Authors
Hubertus Fischer, Katrin J Meissner, Alan C Mix, Nerilie J Abram, Jacqueline Austermann, Victor Brovkin, Emilie Capron, Daniele Colombaroli, Anne-Laure Daniau, Kelsey A Dyez, Thomas Felis, Sarah A Finkelstein, Samuel L Jaccard, Erin L McClymont, Alessio Rovere, Johannes Sutter, Eric W Wolff, Stéphane Affolter, Pepijn Bakker, Juan Antonio Ballesteros-Cánovas, Carlo Barbante, Thibaut Caley, Anders E Carlson, Olga Churakova, Giuseppe Cortese, Brian F Cumming, Basil AS Davis, Anne De Vernal, Julien Emile-Geay, Sherilyn C Fritz, Paul Gierz, Julia Gottschalk, Max D Holloway, Fortunat Joos, Michal Kucera, Marie-France Loutre, Daniel J Lunt, Katarzyna Marcisz, Jennifer R Marlon, Philippe Martinez, Valerie Masson-Delmotte, Christoph Nehrbass-Ahles, Bette L Otto-Bliesner, Christoph C Raible, Bjørg Risebrobakken, María F Sánchez Goñi, Jennifer Saleem Arrigo, Michael Sarnthein, Jesper Sjolte, Thomas F Stocker, Patricio A Velasquez Alvárez, Willy Tinner, Paul J Valdes, Hendrik Vogel, Heinz Wanner, Qing Yan, Zicheng Yu, Martin Ziegler, Liping Zhou
Publication date
2018/7
Source
Nature geoscience
Volume
11
Issue
7
Pages
474-485
Publisher
Nature Publishing Group UK
Description
Over the past 3.5 million years, there have been several intervals when climate conditions were warmer than during the pre-industrial Holocene. Although past intervals of warming were forced differently than future anthropogenic change, such periods can provide insights into potential future climate impacts and ecosystem feedbacks, especially over centennial-to-millennial timescales that are often not covered by climate model simulations. Our observation-based synthesis of the understanding of past intervals with temperatures within the range of projected future warming suggests that there is a low risk of runaway greenhouse gas feedbacks for global warming of no more than 2 °C. However, substantial regional environmental impacts can occur. A global average warming of 1–2 °C with strong polar amplification has, in the past, been accompanied by significant shifts in climate zones and the spatial distribution …
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