Maxwell Kelley

TL;DR: The authors used numerical climate simulations, paleoclimate data, and modern observations to study the effect of growing ice melt from Antarctica and Greenland and found that ice mass loss from the most vulnerable ice, sufficient to raise sea level several meters, is better approximated as exponential than by a more linear response.

TL;DR: Simulation characteristics from eighteen global ocean-sea-ice coupled models are presented with a focus on the mean Atlantic meridional overturning circulation (AMOC) and other related fields in the North Atlantic as discussed by the authors.

TL;DR: In this paper, the authors investigate the issue of "dangerous human-made interference with climate" using simulations with GISS modelE driven by measured or estimated forcings for 1880-2003 and extended to 2100 for IPCC greenhouse gas scenarios as well as the "alternative" scenario of Hansen and Sato (2004).

TL;DR: This article carried out climate simulations for 1880-2003 with GISS modelE driven by ten measured or estimated climate forcings and compared side-by-side simulated climate change for each forcing, all forcings, observations, unforced variability among model ensemble members and, if available, observed variability.

TL;DR: In this article, the authors use numerical climate simulations, paleoclimate data, and modern observations to study the effect of growing ice melt from Antarctica and Greenland, and hypothesize that ice mass loss from the most vulnerable ice is better approximated as exponential than by a more linear response.