CR
Cryospheric Sciences

permafrost

End-of-the-year special: this year’s Cryoblog

End-of-the-year special: this year’s Cryoblog

So this is the last post in 2022 for our blog. We have decided that this time, the topic will not be another exciting story about the science of ice and cold in their various forms. This time we are talking about the blog itself, so a kind of meta-post to take stock and understand …[Read More]

The intriguing order of cold terrains

The intriguing order of cold terrains

Do you know what the periglacial environment is? Well, the word periglacial refers to those environments which are somehow sculpted by seasonal freeze and thaw cycles. The alternation of freezing and thawing conditions can change the landscape, creating some spectacular landforms. Stone circles are certainly among the most mysterious and fascinating. Come and discover them! …[Read More]

You left us too early: a eulogy to permafrost

You left us too early: a eulogy to permafrost

Most problems faced in research are complex and require creativity and critical thinking. Thus, we need to be creative in science! Or maybe, science itself is creative and there is no such thing as non-creative science. Anyhow, in today’s world, where TED-talks, science slams and elevator pitches, not to mention tweets, are ubiquitous, it is …[Read More]

Climatic drivers of permafrost mounds in North American peatlands

Climatic drivers of permafrost mounds in North American peatlands

Permafrost, or perennially frozen, peatlands are among the world’s largest terrestrial carbon stores and are particularly threatened by warming climates. Understanding how modern climate controls the distribution of permafrost peatlands is crucial for making confident predictions of their past and future extents. What are permafrost peatlands? Peatlands are wetlands that develop where cold, wet conditions …[Read More]

Did you know… about the ice content in mountain permafrost?

Did you know… about the ice content in mountain permafrost?

Through the eyes of a researcher studying mountain processes in the European Alps in the context of a global warming climate, let’s discover how geophysical methods help to better understand frozen ground! Permafrost defines a thermal state, i.e. permafrost is soil, sediment, or rock that remains at or below 0°C during at least two consecutive …[Read More]