Climate models have continued to be developed and improved since the AR4, and many
models have been extended into Earth System models by including the representation of …

More than 40 model groups worldwide are participating in the Coupled Model
Intercomparison Project Phase 6 (CMIP6), providing a new and rich source of information to …

Chemical loss of Arctic ozone due to anthropogenic halogens is driven by temperature, with
more loss occurring during cold winters favourable for formation of polar stratospheric …

In this paper the interplay between tropical cyclones (TCs) and the Northern Hemispheric
ocean heat transport (OHT) is investigated. In particular, results from a numerical simulation …

An observed decline in the Eastern African Long Rains from the 1980s to late 2000s
appears contrary to the projected increase under future climate change. This “Eastern …

Using an observed dataset, we study the changes of surface wind speeds from 1979 to 2016
over the Northern Hemisphere and their impacts on wind power potential. The results show …

Understanding how anthropogenic CO2 emissions will influence future precipitation is
critical for sustainably managing ecosystems, particularly for drought-sensitive tropical …

The ocean has absorbed 41 per cent of all anthropogenic carbon emitted as a result of fossil
fuel burning and cement manufacture,. The magnitude and the large-scale distribution of the …

Surface weather patterns related to 35 major sudden stratospheric warmings (SSWs) in
1958–2010 are analyzed based on reanalysis data. Similar analyses are conducted with …

Anthropogenic carbon dioxide uptake varies across Earth System Models for reasons that
have remained obscure. When varied within a single model, the lateral eddy mixing …