The Arctic climate system is rapidly transitioning into a new regime with a reduction in the
extent of sea ice, enhanced mixing in the ocean and atmosphere, and thus enhanced …

The Arctic is warming–fast. Microbes in the Arctic play pivotal roles in feedbacks that magnify
the impacts of Arctic change. Understanding the genome evolution, diversity and dynamics …

We used time‐lapse imagery, seismic and audio recordings, iceberg and glacier velocities,
ocean wave measurements, and simple theoretical considerations to investigate the …

We mapped the terminus position for every marine‐terminating glacier in the Northern
Hemisphere for 2000, 2010, and 2020, including the Greenland Ice Sheet, to provide the first …

The floating ice shelf of Petermann glacier interacts directly with the ocean and is thought to
lose at least 80% of its mass through basal melting. Based on three opportunistic ocean …

The first and strongest signs of global-scale climate change exist in the high latitudes of the
planet. Evidence is now accumulating that the Arctic is warming, and responses are being …

Abstract During the International Polar Year (IPY), comprehensive observational research
programs were undertaken to increase our understanding of the Canadian polar cryosphere …

An Analytical Model of Iceberg Drift in: Journal of Physical Oceanography Volume 47 Issue
7 (2017) Jump to Content Jump to Main Navigation Logo Logo Logo Logo Logo Logo …

A structural glaciological description and analysis of surface morphological features of the
Larsen C ice shelf, Antarctic Peninsula, is derived from satellite images spanning the period …

Sea‐ice ice shelves, at the apex of North America (> 80° N), constitute the oldest sea ice in
the Northern Hemisphere. We document the establishment and subsequent stability of the …