Twitter is a place that can be full of an overwhelming amount of information, and often it becomes difficult to hear about new information amongst the noise of all the tweeting. To help our fellow cryo-enthusiasts learn more about equality, diversity and accessibility within the cryosphere, we’re highlighting a few twitter accounts that we think everyone should follow! Gender equality: @womeninPol ...[Read More]
Drones are not only a cool toy to play with. They are also a useful instrument to monitor and study glaciers and ice caps. By taking thousands of images flying above the ice, we can make 3D models of ice masses at centimetre resolution. Using drones, we can now survey small to medium sized glaciers and ice caps in unprecedented detail. In recent years, we have conducted several surveys on glaciers ...[Read More]
Every time we walk, ski, drive or build upon snow, we’re relying upon the theory of Snow Mechanics; but what is that and why should we care? Mechanics is the engineering terminology used to describe “the branch of applied mathematics dealing with motion and forces producing motion” (Oxford Languages) or more simply, the study of motion, in our case the motion of snow. What causes snow to move? Ge ...[Read More]
Have you ever wondered what the voice of a glacier sounds like? Well, listen here! And if you want to know how the glacier makes these sounds, then let’s take a walk on the ice side… Close your eyes and think of the time you were in the middle of the mountains. On a snow plain, a glacier or a frozen lake; just you. You hear your footsteps in the snow, crunching ice. The wind blows through your hoo ...[Read More]
Every division within the European Geosciences Union is led by a senior and junior representative, who oversee the happenings within their respective divisions. The senior representative of the Cryosphere Division is Carleen Tijm-Reijmer, who we’ve managed to track down here at EGU! We ask Carleen to explain her role within EGU and the CR Division. Please tell us a little bit about yourself! ...[Read More]
After two (long) years of remote work and virtual conferencing, we are looking forward to engaging with fellow scientists in-person at the upcoming EGU22 General Assembly! But, with Covid-19 still in the air, this year’s conference will be held as a hybrid format. In this way, EGU22 will be modified to comply with Austrian pandemic restrictions, as well as introduce new elements to the programme t ...[Read More]
We have waited eight years for it, and it is finally out: the 6th Assessment Report of the Intergovernmental Panel on Climate Change (a.k.a. « IPCC AR6 »)! And it is more than 10,000 pages long across Working Groups! Fortunately, a synthesis report integrating the findings of all three working groups should be released in Autumn 2022. However, we, at the EGU Cryosphere Blog, thought it might be us ...[Read More]
The beautiful island of Taiwan (as given by its colonial name, Ilha Formosa) is primarily known for its lush tropical forests, delicious culinary cuisine, bubbling hot springs, and a bustling cityscape. But, what does Taiwan have to do with the cryosphere? Before you resist the urge to leave and get a bubble tea, read on to find out about Taiwan’s cryospheric past! From cities to mountains Taiwan ...[Read More]
Central Chile has been facing a long dry period since 2010, marked by a high mean precipitation deficit, a so-called Mega Drought (MD) (Garreaud et al., 2019). This, besides long-term temperature increase (Burger et al., 2018; Falvey & Garreaud, 2009), has affected negatively the glaciers’ mass balance in the region mainly due to low snow accumulation throughout a hydrological year (which is f ...[Read More]
More pancakes in the future – that sounds like a very good New Year’s Eve resolution for Sunday brunches, but it could also be a development of the most tasty looking sea ice shape in the Arctic. Let’s find out more! Arctic Sea Ice The growth and melt of Arctic sea ice follows a seasonal cycle. In the springtime, under the midnight sun, the sea ice begins to melt until it reaches its m ...[Read More]
