As a result of the 1987 Montreal Protocol and its amendments, the atmospheric loading of
anthropogenic ozone-depleting substances is decreasing. Accordingly, the stratospheric …

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 …

It is well established that anthropogenic chlorine-containing chemicals contribute to ozone
layer depletion. The successful implementation of the Montreal Protocol has led to …

Assessing the environmental impact of agriculture is a key factor towards reducing human
impacts on the food production chain. Because of the growing consumer interest in healthy …

We analyse simulations performed for the Chemistry-Climate Model Initiative (CCMI) to
estimate the return dates of the stratospheric ozone layer from depletion caused by …

Stratospheric ozone and water vapour are key components of the Earth system, and past
and future changes to both have important impacts on global and regional climate. Here, we …

The amended and adjusted Montreal Protocol has continued to reduce emissions and
atmospheric abundances of most controlled ozone-depleting substances. By 2012, the total …

Wheat (Triticum aestivum L.) is a strategic agricultural crop that plays a significant role in
maintaining national food security and sustainable economic development. Increasing …

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 Antarctic ozone hole is decreasing in size but this recovery will be affected by
atmospheric variability and any unexpected changes in chlorinated source gas emissions …