and convective initiation mechanisms. In a future campaign, we hope to further study dryline formation (incl. land surface processes) and dryline fine-scale dynamics. Boundary-layer circulations over ...

The early stage of these storms, known as convective initiation (CI), can be monitored using geostationary satellites.

Several other key problems in the fields of mesoscale and boundary-layer dynamics are being explored using state-of-the-art observations, including stratified flow over complex terrain, coherent ...