CL
Climate: Past, Present & Future

aeolian transport

Winds of change – How can we reconstruct the directions of winds in the past?

Winds of change – How can we reconstruct the directions of winds in the past?

Invited guest from the EGU 2025 Outstanding Student and PhD candidate Presentation (OSPP) Award Wind is not easily visible. On historical time scales, its directions and velocities have been measured and recorded by instruments. To some degree, these parameters can also be simulated by climate models. But how about winds in the more distant past? And why would we want to know about them? In many p ...[Read More]

Desert loess: formation, distribution, geoscientific value

Desert loess: formation, distribution, geoscientific value

Loess is an aeolian (wind-driven) silty sediment covering over 10% of the Earth’s land surface; it occurs predominantly in the mid-latitudes. On a global scale, loess is among the most widespread unconsolidated sediments, and of crucial importance for agricultural regions where loess deposits are known to form fertile soils because of its ability to store water and retain nutrients. Loess is compr ...[Read More]