NP
Nonlinear Processes in Geosciences

Mathematics

NP Paper of the Month: “Representation learning with unconditional denoising diffusion models for dynamical systems”

NP Paper of the Month: “Representation learning with unconditional denoising diffusion models for dynamical systems”

About the revolution of generating butterflies Imagine the most vibrant butterfly you can conceive. Congratulations – you’ve just achieved what generative AI does! This technology can create images from simple text descriptions, revolutionising image generation. But as geoscientists, how can we use it to improve the prediction of chaotic system like our weather? How can it help us to discover prop ...[Read More]

Bridging Mathematics and Climate Science: the AMS MRC programme for June-July 2024

Bridging Mathematics and Climate Science: the AMS MRC programme for June-July 2024

The American Mathematical Society’s Mathematics Research Communities (MRC) continues to be a beacon for early-career mathematicians seeking professional development. This esteemed program offers opportunities to hone collaborative research skills, cultivate networks within active research domains, and benefit from mentorship by leaders in the field. As part of the MRC initiative, the upcoming conf ...[Read More]

ECS SpotLight: The link between European warm-temperature extremes and atmospheric persistence

ECS SpotLight: The link between European warm-temperature extremes and atmospheric persistence

Persistent atmospheric circulation patterns are not a necessary requirement for warm temperature extremes in Europe. This key finding from a recent study led by Emma Holmberg challenges a more traditional meteorological view of persistence, which typically considers summertime heatwaves, especially in northern regions of Europe, to be synonymous with persistent atmospheric flow patterns. Furthermo ...[Read More]

Exploring the multistable and multiscale climate system via noise

Could our present day “warm” climate turn into a frozen fully glaciated one, as if the whole Earth is a huge “snowball”? That was a question put forward independently by Mikhail Budyko and William Sellers in the late 60s [1,2] who made a first estimate of the necessary changes of incoming solar radiation, such that either the Arctic ice sheet completely melts, or the planet gets fully frozen. Base ...[Read More]