Future climate feedbacks
We have simulated a large set of idealized simulations with the Norwegian Earth System Model (NorESM2) to explore the Earth system response to net-zero and net-negative CO2 emissions. Our simulations […]
We have simulated a large set of idealized simulations with the Norwegian Earth System Model (NorESM2) to explore the Earth system response to net-zero and net-negative CO2 emissions. Our simulations […]
Abrupt permafrost thawing is expected to release large amounts of greenhouse gasses to the atmosphere, creating a positive feedback to climate warming. There is, however, still large uncertainty in the […]
In 2012, the Intergovernmental Platform on Biodiversity and Ecosystem Services (IPBES) was established following on the Intergovernmental Panel on Climate Change (IPCC). Since the launch of the first Methodological Assessment […]
Cloud Regimes (CRs), which is a set of dominant mixtures of cloud types represented by the means of similar co-variations of cloud top pressure (CTP) and optical thickness (COT), has […]
Julia language has been in development since 2012 and saw its first stable version in 2018. It is already among the most popular and fastest growing programming languages, specially in […]
We examine the way various temporal and spatial scales of motion interact to impact the evolving ocean/atmosphere system in the tropical Pacific. A major focus is the link between wind […]
Korean Integrated Model (KIM) has been an operational global model at Korea Meteorological Administration (KMA) since government funded 9-year project of developing a next generation global model. The main components […]
Storms and extreme weather events are stronger in the Southern Hemisphere than in the Northern Hemisphere. In this talk I will combine an energetic perspective, observations and climate model simulations […]
Viruses attack marine organisms from bacteria to whales. In particular phytoplankton blooms can crash because of viral infection. Here we will explore the interaction between viruses, phytoplankton and zooplankton under […]
Toward the end of the Pleistocene, archaic humans in Eurasia such as the Neanderthals and Denisovans were completely replaced by anatomically modern humans dispersing from Africa. Understanding the causes of […]