Abstract The North American Ice Sheet Complex (NAISC; consisting of the Laurentide,
Cordilleran and Innuitian ice sheets) was the largest ice mass to repeatedly grow and decay …

Surface mass balance (SMB) provides mass input to the surface of the Antarctic and
Greenland Ice Sheets and therefore comprises an important control on ice sheet mass …

The Last Glacial Maximum (LGM,~ 21,000 years ago) has been a major focus for evaluating
how well state-of-the-art climate models simulate climate changes as large as those …

The Last Glacial Maximum (LGM, 21 000 years ago) is one of the suite of paleoclimate
simulations included in the current phase of the Coupled Model Intercomparison Project …

This paper reconstructs the deglaciation of the Laurentide Ice Sheet (LIS; including the
Innuitian Ice Sheet) from the Last Glacial Maximum (LGM), with a particular focus on the …

Abstract The Dansgaard-Oeschger events of the last ice age are among the best studied
abrupt climate changes, yet a comprehensive explanation is still lacking. They are most …

New chronologic and stratigraphic constraints from the Garda morainic amphitheater define
the extension of the last glaciation in the Adige-Sarca system and improve the Alpine LGM …

Abstract Dansgaard–Oeschger (D–O) events, millennial-scale climate oscillations between
stadial and interstadial conditions (of up to 10–15∘ C in amplitude at high northern …

A climate/vegetation model simulates episodic wetter and drier periods at the 21,000-y
precession period in eastern North Africa, the Arabian Peninsula, and the Levant over the …

The last deglaciation was characterized by drastic climate changes, most prominently
melting ice sheets. Melting ice sheets have a significant impact on the atmospheric and …