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 …

Abstract The Laurentide Ice Sheet was the largest global ice mass to grow and decay during
the last glacial cycle (~ 115 ka to~ 10 ka). Despite its importance for driving major changes …

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 …

" Sometime before 15,000 years ago, a band of hunter-gatherers arrived in Northeast Asia.
They continued east, becoming the first people to set foot in the Americas. They soon found …

Abstract The Northern Hemisphere experienced dramatic changes during the last glacial,
featuring vast ice sheets and abrupt climate events, while high northern latitudes during the …

Mountains significantly influence weather and climate on Earth, including disturbed surface
winds; altered distribution of precipitation; gravity waves reaching the upper atmosphere; …

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 …

Ice sheet response to forced changes—such as that from anthropogenic climate forcing—is
closely regulated by two‐way interactions with other components of the Earth system. These …

While the climate evolution of North America during the last deglaciation has received
considerable attention, few detailed model–data comparisons of the deglacial hydroclimate …

Both hydroclimate proxies and modeling studies alike present compelling evidence for
abundant precipitation in southwestern North America and Europe at the Last Glacial …