Remember Me
Or use your Academic/Social account:


Or use your Academic/Social account:


You have just completed your registration at OpenAire.

Before you can login to the site, you will need to activate your account. An e-mail will be sent to you with the proper instructions.


Please note that this site is currently undergoing Beta testing.
Any new content you create is not guaranteed to be present to the final version of the site upon release.

Thank you for your patience,
OpenAire Dev Team.

Close This Message


Verify Password:
Verify E-mail:
*All Fields Are Required.
Please Verify You Are Human:
fbtwitterlinkedinvimeoflicker grey 14rssslideshare1
Blankenship, James R.; Crutzen, Paul J. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Various photochemical models based upon the infinite-day assumption were investigated. The effect of the deletion of certain of the photochemical reactions was ascertained. An infinite-day model was developed in which none of the photochemical reactions were deleted. A time-dependent model was developed by an integration over the day. This model provided the distribution of the three oxygen allotropes as a function of height, latitude, time-of-day, and meteorological conditions at a given time of year. The results obtained from the time-dependent model were then compared with those from the infinite-day model and the actual observed data. It was found that the departures between the observed data and the infinite-day model were in many cases greater than the differences between the observed data and the time-dependent model. The seasonal phase lag was obtained by an integration over one year. This lag is then shown as a function of time of year and height at a given latitude.DOI: 10.1111/j.2153-3490.1966.tb00222.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • CHAPMAN,S., 1930, A theory of upper atmospheric ozone. Mem. Roy. SOC.8,, pp. 103-126.
    • DUTSCHH, . U., and CARLTON,L. M., 1964, Uniform evaluation of Umkehr observations from the World Ozone Network. Part 11, Summary Supplement, The vertical distribution of ozone. National Center for Atmospheric Research, Boulder, Colorado.
    • HESSTVEDTE,., 1963, On the determination of characteristic times in a pure oxygen atmosphere. Tell=, 16, 1, pp. 82-88.
    • HESSTVEDTE,., 1966, Some characteristics of the oxygen-hydrogenatmosphere. Qeofykke Publikaajoner, 26, No. 1.
    • JOHNSONF.,, 1964, The solar constant. J . Meteor., 11, pp. 431-439.
    • LEOVY,C., 1963, Mesospheric heating and simple models of thermally driven circulation. Doctoral Thesis, M.I.T.
    • LONDONJ,., 1962, Mesosphere dynamics. Final report, New York University. Contract No. AF19 (604)-6492.
    • NICOLETM,., 1960, Properties and constitution. Phyaica of the Upper Atmoqhere, Academic Press, 2, pp. 17-69.
    • OHRINGO,., 1968,The radiation budget of the Str8tOsphere. J . Meteor., 16, pp. 440-460.
    • PLABSG,I., 1966, The influence of the 9 . 6 o~zone band on the atmosphere infra-red cooling r8te. Roy. Met. Soc., 82, pp. 3043.
    • Handbook of Geophysics, 1960. The Macmillan Company, New York, Chapter 8, p. 6.
  • No related research data.
  • No similar publications.

Share - Bookmark

Cite this article

Collected from