„observations not taken today are lost forever.“ (Wunsch et al., 2013) The Critical Need for CO2 Measurements Imagine the ocean as a giant lung, breathing in carbon dioxide (CO2) and helping to keep our planet cool. It absorbs about 25% of the CO2 emissions from human activities, playing a crucial role in mitigating the pace of climate change. But what happens when we lose sight of this process? B ...[Read More]
This year, the International Day for Disaster Risk Reduction, observed on October 13th, emphasises the crucial role of education in mitigating disaster risks. In this insightful interview, we have the pleasure of discussing this important topic with Engineer Marina Morando, Programme Director at the CIMA Research Foundation in Italy. She brings extensive research and operational experience in civi ...[Read More]
Are you an Early Career Scientist (ECS) working on the topics of the Geochemistry, Mineralogy, Petrology, and Volcanology (GMPV) division? Do you enjoy engaging with scientific communities and communicating with a broad audience? The GMPV division of the EGU is looking for a new Editor-in-Chief to lead our blog team! On the GMPV Blog, we share scientific insights from the GMPV fields and curiositi ...[Read More]
In 1995, the Caribbean Island of Montserrat was shaken by the beginning of one of the most significant volcanic eruptions in recent history: one that profoundly changed the natural, social and economical landscape of the country. Three decades later, Soufrière Hills Volcano and its legacy of destruction still shape the lives of Montserrat’s people. Join us on the first part of our reportage and fi ...[Read More]
Mid-ocean ridges (MOR) and hotspots are two types of magmatic activity occurring in the ocean. The MORs are typically associated with another tectonic feature—oceanic transform faults. While numerous studies have focused on the interactions within MORs, hotspots, and transform faults, there has been limited research on cases where a hotspot and a transform fault are located at the same end ...[Read More]
When we think of hydropower, its environmental impacts usually comes to mind: the dams that disrupt ecosystems, the water bodies that shift, the surface evaporation that increases, and the greenhouse gases that escape from reservoirs1. Hydropower, for all its clean energy potential, is not without its environmental baggage, whether on local water resources or the global surface water storage. But ...[Read More]
On August 23, 2024, a tragic event unfolded in Kuala Lumpur, Malaysia, when an 8-metre-deep sinkhole opened up on Jalan Masjid India, swallowing Vijayalakshmi Gali, a 48-year-old woman visiting from India [1]. The incident has raised serious concerns about public safety and the integrity of urban infrastructure. A sinkhole is a natural depression or hole that occurs in the ground when the surface ...[Read More]
We are finally back with the 8th edition of Geodesy Campfire – Share Your Research. The Geodesy EGU Campfire Events “Share Your Research” give (early career) researchers the chance to talk about their work. We have two exciting talks; one by Leire Retegui-Schiettekatte and the other by Vipin Kumar Maurya. Below you can find detailed descriptions of their talks. We will have time to network a ...[Read More]
Recently, I was reading about the River Trent in the UK and came across a surprising Shakespeare quote that I thought I would highlight to the geomorphology community . The quote below is from Henry IV (Part 1, act 3, scene 1) where the character ‘Hotspur’ references the meandering River Trent: “Methinks my moiety, north from Burton here, In quantity equals not one of yours: See how this river co ...[Read More]
Summer is coming to an end in the northern hemisphere, and it usually signals the end of the field season – at least in northern Europe. During the field season, we mostly take our absolute gravimeter (we call her Greta) to measure gravity at various locations across Sweden. Occasionally, we even take Greta to other countries – but that’s a story for another time. Who is G ...[Read More]
