CR
Cryospheric Sciences

Did you know?

Did you know… about the fluctuating past of north-east Greenland?

November 8, 2019
Did you know… about the fluctuating past of north-east Greenland?
Fig. 1: Map of the north-east sector of Greenland showing the location of the North East Greenland Ice Stream (NEGIS) with its three outlet glaciers (Nioghalvfjerdsfjorden (79N), Zachariae Isstrøm (ZI) and Storstrømmen Glacier (SG)), and the offshore bathymetry and the position of its margin reconstructed for the Last Glacial Maximum (LGM) (dotted black line) [Credit: Ilaria Tabone].

Recent geological data shows that during a very cold phase of our Earth’s climate (between 40,000 and 26,000 years ago), there was a huge expansion of polar ice sheets, yet the north-eastern part of the Greenland ice sheet was less extensive than today. How could this have occurred? In this post we shed light on the potential causes of this ice sheet behaviour. What do we know about present- ...[Read More]

Did you know? – Proglacial lakes accelerate glacier retreat!

October 18, 2019

In a global context, New Zealand’s small mountain glaciers often get overlooked and yet they are a beautiful part of New Zealand’s landscape. They are the water towers for the South Island and an essential part of its tourism, thanks to a few undeniable heroes (Frans Josef and Fox Glaciers), but sadly, they may not be as prominent in the future. In this post we review the state of modern glaciatio ...[Read More]

Did you know? – Storms can make Arctic sea ice disappear even faster

July 19, 2019
Did you know? – Storms can make Arctic sea ice disappear even faster
Fig. 1: The difficulties of in-situ observations on sea ice. Winter storm has broken up an ice floe that was only hours ago more than a kilometer wide into small pieces. Scientists are climbing over cracks and rescuing the equipment [Credit: Tor Ivan Karlsen, Norwegian Polar Institute].

The increase in air and water temperature due to climate change drives the retreat in the Arctic sea-ice cover. During summer, when sunlight reaches the Arctic, the absorption of heat by the dark ocean water enhances the sea-ice melt through the ice-albedo feedback. During winter, when sunlight does not reach the Arctic, another feedback is at work, as storms enhance the energy transfer between ai ...[Read More]