The Paris Agreement long‐term global temperature goal refers to two global warming levels:
well below 2° C and 1.5° C above preindustrial. Regional climate signals at specific global …

Scientists describe the scale of the risks from unmanaged climate change as potentially
immense. However, the scientific models, because they omit key factors that are hard to …

The primary objective of CFMIP is to inform future assessments of cloud feedbacks through
improved understanding of cloud–climate feedback mechanisms and better evaluation of …

We review the ideas behind the pattern scaling technique, and focus on its value and
limitations given its use for impact assessment and within integrated assessment models …

We investigate the climate feedback parameter α (W m− 2 K− 1) during the historical period
(since 1871) in experiments using the HadGEM2 and HadCM3 atmosphere general …

The equilibrium climate sensitivity (ECS, in K) to\(\hbox {CO} _ {2}\) doubling is a large
source of uncertainty in projections of future anthropogenic climate change. Estimates of …

This paper assesses intermodel spread in the slope of global-mean precipitation change Δ
P with respect to surface temperature change. The ambiguous estimates in the literature for …

Mechanisms behind regional tropical rainfall responses to CO2 forcing are examined in
idealized climate model experiments, traceable to transient forcing scenarios. As previously …

This paper highlights detailed projected changes in rainfall over Thailand for the early (2011–
2040), middle (2041–2070) and late (2071–2099) periods of the 21st century under the …

Abstract Analysis of the available Coupled Model Intercomparison Project Phase 5 models
suggests that sea surface temperature‐forced, atmosphere‐only global warming …