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Studies in atmospheric ozone

Abstract:

It has been known for many years that the variations, annual and day-to-day, in total ozone are caused by air movements in the stratosphere. To follow these air movements in detail, it is essential to measure the vertical distribution of ozone in the atmosphere.

To date, only one instrument has been capable of measuring the fine structure of the ozone distribution. This is the transmogrifier developed by Brewer and Milford (1960). Unfortunately it is complicated in construction and ...

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Peer review status:
Peer reviewed

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Department:
University of Oxford
Role:
Author
Type of award:
DPhil
Level of award:
Doctoral
Awarding institution:
University of Oxford
UUID:
uuid:3f41b693-92df-4d7d-8164-31d5d75d45e7
Local pid:
polonsky:9:45
Source identifiers:
601870516
Deposit date:
2017-10-05

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