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 …

Short-lived climate forcers (SLCFs) affect climate and are, in most cases, also air pollutants.
They include aerosols (sulphate, nitrate, ammonium, carbonaceous aerosols, mineral dust …

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 …

Abstract High Mountain Asia (HMA) has experienced a spatial imbalance in water resources
in recent decades, partly because of a dipolar pattern of precipitation changes known as …

The reality of human-induced climate change is unequivocal and exerts an ever-increasing
global impact. Access to the latest scientific information on current climate change and …

Working Group I (WGI) of the Intergovernmental Panel on Climate Change (IPCC) assesses
the current evidence on the physical science of climate change, evaluating knowledge …

During 2010 to 2020, Northeast Pacific (NEP) sea surface temperature (SST) experienced
the warmest decade ever recorded, manifested in several extreme marine heatwaves …

Mineral dust impacts key processes in the Earth system, including the radiation budget,
clouds, and nutrient cycles. We evaluate dust aerosols in 16 models participating in the sixth …

Explaining extreme events of 2014 from a climate perspective Special Supplement to the
Bulletin of the American Meteorological Society Vol. 96, No. 12, December 2015 From A Climate …

The evolving roles of anthropogenic aerosols (AER) and greenhouse gases (GHG) in
driving large-scale patterns of precipitation and SST trends during 1920–2080 are studied …