The quasi-geostrophic equations are a cornerstone in the mathematical modelling of large-scale geophysical flows, where the balance between pressure gradients and the Coriolis effect is paramount.
How winds finally end up blowing the way they do results from a fascinating interplay of different forces, each acting on different length and time scales. Aa Aa Aa The ancient Greeks believed that ...
In this paper, we study the 2D stochastic quasi-geostrophic equation on 𝕋2 for general parameter α ∈ (0, 1) and multiplicative noise. We prove the existence of weak solutions and Markov selections ...
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