Assessing the inherent uncertainties in satellite data products is a challenging task. Different
technical approaches have been developed in the Earth Observation (EO) communities to …

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 …

We describe the construction of a continuous 38-year record of stratospheric aerosol optical
properties. The Global Space-based Stratospheric Aerosol Climatology, or GloSSAC …

In this paper, we describe the construction of the Stratospheric Water and Ozone Satellite
Homogenized (SWOOSH) database, which includes vertically resolved ozone and water …

Ozone profile trends over the period 2000 to 2016 from several merged satellite ozone data
sets and from ground-based data measured by four techniques at stations of the Network for …

The assimilated ozone product from the Modern-Era Retrospective Analysis for Research
and Applications, version 2 (MERRA-2), produced at NASA's Global Modeling and …

After decades of depletion in the 20th century, near-global ozone now shows clear signs of
recovery in the upper stratosphere. The ozone column, however, has remained largely …

Trends in the vertical distribution of ozone are reported and compared for a number of new
and recently revised data sets. The amount of ozone-depleting compounds in the …

The ozone profile records of a large number of limb and occultation satellite instruments are
widely used to address several key questions in ozone research. Further progress in some …

The stratospheric circulation determines the transport and lifetime of key trace gases in a
changing climate, including water vapor and ozone, which radiatively impact surface …