1 / 56

A variational formulation for higher order macroscopic traffic flow models of the GSOM family

A variational formulation for higher order macroscopic traffic flow models of the GSOM family. J.P. Lebacque UPE-IFSTTAR-GRETTIA Le Descartes 2, 2 rue de la Butte Verte F93166 Noisy-le-Grand, France Jean-patrick.lebacque@ifsttar.fr M.M. Khoshyaran E.T.C. Economics Traffic Clinic

abrial
Download Presentation

A variational formulation for higher order macroscopic traffic flow models of the GSOM family

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. A variational formulation for higher order macroscopic trafficflow models of the GSOM family J.P. Lebacque UPE-IFSTTAR-GRETTIA Le Descartes 2, 2 rue de la Butte Verte F93166 Noisy-le-Grand, France Jean-patrick.lebacque@ifsttar.fr M.M. Khoshyaran E.T.C. Economics Traffic Clinic 34 Avenue des Champs-Elysées, 75008, Paris, France www.econtrac.com ISTTT 20, July 17-19, 2013

  2. Outline of the presentation • Basics • GSOM models • Lagrangian Hamilton-Jacobi and variational interpretation of GSOM models • Analysis, analytic solutions • Numerical solution schemes ISTTT 20, July 17-19, 2013

  3. Scope • The GSOM model is close to the LWR model • It isnearly as simple (non trivial explicit solutions fi) • But itaccounts for driver variability (attributes) • More scope for lagrangianmodeling, driver interaction, individualproperties • Admits a variational formulation • Expectedbenefits: numericalschemes, data assimilation ISTTT 20, July 17-19, 2013

  4. The LWR model ISTTT 20, July 17-19, 2013

  5. The LWR model in a nutshell (notations) • Introduced by Lighthill, Whitham (1955), Richards (1956) • The equations: • Or: ISTTT 20, July 17-19, 2013

  6. Solution of the inhomogeneous Riemann problem • Analytical solutions, boundary conditions, nodemodeling Density Position ISTTT 20, July 17-19, 2013

  7. Demand Supply The LWR model: supply / demand • the equilibrium supply and demand functions (Lebacque, 1993-1996) ISTTT 20, July 17-19, 2013

  8. The LWR model: the min formula • The local supply and demand: • The min formula • Usage: numerical schemes, boundary conditions →intersection modeling ISTTT 20, July 17-19, 2013

  9. Inhomogeneous Riemann problem (discontinuous FD) • Solution with Min formula • Can berecovered by the variational formulation of LWR (Imbert MonneauZidani 2013) Time (a,0 ) (b,0 ) (a ) (b ) Position ISTTT 20, July 17-19, 2013

  10. GSOM models ISTTT 20, July 17-19, 2013

  11. GSOM (Generic second ordermodelling) models • (Lebacque, Mammar, Haj-Salem 2005-2007) • In a nutshell • Kinematicwaves = LWR • Driver attributedynamics • Includesmanycurrentmacroscopicmodels ISTTT 20, July 17-19, 2013

  12. GSOM Family: description • Conservation of vehicles(density) • Variable fundamental diagram, dependent on a driver attribute (possibly a vecteur) I • Equation of evolution for Ifollowing vehicle trajectories (example: relaxation) ISTTT 20, July 17-19, 2013

  13. GSOM: basic equations Conservation des véhicules Dynamics of I along trajectories Variable fundamental Diagram ISTTT 20, July 17-19, 2013

  14. Example 0: LWR (Lighthill, Whitham, Richards 1955, 1956) • No driver attribute • One conservation equation ISTTT 20, July 17-19, 2013

  15. Example 1: ARZ (Aw,Rascle 2000, Zhang,2002) • Lagrangien attribute I= difference between actual and mean equilibrium speed ISTTT 20, July 17-19, 2013

  16. Increasing values of I Example 2: 1-phase Colombo model (Colombo 2002, Lebacque MammarHaj-Salem 2007) • Variable FD (in the congested domain + critical density) • The attribute Iis the parameter of the family of FDs ISTTT 20, July 17-19, 2013

  17. Fundamental Diagram (speed-density) ISTTT 20, July 17-19, 2013

  18. modéle 2-phase modéle 1-phase Example 2 continued (1-phase Colombo model) • 1-phase vs 2-phase: Flow-density FD ISTTT 20, July 17-19, 2013

  19. Example 3: Cremer-Papageorgiou • Based on the Cremer-Papageorgiou FD (Haj-Salem 2007) ISTTT 20, July 17-19, 2013

  20. Example 4: « multi-commodity » models • GSOM Model • + advection (destinations, vehicle type) • = multi-commodity GSOM ISTTT 20, July 17-19, 2013

  21. Example 5: multi-lane model • Impact of multi-lanetraffic • Two states: congestion (stronglycorrelatedlanes) et fluid (weaklycorrelatedlanes) •  2 FDsseparated by the phase boundaryR(v) • Relaxation towardseachregime •  eulerian source terms ISTTT 20, July 17-19, 2013

  22. Example 6: Stochastic GSOM (Khoshyaran Lebacque 2007-2008) • Idea: • Conservationof véhicles • Fundamental Diagram depends on driver attributeI • Iis submitted to stochastic perturbations (other vehicles, traffic conditions, environment) ISTTT 20, July 17-19, 2013

  23. Two fundamental properties of the GSOM family (homogeneous piecewise constant case) • 1.discontinuities of Ipropagate with the speed v of traffic flow • 2.If the invariant Iis initially piecewise constant, it stays so for all times t > 0 • ⇒On any domain on which I is uniform the GSOM model simplifies to a translated LWR model (piecewise LWR) ISTTT 20, July 17-19, 2013

