Last Glacial Maximum pattern effects reduce climate sensitivity estimates
Here, we show that the Last Glacial Maximum (LGM) provides a stronger constraint on equilibrium climate sensitivity (ECS), the global warming from increasing greenhouse gases, after accounting for temperature patterns. Feedbacks governing ECS depend on spatial patterns of surface temperature ("pattern effects"); hence, using the LGM to constrain future warming requires quantifying how temperature patterns produce different feedbacks during LGM cooling versus modern-day warming. Combining data assimilation reconstructions with atmospheric models, we show that the climate is more sensitive to LGM forcing because ice sheets amplify extratropical cooling where feedbacks are destabilizing. Accounting for LGM pattern effects yields a median modern-day ECS of 2.4 degrees C, 66% range 1.7 degrees to 3.5 degrees C (1.4 degrees to 5.0 degrees C, 5 to 95%), from LGM evidence alone. Combining the LGM with other lines of evidence, the best estimate becomes 2.9 degrees C, 66% range 2.4 degrees to 3.5 degrees C (2.1 degrees to 4.1 degrees C, 5 to 95%), substantially narrowing uncertainty compared to recent assessments.
document
https://n2t.org/ark:/85065/d7hh6q8h
eng
geoscientificInformation
Text
publication
2016-01-01T00:00:00Z
publication
2024-04-19T00:00:00Z
Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
None
OpenSky Support
UCAR/NCAR - Library
PO Box 3000
Boulder
80307-3000
name: homepage
pointOfContact
OpenSky Support
UCAR/NCAR - Library
PO Box 3000
Boulder
80307-3000
name: homepage
pointOfContact
2025-07-10T20:02:46.870098