Radiative effects of ozone on the climate of a Snowball Earth
Some geochemical and geological evidence has been interpreted to suggest that the concentration of atmospheric oxygen was only 1–10 % of the present level in the time interval from 750 to 580 million years ago when several nearly global glaciations or Snowball Earth events occurred. This low con...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2012-12-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/8/2019/2012/cp-8-2019-2012.pdf |