  24. rr vr rl vl x FDl FDr Inhomogeneous Riemann problem • I = Il in all of sector (S) • I = Ir in all of sector (T) ISTTT 20, July 17-19, 2013

  25. Generalized (translated) supply- Demand (Lebacque MammarHaj-Salem 2005-2007)Example: ARZ model • TranslatedSupply / Demand = supplyrespdemand for the « translated » FD (withresp to I ) ISTTT 20, July 17-19, 2013

  26. Example of translatedsupply / demand: the ARZ family ISTTT 20, July 17-19, 2013

  27. Solution of the Riemann problem (summary) • Define the upstream demand, the downstream supply (which depend on Il ): • The intermediate stateUm is given by • The upstream demand and the downstream supply (as functions of initial conditions) : • Min Formula: ISTTT 20, July 17-19, 2013

  28. Applications • Analytical solutions • Boundary conditions • Intersection modeling • Numericalschemes ISTTT 20, July 17-19, 2013

  29. Lagrangian GSOM; HJ and variationalinterpretation ISTTT 20, July 17-19, 2013

  30. Variational formulation of GSOM models • Motivation • Numericalschemes (grid-free cfMazaré et al 2011) • Data assimilation (floatingvehicle / mobile data cf Claudel Bayen 2010) • Advantages of variationalprinciples • Difficulty • Theorycomplete for LWR (Newell, Daganzo, also Leclercq Laval for variousrepresentations ) • Need of a unique value function ISTTT 20, July 17-19, 2013

  31. Lagrangian conservation law t • Spacingr • The rate of variation of spacingrdepends on the gradient of speed with respect to vehicle index N r x The spacingis theinverse of density ISTTT 20, July 17-19, 2013

  32. Lagrangian version of the GSOM model • Conservation law in lagrangiancoordinates • Driver attributeequation (naturallagrangian expression) • Weintroducethe position of vehicle N: • Note that: ISTTT 20, July 17-19, 2013

  33. Lagrangian Hamilton-Jacobi formulation of GSOM (Lebacque Khoshyaran2012) • Integrate the driver-attributeequation • Solution: • FD Speed becomes a function of driver, time and spacing ISTTT 20, July 17-19, 2013

  34. Lagrangian Hamilton-Jacobi formulation of GSOM • Expressing the velocityv as a function of the position X ISTTT 20, July 17-19, 2013

  35. Associatedoptimizationproblem • Define: • Note implication: W concave with respect to r (ie flow density FD concave with respect to density • Associatedoptimizationproblem ISTTT 20, July 17-19, 2013

  36. FunctionsM and W ISTTT 20, July 17-19, 2013

  37. Illustration of the optimizationproblem: • Initial/boundary conditions: • Blue: IC + trajectory of first vh • Green: trajectories of vhs with GPS • Red: cumulative flow on fixed detector t N ISTTT 20, July 17-19, 2013

  38. Elements of resolution ISTTT 20, July 17-19, 2013

  39. Characteristics • Optimal curves characteristics (Pontryagin) • Note: speed of charcteristics: > 0 • Boundary conditions ISTTT 20, July 17-19, 2013

  40. Initial conditions for characteristics • IC • Vhtrajectory N t ISTTT 20, July 17-19, 2013

  41. Initial / boundary condition • Usuallytwo solutions r0 (t ) t ISTTT 20, July 17-19, 2013

  42. Example: Interaction of a shockwavewith a contact discontinuityEulerianview ISTTT 20, July 17-19, 2013

  43. Initial conditions: • Top: eulerian • Down: lagrangian ISTTT 20, July 17-19, 2013

  44. Example: Interaction of a shockwavewith a contact discontinuityLagrangianview ISTTT 20, July 17-19, 2013

  45. Anotherexample: total refraction of characteristicsand lagrangiansupply • ??? ISTTT 20, July 17-19, 2013

  46. Decompositionproperty (inf-morphism) • The set of initial/boundary conditions is union of several sets • Calculate a partial solution (corresponding to a partial set of IBC) • The solution is the min of partial solutions ISTTT 20, July 17-19, 2013

  47. The optimalitypbcanbesolved on characteristicsonly • This is a Lax-Hopflike formula • Application: numericalschemesbased on • Piecewise constant data (including the system yieldingI ) • Decomposition of solutions based on decomposition of IBC • Use characteristics to calculate partial solutions ISTTT 20, July 17-19, 2013

  48. Numericalschemebased on characteristics (continued) • If the initial condition on I ispiecewise constant  • the spacingalongcharacteristicsispiecewise constant • Principleillustrated by the example: interaction betweenshockwave and contact discontinuity ISTTT 20, July 17-19, 2013

  49. Alternatescheme: particlediscretization • Particlediscretization of HJ • Use charateristics • Yields a Godunov-likescheme (in lagrangiancoordinates) • BC: Upstreamdemand and downstreamsupply conditions ISTTT 20, July 17-19, 2013

  50. Numericalexample • Model: Colombo 1-phase, stochastic • Process for I: Ornstein-Uhlenbeck, twolevels (highat the beginning and end, lowotherwise)  refraction of charateristics and waves • Demand: Poisson, constant level • Supply: highat the beginning and end, lowotherwise inducesbackwards propagation of congestion • Particles: 5 vehicles • Duration: 20 mn • Length: 3500 m ISTTT 20, July 17-19, 2013

More Related