Key Questions
- How fast will O3 recover at mid- and tropical latitudes?
- Will Antarctic O3 depletion stabilize?
- Will Arctic O3 loss increase?
- At what rate will stratospheric halogen loading continue to decrease?
Temporal evolution of inorganic chlorine content
above Jungfraujoch (upper pannel) and organic chlorine at the Earth
surface.
Objectives
- Continued monitoring of O3, NO2, BrO, Cly/Fy, T, H2O, aerosol/PSC from ground (NDACC) and space
- Homogenisation and consistency of time series
- Identify links between stratospheric O3 and climate changes.
Observations in the GEOmon activity on Stratospheric Ozone & Climate
Workpackages
