<p>Backwards geodesics for TASEP were introduced in [<CitationRef CitationID="CR30">30</CitationRef>]. We consider flat initial conditions and show that under proper scaling the end-point of the geodesic converges to maximizer argument of the <InlineEquation ID="IEq1"> <InlineMediaObject> <ImageObject Color="BlackWhite" FileRef="10955_2025_3488_Article_IEq1.gif" Format="GIF" Height="18" Rendition="HTML" Resolution="72" Type="Linedraw" Width="39" /> </InlineMediaObject> <EquationSource Format="TEX">\(\hbox {Airy}_2\)</EquationSource> <EquationSource Format="MATHML"><math> <msub> <mtext>Airy</mtext> <mn>2</mn> </msub> </math></EquationSource> </InlineEquation> process minus a parabola. We generalize its definition to generic non-integrable models including ASEP and speed changed ASEP (call it quasi-geodesics). We numerically verify that its end-point is universal, where the scaling coefficients are analytically computed through the KPZ scaling theory.</p>

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Quasi-Geodesics in Integrable and Non-Integrable Exclusion Processes

  • Patrik L. Ferrari,
  • Min Liu

摘要

Backwards geodesics for TASEP were introduced in [30]. We consider flat initial conditions and show that under proper scaling the end-point of the geodesic converges to maximizer argument of the \(\hbox {Airy}_2\) Airy 2 process minus a parabola. We generalize its definition to generic non-integrable models including ASEP and speed changed ASEP (call it quasi-geodesics). We numerically verify that its end-point is universal, where the scaling coefficients are analytically computed through the KPZ scaling theory.