Glacial inception through rapid ice area increase driven by albedo and vegetation feedbacks
<p>We present transient simulations of the last glacial inception using the Earth system model CLIMBER-X with dynamic vegetation, interactive ice sheets, and visco-elastic solid Earth responses. The simulations are initialized at the middle of the Eemian interglacial (125 kiloyears before pres...
Main Authors: | M. Willeit, R. Calov, S. Talento, R. Greve, J. Bernales, V. Klemann, M. Bagge, A. Ganopolski |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2024-03-01
|
Series: | Climate of the Past |
Online Access: | https://cp.copernicus.org/articles/20/597/2024/cp-20-597-2024.pdf |
Similar Items
-
Glacial‐Isostatic Adjustment Models Using Geodynamically Constrained 3D Earth Structures
by: M. Bagge, et al.
Published: (2021-11-01) -
The role of regional feedbacks in glacial inception on Baffin Island: the interaction of ice flow and meteorology
by: Birch, Leah, et al.
Published: (2020) -
Asymmetry and uncertainties in biogeophysical climate–vegetation feedback over a range of CO<sub>2</sub> forcings
by: M. Willeit, et al.
Published: (2014-01-01) -
Glacial Inception on Baffin Island: The Interaction of Ice Flow andMeteorology
by: Birch, Leah, et al.
Published: (2018) -
Ice Caps and Ice Belts: The Effects of Obliquity on Ice−Albedo Feedback
by: Rose, Brian E. J., et al.
Published: (2018)