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A story about CO2 -fluxes between sea-ice and the atmosphere What’s it all about? Whenever I have had to describe my PhD research project to people outside of my research community, I have always found it useful to use an analogy most people are familiar with, namely beers. Now that I have the full attention …[Read More]
The Tibetan Plateau – area: 2.5 million km2, mean elevation: 4,700 m a.s.l., surrounded by a series of high mountain ranges that are home to some of the world’s highest peaks: Himalayas, Karakoram, Pamir, Kunlun Shan. Considering these characteristics and the unique cultural heritage of Tibet the decision was easy when I was asked if …[Read More]
Surge-type glaciers are the bi-polar member of the family of glacier dynamics. Every now and then they go into a complete fury and nobody really understands why. What are surge-type glaciers? Surge-type glaciers typically go through what we call the “surge cycle”. It is divided into two phases; a long quiescent phase during which the …[Read More]
You’re an early career scientist (ECS), or maybe you mentor one. So you know that we ECS are busy people, with responsibilities ranging from coursework to teaching, research to outreach, and labwork to fieldwork. And now there is this listicle (no, I’m not embarrassed about choosing this format) telling you to make time in your …[Read More]
In the summer of 2014, our group at Aberystwyth University and the University of Cambridge decided to pursue an ambitious but exciting field campaign in West Greenland. The aim was to survey Store Glacier once a day using a fixed-wing unmanned aerial vehicle (UAV) (see photo above for a view from the UAV on its …[Read More]
Hello and welcome to the blog of the EGU Cryosphere Division. This blog aims to spread the enthusiasm for ice in all its forms – from snow, glaciers and ice sheets, to ice crystals, extra-terrestrial ice bodies and isotopic ice composition. The blog will feature stories related to cryospheric research, particularly the latest in fieldwork …[Read More]
