DOCUMENT RESOURCES FOR EVERYONE
Documents tagged
Documents Plans for the 2010 WMO/UNEP Assessment of ozone Depletion Ozone Research Managers Meeting, Geneva,.....

Slide 1Plans for the 2010 WMO/UNEP Assessment of ozone Depletion Ozone Research Managers Meeting, Geneva, Switzerland May 19, 2008 2010 WMO/UNEP Assessment Co-chairs: Ayité-Lô…

Documents Ozone Data Assimilation K. Wargan S. Pawson M. Olsen A. Douglass P.K. Bhartia J. Witte Global...

Slide 1 Ozone Data Assimilation K. Wargan S. Pawson M. Olsen A. Douglass P.K. Bhartia J. Witte Global Modeling and Assimilation Office Slide 2 Motivation and challenges …

Documents Impact of Pollutants on the Ozone Layer *ozone observations *the ‘Ozone Hole’ *Heterogeneous...

Slide 1 Impact of Pollutants on the Ozone Layer *ozone observations *the ‘Ozone Hole’ *Heterogeneous chemistry *global ozone depletion Dr Tony Cox ERCA 2004 -Lecture…

Documents AOPC-20 (2015)Atmos. Comp. JH Butler Atmospheric Composition Issues James H. Butler Global...

Slide 1 Atmospheric Composition Issues James H. Butler Global Monitoring Division, NOAA/ESRL Boulder, CO, USA WMO Global Atmosphere Watch, Geneva, CH AOPC-20, March 17-21,…

Documents Matthew Cooper, Randall Martin Dalhousie University Bastien Sauvage Universit é de Toulouse, CNRS

Evaluation of Tropical Upper Tropospheric Ozone from ACE-FTS and MAESTRO; Estimation of Ozone Production Efficiency Matthew Cooper, Randall Martin Dalhousie University Bastien…

Documents Ozone Data Assimilation

Slide 1 Ozone Data Assimilation K. Wargan S. Pawson M. Olsen A. Douglass P.K. Bhartia J. Witte Global Modeling and Assimilation Office Motivation and challenges Ozone is…

Documents Enhanced Tropospheric Ozone and the Arabian Anti-Cyclone (or the “Middle east ozone maximum?”)

Enhanced Tropospheric Ozone and the Arabian Anti-Cyclone (or the “Middle east ozone maximum?”) John Worden1, Jane Liu2, Dylan Jones2, Kevin Bowman1, Helen Worden3, Ming…

Documents Chapter 8: Natural Variability of Stratospheric Ozone

preamble.indd8.1 Introduction Stratospheric ozone is known to vary in response to a number of natural factors, such as the seasonal and the 11-year cycles in solar irradiance,