Ozone loss In the Arctic winter 2014/2015

Using a vortex-edge definition based on the location of the steepest gradient in potential vorticity the vortex-averaged ozone depletion for the Arctic winter and spring 2002/2003

Using the tight correlation observed between PSC areas and total vortex ozone deple- tion and taking into account the decreasing amounts of ozone depleting substances, we predict

In this section we apply the CTM-PS technique using both the Pure and Pseudo Pas- sive SLIMCAT CTM results to infer the magnitude of ozone loss inside the Arctic vortex during

Study of the interannual ozone loss and the permeability of the Antarctic polar vortex from aerosol and ozone lidar measurements in Dumont dUrville (66.4°S 140°E) Sophie Godin,

Vortex averaged (ten-day boxcar average) ozone loss estimated from the ground-based (GB) measurements (as listed in the plots) in red, the OMI observations in blue (OMI), the

The ozone trends based on the equivalent effective Antarctic stratospheric chlorine (EEASC) and piecewise linear trend (PWLT) functions for the vortex averaged ground-based, Total

vortex goes hand in hand with a weaker meridional circulation, which means lower temperature and low total ozone inside the polar vortex and higher temperature and high total ozone

A total ozone depletion of 68 Dobson units from 10 December 2002 to 10 March 2003 is derived by the vortex-average method taking into account both diabatic descent of the air masses