Arctic amplification (AA)—referring to the enhancement of near-surface air temperature
change over the Arctic relative to lower latitudes—is a prominent feature of climate change …

The concept of feedback is key in assessing whether a perturbation to a system is amplified
or damped by mechanisms internal to the system. In polar regions, climate dynamics are …

In recent decades, the warming in the Arctic has been much faster than in the rest of the
world, a phenomenon known as Arctic amplification. Numerous studies report that the Arctic …

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 Atlantic meridional overturning circulation (AMOC) is a major tip** element in the
climate system and a future collapse would have severe impacts on the climate in the North …

Many feedback loops significantly increase warming due to greenhouse gas emissions.
However, not all of these feedbacks are fully accounted for in climate models. Thus …

This paper describes the main characteristics of CNRM‐CM6‐1, the fully coupled
atmosphere‐ocean general circulation model of sixth generation jointly developed by …

The Arctic is rapidly warming and experiencing tremendous changes in sea ice, ocean and
terrestrial regions. Lack of long-term scientific observations makes it difficult to assess …

Warming in the Arctic has been much faster than the rest of the world in both observations
and model simulations, a phenomenon known as the Arctic amplification (AA) whose cause …

There is growing evidence that the rate of warming is amplified with elevation, such that high-
mountain environments experience more rapid changes in temperature than environments …