A data assimilation algorithm for the subcritical surface quasi-geostrophic equation
MS Jolly, VR Martinez, ES Titi - Advanced Nonlinear Studies, 2017 - degruyter.com
In this article, we prove that data assimilation by feedback nudging can be achieved for the
three-dimensional quasi-geostrophic equation in a simplified scenario using only large …
three-dimensional quasi-geostrophic equation in a simplified scenario using only large …
Continuous data assimilation with blurred-in-time measurements of the surface quasi-geostrophic equation
MS Jolly, VR Martinez, EJ Olson, ES Titi - Chinese Annals of Mathematics …, 2019 - Springer
An intrinsic property of almost any physical measuring device is that it makes observations
which are slightly blurred in time. The authors consider a nudging-based approach for data …
which are slightly blurred in time. The authors consider a nudging-based approach for data …
Minimality properties of set-valued processes and their pullback attractors
M Coti Zelati, P Kalita - SIAM Journal on Mathematical Analysis, 2015 - SIAM
We discuss the existence of pullback attractors for multivalued dynamical systems on metric
spaces. Such attractors are shown to exist without any assumptions in terms of continuity of …
spaces. Such attractors are shown to exist without any assumptions in terms of continuity of …
Non-unique weak solutions of forced SQG
M Dai, Q Peng - arXiv preprint arXiv:2310.13537, 2023 - arxiv.org
We construct non-unique weak solutions $\theta\in C_t^ 0C_x^{0-} $ for forced surface quasi-
geostrophic (SQG) equation. This is achieved through a convex integration scheme adapted …
geostrophic (SQG) equation. This is achieved through a convex integration scheme adapted …
Non-unique stationary solutions of forced SQG
M Dai, Q Peng - arXiv preprint arXiv:2302.03283, 2023 - arxiv.org
We show the existence of non-unique stationary weak solutions for forced surface quasi-
geostrophic (SQG) equation via a convex integration scheme. The scheme is implemented …
geostrophic (SQG) equation via a convex integration scheme. The scheme is implemented …
Uniformly attracting limit sets for the critically dissipative SQG equation
We consider the global attractor of the critical SQG semigroup $ S (t) $ on the scale-invariant
space $ H^ 1 (\mathbb {T}^ 2) $. It was shown in~\cite {CTV13} that this attractor is finite …
space $ H^ 1 (\mathbb {T}^ 2) $. It was shown in~\cite {CTV13} that this attractor is finite …
Rayleigh-Bénard problem for thermomicropolar fluids
P Kalita, G Łukaszewicz, J Siemianowski - 2018 - projecteuclid.org
The two-dimensional Rayleigh-Bénard problem for a thermomicropolar fluids model is
considered. The existence of suitable weak solutions which may not be unique, and the …
considered. The existence of suitable weak solutions which may not be unique, and the …
Determining modes for the surface quasi-geostrophic equation
A Cheskidov, M Dai - Physica D: Nonlinear Phenomena, 2018 - Elsevier
We introduce a determining wavenumber for the surface quasi-geostrophic (SQG) equation
defined for each individual trajectory and then study its dependence on the force. While in …
defined for each individual trajectory and then study its dependence on the force. While in …
A determining form for the subcritical surface quasi-geostrophic equation
MS Jolly, VR Martinez, T Sadigov, ES Titi - Journal of Dynamics and …, 2019 - Springer
We construct a determining form for the surface quasi-geostrophic (SQG) equation with
subcritical dissipation. In particular, we show that the global attractor for this equation can be …
subcritical dissipation. In particular, we show that the global attractor for this equation can be …
Smooth attractors for weak solutions of the SQG equation with critical dissipation
We consider the evolution of weak vanishing viscosity solutions to the critically dissipative
surface quasi-geostrophic equation. Due to the possible non-uniqueness of solutions, we …
surface quasi-geostrophic equation. Due to the possible non-uniqueness of solutions, we …