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Climate implications of observed changes in ozone vertical distributions at middle and high latitudes of the northern hemisphere
Author(s) -
Wang WeiChyung,
Zhuang YiCheng,
Bojkov Rumen D.
Publication year - 1993
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/93gl01318
Subject(s) - troposphere , radiative forcing , atmospheric sciences , environmental science , stratosphere , northern hemisphere , context (archaeology) , longwave , climatology , greenhouse gas , forcing (mathematics) , middle latitudes , latitude , southern hemisphere , ozone layer , radiative transfer , climate change , geology , physics , geodesy , paleontology , oceanography , quantum mechanics
Ozone soundings at middle and high latitudes of the Northern Hemisphere during recent decades indicate a decreasing trend in the lower stratosphere and an increasing trend in the troposphere especially at the upper troposphere. Changes in the O 3 vertical distribution can change the radiative forcing (solar and longwave radiation) to the troposphere‐surface system with climate implications. Here, we use the O 3 soundings at seven middle and high latitudes stations to study its variations in the last few decades and discuss the climate implications in the context of increasing other greenhouse gases CO 2 , CH 4 , CFC‐11, CFC‐12 and N 2 O. The results suggest that changes in O 3 vertical distribution can perturb substantially the radiative forcing, in particular at the middle latitudes where the tropospheric increases can induce a positive radiative forcing (warming) with magnitude comparable to that due to increasing these other greenhouse gases.