Physics & Astronomy ETDs

Publication Date

6-3-1957

Abstract

The Vertical distribution of atmospheric ozone has been determined spectroscopically either from surface observations or from balloon-borne spectrographs sent aloft. These spectrographic techniques have several disadvantages. Surface observations of the "Umkehr Effect" give only a rough distribution, four or five points for the entire atmosphere.

Degree Name

Physics

Level of Degree

Masters

Department Name

Physics & Astronomy

First Committee Member (Chair)

Victor H. Regener

Second Committee Member

Jack Katzenstein

Third Committee Member

John Root Green

Language

English

Document Type

Thesis

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