Past and future polar amplification of climate change: climate model intercomparisons and ice-core constraints

294 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

What caused Earths temperature variations during the last 800,000 years? Data-based evidences on radiative forcing and constraints on climate sensitivity (2009, background): “In this respect one has to bear in mind, that the polar amplification factor is probably not constant in time, e.g. it is estimated to be smaller in scenarios for future climate change (Masson-Delmotte et al., 2006).”
Global characterization of the Holocene Thermal Maximum (2012, background): “However, the high-latitude HTM response is also stronger because of positive feedbacks, the most prominent ones involving snow and ice, contributing to the well-known polar amplification of climate change (e.g., Holland and Bitz, 2003; Masson-Delmotte et al., 2006; Miller et al., 2010b).”
Simulated Antarctic precipitation and surface mass balance at the end of the twentieth and twenty-first centuries (2006, methodology): “This situates the model close to the average of the 4th IPCC assessment report models (Masson-Delmotte et al. 2006).”