CL
Climate: Past, Present & Future

Climate of the Present

Open climate science is brave climate science

Open climate science is brave climate science

Why are we climate scientists? For us, there is a number of reasons: we feel a strong bond to nature, we like to solve puzzles and we want to understand the mechanisms of what we see every day.  And – even if it only manifests at the end of a causal chain – we want to contribute to a just and livable world via working in climate science. Thus, due to distant and abstract state funding ...[Read More]

Modelling the heat mitigation effects of blue roofs and green roofs to assess climate change adaptation potentials in dense urban environments

Modelling the heat mitigation effects of blue roofs and green roofs to assess climate change adaptation potentials in dense urban environments

Urban areas often show higher temperatures than their surrounding rural areas, especially during heat events. This phenomenon is called the Urban Heat Island (UHI) effect. The magnitude of the UHI effect is expressed by the absolute temperature difference between the rural and the urban area and can reach more than 10 °C. During past decades, the magnitude of the UHI effect has intensified in many ...[Read More]

Spotlighting the Climate Division’s sessions for EGU24

Spotlighting the Climate Division’s sessions for EGU24

Dear community of climate enthusiasts and EGU lovers, We know that being part of the EGU is not just about staying in the loop with the latest geoscience works – especially when it comes to our all-time favorite realm of sciences: climate sciences 🤩. It is also an amazing opportunity to spark exciting collaborations and expand your network with scientists from all over Europe and the world. EGU is ...[Read More]

The Walker Circulation: what is it and why does it matter

The Walker Circulation: what is it and why does it matter

What is the Walker Circulation? The El Niño Southern Oscillation, or ‘ENSO’, is one of the major causes of year to year variability in Earth’s climate. ENSO is characterised by: changes in the temperature of the ocean’s surface in the tropical Pacific Ocean, and by changes in atmospheric circulation in an east-west direction above the Pacific Ocean.   Number two in that list is what makes ENS ...[Read More]