This chapter assesses simulations of future global climate change, spanning time horizons
from the near term (2021–2040), mid-term (2041–2060), and long term (2081–2100) out to …

The AR5 concluded that human influence on the climate system is clear, evident from
increasing greenhouse gas concentrations in the atmosphere, positive radiative forcing …

Global‐scale changes in water vapor and responses to surface temperature variability since
1979 are evaluated across a range of satellite and ground‐based observations, a reanalysis …

Forcing due to solar and volcanic variability, on the natural side, and greenhouse gas and
aerosol emissions, on the anthropogenic side, are the main inputs to climate models …

We document and evaluate the aerosol schemes as implemented in the physical and Earth
system models, the Global Coupled 3.1 configuration of the Hadley Centre Global …

Hurricanes often cause severe damage and loss of life, and storms that intensify close to the
coast pose a particularly serious threat. While changes in hurricane intensification and …

Abstract Climate change over High Mountain Asia (HMA, including the Tibetan Plateau) is
investigated over the period 1979–2014 and in future projections following the four Shared …

Due to its wide‐ranging impacts, predicting decadal variations of sea surface temperature
(SST) in the subpolar North Atlantic remains a key goal of climate science. Here, we …

Future precipitation changes are typically estimated from climate model simulations, while
the credibility of such projections needs to be assessed by their ability to capture observed …

This paper reviews developments in climate science and hydrological modelling studies in
Zimbabwe over the past 29 years in an effort to expose knowledge gaps within this research …