Skip to content
DraconiticResearch
Search Sources API
203,203 studies31 sourcesUpdated 37 min ago
PreprintarXiv licencearXiv

Score-based stochastic reduced-order models of barotropic quasi-geostrophic turbulence

Abstract

In many turbulent flows, the quantities of interest are coarse-grained variables, either because resolving the fine scales is computationally prohibitive or because only coarse observations are available; in both cases, data-driven reduced-order models that evolve only these variables are required. Even when the governing equations are known, their projection onto the coarse variables is not closed, and the central difficulty lies in representing the feedback of the unresolved scales so that the reduced model reproduces the statistical and dynamical properties of the projected high-resolution system. We address this problem with a score-based framework, constructing a reduced-order model of quasi-geostrophic turbulence whose stationary distribution coincides by construction with the distribution learned from data and whose dynamics are calibrated to reproduce the finite-time correlations of the energies in individual wavenumber shells. The resulting model reproduces the stationary statistics of the resolved flow with high accuracy, and its calibration is computationally inexpensive because it requires no forward integration of the model.

Related

  1. Stochastic Operator Inference for reduced-order modeling of capillary wave turbulence using experimental measurements
    Hyeonghun Kim, Lei Zhang, James Friend +1
    arXivPreprintCC BY-NC-ND 4.0Full textComputational physicsarXiv
  2. Growth of small localized perturbations in Surface Quasi-Geostrophic turbulence
    V. J. Valadão, M. Cencini, F. De Lillo +2
    arXivPreprintCC BY 4.0Full textAtmospheric science & meteorologyFluid dynamicsarXiv
  3. Wave-driven geostrophic vortices in rotating turbulence
    Vladimir Parfenyev, Sergey Vergeles
    arXivPreprintCC BY 4.0Full textFluid dynamicsarXiv
  4. Internal heating in rapidly rotating convection is not a shortcut to geostrophic turbulence
    Justin A. Nicoski, Tobias G. Oliver, Stefano Maffei +1
    arXivPreprintCC BY 4.0Full textPlanetary science & exoplanetsSolar & stellar physicsarXiv
  5. Evidence for an Obstruction to Perturbative Renormalization Group in Stochastic Turbulence
    L. Ts. Adzhemyan, D. A. Davletbaeva, D. A. Evdokimov +1
    arXivPreprintarXiv licenceFull textStatistical & nonlinear physicsarXiv
BibTeX
@misc{giorgini2026scorebased,
  title = {{Score-based stochastic reduced-order models of barotropic quasi-geostrophic turbulence}},
  author = {Ludovico Theo Giorgini},
  howpublished = {arXiv},
  year = {2026},
  month = sep,
  doi = {10.48550/arxiv.2609.34028},
  eprint = {2609.34028},
  archivePrefix = {arXiv},
  url = {https://arxiv.org/abs/2609.34028},
}
RIS
TY  - UNPB
TI  - Score-based stochastic reduced-order models of barotropic quasi-geostrophic turbulence
AU  - Ludovico Theo Giorgini
PY  - 2026
DA  - 2026/09/27
PB  - arXiv
DO  - 10.48550/arxiv.2609.34028
UR  - https://arxiv.org/abs/2609.34028
AB  - In many turbulent flows, the quantities of interest are coarse-grained variables, either because resolving the fine scales is computationally prohibitive or because only coarse observations are available; in both cases, data-driven reduced-order models that evolve only these variables are required. Even when the governing equations are known, their projection onto the coarse variables is not closed, and the central difficulty lies in representing the feedback of the unresolved scales so that the reduced model reproduces the statistical and dynamical properties of the projected high-resolution system. We address this problem with a score-based framework, constructing a reduced-order model of quasi-geostrophic turbulence whose stationary distribution coincides by construction with the distribution learned from data and whose dynamics are calibrated to reproduce the finite-time correlations of the energies in individual wavenumber shells. The resulting model reproduces the stationary statistics of the resolved flow with high accuracy, and its calibration is computationally inexpensive because it requires no forward integration of the model.
ER  -