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During the past two decades, the ozone layer has developed a “hole” each winter and spring above the Antarctic continent. Also in cold Arctic winters substantial stratospheric ozone depletion has been measured, although less than in the Antarctic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dris___00893::22928c9b362d0d59925dcc469866b1af
https://hdl.handle.net/1874/1106
https://hdl.handle.net/1874/1106