Differences in Arctic and Antarctic PSC occurrence as observed by lidar in Ny-Ålesund (79° N, 12° E) and McMurdo (78° S, 167° E)

The extent of springtime Arctic ozone loss does not reach Antarctic ``ozone hole' dimensions because of the generally higher temperatures in the northern hemisphere vortex and consequent less polar stratospheric cloud (PSC) particle surface for heterogeneous chlorine activation. Yet, with incre...

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Bibliographic Details
Published in:Atmospheric Chemistry and Physics
Main Authors: Maturilli, M., Neuber, R., Massoli, P., Cairo, F., Adriani, A., Moriconi, M. L., Donfrancesco, G.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/acp-5-2081-2005
https://www.atmos-chem-phys.net/5/2081/2005/