Tropospheric anthropogenic aerosols contribute the second-largest forcing to climate
change, but with high uncertainty owing to their spatio-temporal variability and complicated …

Globally, thermodynamics explains an increase in atmospheric water vapor with warming of
around 7%/° C near to the surface. In contrast, global precipitation and evaporation are …

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 …

Most climate change detection and attribution studies have focused on mean or extreme
temperature or precipitation, neglecting to explore long-term changes in drought …

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

The effect of an increase in atmospheric aerosol concentrations on the distribution and
radiative properties of Earth's clouds is the most uncertain component of the overall global …

Monsoon rainfall has profound economic and societal impacts for more than two-thirds of the
global population. Here we provide a review on past monsoon changes and their primary …

Although anthropogenic climate change is expected to have caused large shifts in
temperature and rainfall, the detection of human influence on global drought has been …

Despite the pervasive impact of drought on human and natural systems, the large-scale
mechanisms conducive to regional drying remain poorly understood. Here we use a …

Challenges in Quantifying Changes in the Global Water Cycle in: Bulletin of the American
Meteorological Society Volume 96 Issue 7 (2015) Jump to Content Jump to Main Navigation …