News
A new mechanism for synchronising Heinrich events with Dansgaard-Oeschger cycles
The northern hemisphere climate during the last glacial period (about 65,000-15,000 years before present) was dominated by two prominent signals of…
Ocean CO2 measurements: a single sailboat yacht makes a difference
Have you ever wondered how much a single measurement campaign matters when estimating the ocean's carbon sink? In a study published recently in…
What happens after a snowball Earth melts?
When a snowball Earth deglaciates, the planet transitions rapidly into a hot "supergreenhouse" climate that persists for a hundred thousand years or…
Coupled climate models systematically underestimate the radiation response to surface warming
Do climate models realistically represent the coupling between Earth’s surface warming and the top-of-the atmosphere radiation? Dirk Olonscheck,…