CL
Climate: Past, Present & Future

Climate: Past, Present & Future

Generation #polarprediction

Generation #polarprediction

More than 11 years ago, I joined the Université catholique de Louvain (UCLouvain) in Belgium as a teaching assistant. The 2007-2009 International Polar Year (IPY), a worldwide collaborative effort aiming at better understanding our polar regions, had just finished, and the scientific community was concerned about the sudden drop in the summer Arctic sea ice extent that had occurred two years befor ...[Read More]

Presenting a new European loess map

Presenting a new European loess map

Loess is a silt-sized, aeolian sediment that was produced in large quantities in past geological eras of mid-latitude Europe and Asia, among others (Fig. 1). It is used in Quaternary science to infer about past climatic and environmental conditions. Generally, layers of loess formed during cold and dry periods, while soils formed within/on top the loess during warmer and wetter periods. These soil ...[Read More]

Reconstructing ice sheets and topography of the past

Reconstructing ice sheets and topography of the past

  One of the most profound consequences of past climate changes are the geologically rapid (<100,000 year) changes in global topography. For thousands of years, large ice sheets, similar to what currently exists in Greenland and Antarctica, waxed and waned on North America and Europe. Only 20,000 years ago, if you were sitting in the middle of Canada or Sweden, you would be under thousands ...[Read More]

New metric to interpret linear trends from short time series: Trend to variability ratio (TVR)

New metric to interpret linear trends from short time series: Trend to variability ratio (TVR)

  Availability of good quality data is essential to deduce meaningful information in all disciplines of science and technology. This statement is especially relevant in climate research, which is under constant scrutiny from sceptics. In order to better understand the Earth system response to the ongoing anthropogenic global warming, we require global observations of climate indicators at ver ...[Read More]