Abstract The Late-Quaternary climate of Beringia remains unresolved despite the region's
role in modulating glacial-interglacial climate and as the likely conduit for human dispersal …

Holocene paleotemperature records from ice-free margins of Greenland suggest
spatiotemporal heterogeneity in the timing of key climate transitions following retreat of the …

Recent climate change in the Arctic has been rapid and dramatic, leading to numerous
physical and societal consequences. Many studies have investigated these ongoing and …

The flux of low-salinity Pacific water (PW) through Bering Strait (BS) weights on the
freshwater budget of the Arctic Ocean, which, in turn, impacts the Atlantic Meridional …

Global hydroclimate significantly differed from modern climate during the mid-Holocene (6
ka) and Last Glacial Maximum (21 ka). Consequently, both periods have been described as …

The Asian summer monsoon (ASM), including the intensity and range limits of it's associated
rainfall belt, is relevant to ecosystems, agriculture, natural hazards and water availability for …

Processes controlling environmental change in the subarctic Pacific Ocean on millennial to
orbital timescales are not well understood. Here we use a 230‐kyr sedimentary record from …

Anthropogenic climate warming is degrading permafrost across Interior Alaska. Information
from past warming events provides long-term perspectives of future trajectories, however …

Svalbard spans large climate gradients, associated with atmospheric circulation patterns
and variations in ocean heat content and sea ice cover. Future precipitation increases are …

Major shifts in hydroclimate have been documented during the last deglacial period and the
Holocene in south‐central Alaska. Rare freshwater calcium carbonate (marl) deposits in …