Last Glacial Maximum (LGM)
The effect of a dynamic soil scheme on the climate of the mid-Holocene and the Last Glacial Maximum
20
Glacial dynamics in pre-Alpine narrow valleys during the Last Glacial Maximum inferred by lowland fluvial records (northeast Italy)
20
Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum
24
Skill and reliability of climate model ensembles at the Last Glacial Maximum and mid-Holocene
13
Reduced oxygenation at intermediate depths of the southwest Pacific during the last glacial maximum
29
Understanding the Australian Monsoon change during the Last Glacial Maximum with a multi-model ensemble
16
Different ocean states and transient characteristics in Last Glacial Maximum simulations and implications for deglaciation
15
New Last Glacial Maximum ice thickness constraints for the Weddell Sea Embayment, Antarctica
17
Reconstructing paleosalinity from δ¹⁸O: Coupled model simulations of the Last Glacial Maximum, Last Interglacial and Late Holocene
41
The simulated climate of the Last Glacial Maximum and insights into the global marine carbon cycle
25
Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments
17
The paleolake of La Larri (Pineta valley, Pyrenees): explanation in the framework of the last glacial maximum in the Pyrenees
20
The impacts of deglacial meltwater forcing on the South Atlantic Ocean deep circulation since the Last Glacial Maximum
12
Low terrestrial carbon storage at the Last Glacial Maximum: constraints from multi-proxy data
31
Transient simulations of the carbon and nitrogen dynamics in northern peatlands: from the Last Glacial Maximum to the 21st century
22
Climate of the Last Glacial Maximum: sensitivity studies and model-data comparison with the LOVECLIM coupled model
20
A community-based geological reconstruction of Antarctic Ice Sheet deglaciation since the Last Glacial Maximum
9
A new global reconstruction of temperature changes at the Last Glacial Maximum
10
Responses of basal melting of Antarctic ice shelves to the climatic forcing of the last glacial maximum and CO2 doubling
25
Climate during the Last Glacial Maximum in the Northern Sawatch Range, Colorado, USA
27