North Atlantic Versus Global Control on Dansgaard‐Oeschger Events
Abstract The classic scenario for the generation of Dansgaard‐Oeschger (DO) events assumes a link to changes in the Atlantic Meridional Overturning Circulation (AMOC) induced by North Atlantic freshwater perturbations. Recent proxy data emphasize the existence of leads and lags between DO fingerprin...
Saved in:
| Main Authors: | M. Dima, G. Lohmann, G. Knorr |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Wiley
2018-12-01
|
| Series: | Geophysical Research Letters |
| Subjects: | |
| Online Access: | https://doi.org/10.1029/2018GL080035 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Thermohaline instability and the formation of glacial North Atlantic super polynyas at the onset of Dansgaard‐Oeschger warming events
by: Guido Vettoretti, et al.
Published: (2016-05-01) -
Atmospheric and Oceanic Pathways Drive Separate Modes of Southern Hemisphere Climate in Simulations of Spontaneous Dansgaard‐Oeschger‐Type Oscillations
by: Irene Trombini, et al.
Published: (2025-03-01) -
The Impact of CO2 and Climate State on Whether Dansgaard–Oeschger Type Oscillations Occur in Climate Models
by: Irene Malmierca‐Vallet, et al.
Published: (2024-07-01) -
Controls on Cyclic Formation of Quaternary Early Diagenetic Dolomite
by: J. McCormack, et al.
Published: (2018-04-01) -
Shifts in Greenland interannual climate variability lead Dansgaard–Oeschger abrupt warming by hundreds of years
by: C. A. Brashear, et al.
Published: (2025-02-01)