Are you starting your studies in cryospheric sciences, or are coming into our field from another subject? If so, you may have unsuspectingly waded into a (very thick) soup of acronyms! Don’t fret–here is your “one stop shop” that tells you where to look for more information! Early Career Organisations Unless you’re fortunate enough to be working in a polar-oriented institute (some of our previous ...[Read More]
We’ve spent a lot of time in the past talking about imposter syndrome, coping with the stresses of academic life and how to make sure you’re looking after yourself. Today though, it’s time for a little practical advice. As a new PhD researcher, Felix has been feeling like he’s been thrown in the deep end and is desperately trying to catch up. However, he feels like it is ta ...[Read More]
Dr. Anouk Beniest, an Assistant Professor in Tectonics at the Vrije Universiteit Amsterdamat, is an interdisciplinary earth scientist, bringing together geology, geophysics and geodynamics to help us understand complex geological problems. Her research revolves predominantly around plate tectonics, with a focus on extensional systems and she has kindly put together this blog post to convince you t ...[Read More]
Imagine it is your first time going on a field trip. After spending hours in the lecture theatre, you are excited to get outside and see those environmental processes that so far you have only seen in graphs and figures. You get off the bus, and the first thing your professor says is: “people less comfortable with climbing on the rocks can just take the notes”, while looking at you and your femal ...[Read More]
As academics, a lot of our time is invested in activities that are not seemingly related to our research. Teaching, organising seminars, writing EGU blog posts, reviewing papers. While I don’t deny the time consumingness of it, reviewing papers is a necessary and useful activity, at least as long as the publishing system works the way it currently does (that’s a topic for another post) ...[Read More]
Hidden beneath the surface of ice sheets lies an intricate structure carrying a unique fingerprint of past ice flow and climate conditions. Disentangling the drivers of an ice sheet’s enigmatic stratigraphy could theoretically unravel the ice sheet’s past evolution and provide a much clearer picture of things to come in the future. One way to detect this mysterious stratigraphy is to use ice-penet ...[Read More]
On October 23 2022, a tornado outbreak occurred in France, causing extensive damages. Tornadoes in France are a relatively rare phenomenon, even more so in the second half of October. This weather phenomenon is linked to intense thunderstorms, and it is difficult to predict because it is very localized. Will global warming make this weather more frequent or intense? A thundercloud that grows visib ...[Read More]
Emergence of the field of molecular paleoecology Sequencing DNA of organisms that died a long time ago sounds like the synopsis of the movie Jurassic Park (1993). Let’s make it clear right now, dinosaur DNA has never been collected by humans. To date, the oldest DNA recovered is more than one million years old and comes from mammoths. In addition to the DNA recovered from fossils, aquatic and terr ...[Read More]
Have you ever wondered to learn more about the geological setting of the Nevado volcano in Central-West Argentina? In this week’s blog, we have Georgina Rubiano Lorenzoni, a Ph.D. Geologist student from the Universidad Nacional de La Pampa in Argentina, who will guide us through her thesis aims, which are the identification and investigation of the petrogenesis and geochronology of the mountain ra ...[Read More]
Every natural event that causes damage to the built environment must be followed by recovery; however, this phase of disaster risk management has received less attention from academics than the others [1]. In all its aspects, disaster recovery has remained a contentious topic, with experts debating its definition, approaches, objectives, activities, and even when it should begin and finish [2–4]. ...[Read More]
