TY  - JOUR
A1  - Wunderling, Nico
A1  - Willeit, Matteo
A1  - Donges, Jonathan Friedemann
A1  - Winkelmann, Ricarda
T1  - Global warming due to loss of large ice masses and Arctic summer sea ice
JF  - Nature Communications
N2  - Several large-scale cryosphere elements such as the Arctic summer sea ice, the mountain glaciers, the Greenland and West Antarctic Ice Sheet have changed substantially during the last century due to anthropogenic global warming. However, the impacts of their possible future disintegration on global mean temperature (GMT) and climate feedbacks have not yet been comprehensively evaluated. Here, we quantify this response using an Earth system model of intermediate complexity. Overall, we find a median additional global warming of 0.43 degrees C (interquartile range: 0.39-0.46 degrees C) at a CO2 concentration of 400 ppm. Most of this response (55%) is caused by albedo changes, but lapse rate together with water vapour (30%) and cloud feedbacks (15%) also contribute significantly. While a decay of the ice sheets would occur on centennial to millennial time scales, the Arctic might become ice-free during summer within the 21st century. Our findings imply an additional increase of the GMT on intermediate to long time scales. The disintegration of cryosphere elements such as the Arctic summer sea ice, mountain glaciers, Greenland and West Antarctica is associated with temperature and radiative feedbacks. In this work, the authors quantify these feedbacks and find an additional global warming of 0.43 degrees C.
Y1  - 2020
U6  - https://doi.org/10.1038/s41467-020-18934-3
SN  - 2041-1723
VL  - 11
IS  - 1
PB  - Nature Publishing Group
CY  - Berlin
ER  -