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 …

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 …

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 …

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 …

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 …

Modern weather and climate models share a common heritage and often even components;
however, they are used in different ways to answer fundamentally different questions. As …

Isolating the Evolving Contributions of Anthropogenic Aerosols and Greenhouse Gases: A New
CESM1 Large Ensemble Community Resource in: Journal of Climate Volume 33 Issue 18 …

Anthropogenic aerosol (AA) forcing has been shown as a critical driver of climate change
over Asia since the mid-20th century. Here we show that almost all Coupled Model …

Many different emission pathways exist that are compatible with the Paris climate
agreement, and many more are possible that miss that target. While some of the most …