How aerosols and greenhouse gases influence the diurnal temperature range

The GPP P and GPP S metrics illustrate the interplay between the two drivers (the atmospheric component of the radiative forcing, and the surface temperature change) for

We find that the overall climate feedback through chem- istry and aerosols is negative in the sixth Coupled Model Intercomparison Project (CMIP6) Earth system models due to

RCMIP Phase 1 fo- cused on basic comparisons of RCMs with observed global- mean temperature changes, comparisons of RCMs with the global-mean temperature response of

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Based on the above-mentioned tensions, a recommendation for further research is to examine whether young people who have participated in the TP influence their parents and peers in

However, a shift in research and policy focus on the European Arctic from state security to human and regional security, as well as an increased attention towards non-military

Differences between a 1.5 and 2.0 ◦ C warmer climate than 1850 pre-industrial conditions are in- vestigated using a suite of uncoupled (Atmospheric Model Intercomparison Project;

We investigate such nitric acid enhancements resulting from energetic electron precipitation events using a recently developed variant of the Whole Atmosphere Community Climate