Global warming particularly impacts terrestrial and aquatic ecosystems in the Arctic. To
constrain the sensitivity of Arctic lakes and make meaningful predictions about future change …

Higher boreal summer insolation in the early to middle Holocene drove thousands of years
of summer warming across the Arctic. Modern-day warming has distinctly different causes …

The number of Arctic glaciers with direct, long-term measurements of mass balance is
limited. Here we used satellite-based observations of the glacier snowline altitude (SLA), the …

Alpine glaciers are sensitive responders to climate fluctuations, especially to changes in
summer temperature, and thus their past extents are invaluable indicators of past climate …

Three paleosols buried in the left lateral moraines of the Greater Azau Glacier (Northern
Caucasus) were identified in an excavated outcrop (43.2658 N, 42.4766 E, 2370 m asl) …

The recent retreat of nearly all glaciers and ice caps (GICs) located in Arctic regions is one of
the most clear and visible signs of ongoing climate change. This paper synthesizes …

The timing of mountain glacier fluctuations is poorly constrained in some parts of Greenland
during the Late Holocene. We present 31 10Be cosmic‐ray exposure ages (CRE) of …

Abstract The Greenland Ice Sheet (GrIS) is a key component of the global climate system.
However, our current understanding of the spatio-temporal oscillations and landscape …

Greenlandic fjords, located between the ice sheet and the ocean, are dynamic systems that
can sustain highly variable levels of primary productivity and are sensitive to climate change …

Although the spatiotemporal oscillations of the Greenland Ice Sheet (GrIS) during the last
millennia have played a prominent role in global environmental changes, its glacial …