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# Data Assimilation

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  1. arXiv

    Subsurface flow data assimilation gets adaptive-tempered sequential Monte Carlo: posteriors match reference MCMC on four synthetic truths, with 2.5–7.0× single-GPU speedups

    Geological uncertainty in subsurface flow systems is often hierarchical: a set of geological metaparameters controls overall statistics while cell-by-cell property fields vary, and both must be estimated from observations. An adaptive-tempered sequential Monte Carlo method estimates metaparameters and Gaussian latent variables jointly within one likelihood framework, with surrogate models supplying all forward evaluations. Across four synthetic true models, its posterior metaparameter distributions and flow predictions agree closely with reference MCMC results, while single-GPU data assimilation is 2.5–7.0 times faster and needs fewer function evaluations.

  2. arXiv

    GraphCast takes over only ensemble perturbations: a month of real-observation cycling keeps background errors at least level with a physics model

    Placing the machine-learning weather model GraphCast inside a real data-assimilation cycle, with the mean still supplied by the physics-based MPAS model and GraphCast evolving only ensemble perturbations, gives ensemble spread and covariance structure comparable to an all-physics baseline over one month; the EnVar background RMSE against GFS analyses is consistently lower below model level 40, while degradation appears near the model top from interpolation and extrapolation.

  3. arXiv

    MarsNet learns the Martian atmosphere from observations alone: 4.2 K near-surface temperature error and the best surface pressures of four products

    The Martian atmosphere has been described by reanalyses that assimilate spacecraft retrievals into general circulation models, so where observations are sparse their fields largely reflect the model. MarsNet trains a two-hour forecast and a per-window observation update jointly inside a fixed physical structure, using no reanalysis or model field as input or target. On MGS radio-occultation temperatures assimilated by no dataset, it matches or improves on the three reanalyses in the lowest three scale heights, with a near-surface RMSE of 4.2 K against 4.4–5.4 K, but is less accurate aloft.

  4. medRxiv

    Sepsis glucose digital twins stop waiting for error thresholds: a frozen PatchTST plus reinforcement-learning residual fix improved one-step forecasts in all 10 ICU patients

    Glucose digital twins in septic intensive care previously refit the model only after forecast error crossed a threshold, a reactive correction. This work reports a proactive workflow: a frozen PatchTST foundation model produces a one-step forecast, and an Actor–Critic reinforcement-learning agent uses the last 30-minute glucose window and recent residual history to apply a correction bounded at ±0.05 to that first step, which is then rolled out recursively over 15 steps. On minute-by-minute continuous glucose monitoring from 10 septic ICU patients, the pretrained agent lowered one-step forecast error in all 10 without patient-specific retraining, and mean absolute percentage error on the source patient's test set fell from 0.49% to 0.34%.

  5. Ammonia inversions no longer need 60 chemistry runs: EnsAI builds the ensemble 3300 times faster

    Ammonia emissions inversions rely on ensembles to carry meteorology-dependent error covariances, but each ensemble means repeatedly running the GEM-MACH chemistry model. EnsAI replaces that with a U-Net that maps ammonia emissions perturbations plus temperature and wind fields directly to surface concentration perturbations, producing a week of simulated data per member in 7 seconds against roughly 6.5 hours for GEM-MACH on 720 nodes. Inversions using the EnsAI ensemble gave annual total emissions 2.6% lower than the GEM-MACH ensemble inversions, with monthly totals within 10% for every month.

  6. Sparse particle tracks can still yield turbulent flow fields: physics-constrained networks degrade more slowly as seeding thins

    The German Aerospace Center team applied physics-informed neural networks (PINNs) to reconstruct Eulerian flow fields from sparse 3D Lagrangian particle tracking data, comparing them systematically with polynomial binning and FlowFit on identical preprocessed data. Across homogeneous isotropic turbulence, a synthetic turbulent boundary layer, and wind-tunnel boundary-layer measurements, PINNs gave the lowest velocity and pressure errors over the investigated sparsity levels and degraded more slowly as particle density fell. FlowFit achieved lower vorticity errors at several densely seeded conditions and kept its divergence residual near machine precision.

  7. Integrating image inpainting into an ensemble score filter to track surface quasi-geostrophic dynamics under partial observations

    The work develops an ensemble score filter (EnSF) that integrates image inpainting to address data assimilation with partial observations: at each filtering step a training-free diffusion model estimates the observed states by incorporating likelihood information into the score function, and image inpainting methods then predict the unobserved state variables, with performance demonstrated by tracking Surface Quasi-Geostrophic (SQG) model dynamics across a variety of scenarios as a proof of concept.

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