My name is Kathi Unglert, and I’m reporting from the EGU 2016 General Assembly as part of the EGU student reporter programme. Below is my second contribution to the Cryosphere Blog – this time about how cryosphere research can have a real impact on people’s lives. Antoni Lewkowicz – he’s famous, according to a comment I overheard in Tuesday’s PICO session on applied geophysics in cryosphere ...[Read More]
The EGU General Assembly, which takes place each year in Vienna, Austria, draws to a close today. Attended by nearly 13,650 participants from 111 countries, with around a third of those being students – a great turn-out for this vital part of the early career scientists (ECS) community! It has been a very productive meeting for the cryosphere division with a huge number and variety of oral ...[Read More]
Ice sheets and glaciers are very visible and much photographed (e.g. here) elements of the Cryosphere but what about the vast, invisible and buried parts? Around a quarter of the land in the Northern hemisphere remains frozen year round, making up a hugely important part of the cryosphere known as permafrost. Permafrost largely exists at high latitudes (e.g. Siberia and the Canadian Arctic) and t ...[Read More]
Hello everyone! My name is Kathi Unglert and I’m a PhD student in volcanology at the University of British Columbia in Vancouver. I will be reporting for the Cryospheric Sciences blog during the upcoming EGU General Assembly as part of the “Student Reporter Programme”. With the meeting only a few days away, I thought I’d put together a quick guide how to make the most out of a whole week of confer ...[Read More]
The colourful graphs above show how the climate changed in the period from 65 to 25 thousand years ago when Earth was experiencing an ice age. A wealth of information on the dynamics of our climate is embedded in the curves, especially how the northern and southern hemisphere interact, and how fast climate can change. The figure represents thousands and thousands of hours of work by scientists, te ...[Read More]
Are you going to the EGU General Assembly in Vienna next week? Check out these events for early career scientists. To remind you when and where all these nice events and activities take place, you can directly view and import them in your electronic calendar (Isn’t it wonderful?! :-)) Social event for Early Career Cryosphere Scientists! If you cannot make it to anything else; make it to our ...[Read More]
A few weeks ago, we focussed our image of the week on very particular parts of Antarctica, which display blue ice at the surface. Today we would like to put the spotlight on an even more extreme chromatic phenomenon : the Fyndið ísjaki Brandari (should be pronounced “/fɪːntɪð/ˈiːsjacɪ /ˈprantaːrɪ/“, even though a bit of phonetics never hurt anyone, for the sake of simplicity this phenomenon ...[Read More]
Today’s Image of the Week shows meltwaters originating from Leverett Glacier pouring over a waterfall in southwest Greenland. We have previously reported on how meItwater is of interest to Glaciologist (e.g. here) but today we are going to delve into how and why Biologists also study these meltwaters and how the cryosphere interacts with biogeochemical cycles in our oceans. Where? Leverett G ...[Read More]
Why? When a river freezes over, it changes the amount of water that flows through the river system. River ice affects many of the world’s largest rivers, and in the Northern Hemisphere, approximately 60% of rivers experience significant seasonal effects. The formation and evolution of river ice changes river discharge and is not only of interest to local ice skating enthusiasts. The variations in ...[Read More]
With today’s image of the week we want to transport you to Patagonia to look at a unique fresh-water calving glacier – Perito Moreno in Argentina. This is a hot topic at the moment as the glacier did something rather unusual yesterday, read on to find out more….. This large glacier (Fig 2, highlighted red) flows down a valley, calving into the southwestern arm of Lago Argentino ...[Read More]
