P. H. McMurry, D. W. Fahey, T. F. Hanisco, and K. S. Carslaw for useful conversations. The University of Denver research reported here was supported by the Upper Atmosphere Research Program, the Radiation Sciences Program and the Atmospheric Effects of Aviation Project of the NASA Earth Sciences Enterprise.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.