Large volcanic eruptions have a significant impact on the Earth’s climate as aerosols (including sulphur dioxide and water vapour), together with ash are released into the atmosphere and increase the amount of sunlight reflected back into space (the albedo). This increase in reflectance (or decrease in energy absorption) can cause widespread climatic cooling, known as a ‘volcanic winter’. However, ...[Read More]
Imaggeo on Mondays: Vanishing Lakes and Dry Arctic Landscapes
The Koukdjuak Plains (south-west Baffin Island, Canada) form a vast postglacial marine plain that borders the Foxe Basin, an area that has been progressively uplifted due to glacio-isostatic rebound following the end of the last glaciation about 6600 years ago. The weight of glaciers on the Earth’s crust causes the ground to be depressed, which, once the glacier melts, bounces back (at a geologica ...[Read More]
GeoTalk: Xavier Fettweis
Today in GeoTalk, we’re talking to Xavier Fettweis, an award-winning climate scientist from the University of Liège. He tells us about his work on the Greenland ice sheet. First, could you introduce yourself and let us know a bit about your current projects at the University of Liège? As a child, I was already interested by the meteorology thanks to a small weather station installed at my parents’ ...[Read More]
Geosciences Column: Rainfall and Climate – a Dynamic Problem
“Rain is grace; rain is the sky descending to the earth; without rain, there would be no life.” – John Updike Rain quenches the thirst of soils and vegetation, fuelling ecosystems and much of the world’s agriculture. Whether it ruins a day on the beach or destroys a season’s harvest, it makes humans deeply aware of their vulnerability to the vagaries of the atmosphere. It’s important to understand ...[Read More]