Iodine Monoxide and the Relations to Sea Ice - Congrex

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Global observations of IO slant columns IO present only in small amounts � Temporal averaging necessary Anja.Schoenhardt@iup.physik.uni-bremen.de SOLAS-ESA-EGU conference Frascati, 29 Nov – 2 Dec 2011 10
Global observations of IO slant columns • IO above Antarctica • IO in East Pacific upwelling region Anja.Schoenhardt@iup.physik.uni-bremen.de SOLAS-ESA-EGU conference Frascati, 29 Nov – 2 Dec 2011 11
Page 1 and 2: Iodine monoxide and the relations t
Page 3 and 4: Halogens in the Polar Regions Ozone
Page 5 and 6: Important questions and aspects Imp
Page 7 and 8: The satellite instrument SCIAMACHY:
Page 9: Results: IO from SCIAMACHY Anja.Sch
Page 13 and 14: IO above Antarctica Sep/Oct Dec/Jan
Page 15 and 16: IO in Antarctica: relation to sea i
Page 17 and 18: Connection of iodine to the biosphe
Page 19 and 20: Comparison: IO columns and chloroph
Page 21 and 22: Outlook Next steps • Detailed cor
Page 23 and 24: The End Anja.Schoenhardt@iup.physik
Page 25 and 26: transfer to land/ice precipitation
Page 27 and 28: 180° (Max. sea ice extent) 3. Iodi
Page 29 and 30: Vertical columns of iodine monoxide
Page 31 and 32: Vertical columns of IO - AMF studie
Page 33 and 34: The very End (Lizotte, 2001) Primar

Iodine Monoxide and the Relations to Sea Ice - Congrex

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