Ozone forms in the Earth's atmosphere from the photodissociation of molecular oxygen,
primarily in the tropical stratosphere. It is then transported to the extratropics by the Brewer …

Climate models robustly project acceleration of the Brewer‐Dobson circulation (BDC) in
response to climate change. However, the BDC trends simulated by comprehensive models …

We have analyzed near-global stratospheric data (and mesospheric data as well for H 2 O)
in terms of absolute abundances, variability, and trends for O 3, H 2 O, HCl, N 2 O, and HNO …

There is evidence that the ozone layer has begun to recover owing to the ban on the
production of halogenated ozone-depleting substances (hODS) accomplished by the …

A comprehensive analysis of the temporal evolution of tropospheric ozone in Antarctica
using more than 25 years of surface ozone and ozonesonde measurements reveals …

The polar vortex is a strong jet of westerly wind which forms each winter around the polar
stratosphere. Sometimes, roughly every other winter, the polar vortex in the Northern …

This article describes the volcanic effect of the Mt Pinatubo eruption in June 1991 on the
ozone (O 3) and methane (CH 4) distribution in the stratosphere, as simulated with the …

To simulate the impacts of volcanic eruptions on the stratosphere, chemistry–climate models
that do not include an online aerosol module require temporally and spatially resolved …

The solar cycle (SC) stratospheric ozone response is thought to influence surface weather
and climate. To understand the chain of processes and ensure climate models adequately …

Abstract The tropical Madden–Julian oscillation (MJO) excites a northward propagating
Rossby wave train that largely determines the extratropical surface weather consequences …