European Geoscience Union (EGU) is an organisation made of different disciplines in geosciences, and each disciplines have their own Division. Within each Division, there are many different volunteered positions. Each year at the EGU General Assembly (a conference), Division members come together to nominate members for those positions. There are variety of positions from President and Deputy Pres ...[Read More]
A modern take on the 19th-century scientific expeditions: cruise MSM104/1
Figure 1. Sunset onboard RV Maria S Merian (Photo: Eduardo Queiroz Alves).
“Every ship that navigates the high seas, with these charts and blank abstract logs on board, may henceforth be regarded as a floating observatory, a temple of science.” – Matthew Fontaine Maury This is a joint post, published together with the climate sciences division blog and the ocean sciences division blog. The ocean has always been important for humanity, with trade and war being just ...[Read More]
Land snails in the service of paleoecological studies
Paleoecological use of land snail shells is no longer a new field of science. They are studied by malacologists and palaeontologists who specialise in the study of molluscs. During the last glaciation, loess, a light yellow, fine-grained sediment, was deposited over large areas, mainly in the periglacial regions of Eurasia and North America. In addition to its many advantages, it has also provided ...[Read More]
How glaciers record the winds of change
Primary downlink station for the Gravity Recovery and Climate Experiment (GRACE) and GRACE-Follow On satellite data in Ny-Ålesund, a town in Svalbard, operated as crucial part of the Ground Data System by the Helmholtz Centre Potsdam German Research Center for Geosciences for the joint mission with the NASA Jet Propulsion Laboratory. Source: Carsten Falck from the German Research Center for Geosciences.
After decades of observation, one of the profound consequences of anthropogenic global warming is the rapid rise in temperature in the Arctic, refered to as Arctic Amplification. Compared to the mid-latitudes, warming in the Arctic is twice as fast. The reason is mainly due to the positive feedback of a melting cryosphere: Darker surfaces are revealed from melting cryosphere, reflecting less short ...[Read More]