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pith:2026:ECPKF6XLH3CKDOWZV6EHDQW2LB
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Systematic Evaluation of Stencil Configuration, Forcing Scheme, and Resolution Effects in the Stratified Taylor--Green Vortex: A Lattice Boltzmann Study

Hongxuan Zhang

The D3Q27×19 lattice configuration in the double-distribution-function framework reproduces kinetic and potential energy evolution in the stratified Taylor-Green vortex with the best accuracy-efficiency trade-off.

arxiv:2605.14505 v1 · 2026-05-14 · physics.flu-dyn

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Claims

C1strongest claim

The D3Q27×19 configuration achieves an optimal balance between numerical accuracy and computational efficiency, accurately reproducing the temporal evolution of kinetic and potential energies as well as the characteristic double-peak dissipation structure. Under strongly stratified conditions, the velocity-shift forcing schemes outperform discrete source-term approaches, reducing the overall error by approximately 45.54%.

C2weakest assumption

The double-distribution-function framework under the Boussinesq approximation is assumed to capture the essential physics of the stratified flow without needing corrections for compressibility or other non-Boussinesq effects at the tested stratification levels.

C3one line summary

D3Q27x19 stencil combined with velocity-shift forcing in LBM accurately reproduces kinetic and potential energies in stratified Taylor-Green vortex at 256^3 resolution, cutting error by about 45% versus other schemes.

References

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[1] The energy cascade in a strongly stratified fluid.Journal of Fluid Mechanics, 550:207–242, 2006 2006
[2] Fluid motions in the presence of strong stable stratifi- cation.Annual review of fluid mechanics, 32(1):613–657, 2000 2000
[3] Stratified turbulence: A possible interpretation of some geo- physical turbulence measurements.Journal of the Atmospheric Sciences, 65(7):2416–2424, 2008 2008
[4] Similarity scaling and vorticity structure in high-reynolds-number stably stratified turbulent wakes.Journal of Fluid Mechanics, 671:52–95, 2011 2011
[5] Layering, instabilities, and mixing in turbulent stratified flows.Annual Review of Fluid Mechanics, 53(1):113–145, 2021 2021

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First computed 2026-05-17T23:39:06.264380Z
Builder pith-number-builder-2026-05-17-v1
Signature Pith Ed25519 (pith-v1-2026-05) · public key
Schema pith-number/v1.0

Canonical hash

209ea2faeb3ec4a1bad9af8871c2da58637125d49ae5bb4a709894883a498290

Aliases

arxiv: 2605.14505 · arxiv_version: 2605.14505v1 · doi: 10.48550/arxiv.2605.14505 · pith_short_12: ECPKF6XLH3CK · pith_short_16: ECPKF6XLH3CKDOWZ · pith_short_8: ECPKF6XL
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curl -sH 'Accept: application/ld+json' https://pith.science/pith/ECPKF6XLH3CKDOWZV6EHDQW2LB \
  | jq -c '.canonical_record' \
  | python3 -c "import sys,json,hashlib; b=json.dumps(json.loads(sys.stdin.read()), sort_keys=True, separators=(',',':'), ensure_ascii=False).encode(); print(hashlib.sha256(b).hexdigest())"
# expect: 209ea2faeb3ec4a1bad9af8871c2da58637125d49ae5bb4a709894883a498290
Canonical record JSON
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    "primary_cat": "physics.flu-dyn",
    "submitted_at": "2026-05-14T07:48:42Z",
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