Equation (1) is Underdamped Langevin dynamics for a unit-mass particle in potential , coupled to a heat bath of temperature . The coefficient is viscous friction, and the noise amplitude is fixed by the Fluctuation-dissipation theorem. Its Fokker-Planck equation is
For , velocity relaxes rapidly, so formally
Thus the Overdamped Langevin dynamics is
and its density obeys
For , stationary points satisfy . There is one minimum and one maximum per period. The potential is a sinusoidal washboard tilted downward to the right by per period.
Periodization partitions the real line into translated cells, so
Translation by merely reindexes the sum, proving periodic boundary conditions; summing the Fokker--Planck equation proves that obeys it.
At stationarity the current is constant. Solving this first-order equation and imposing periodicity gives
Here is the stationary probability crossing any point per unit time. Normalization determines it:
Each net crossing of a periodic cell advances the unwrapped particle by . The stationary mean velocity is therefore
For the numerator is positive, so motion is on average toward increasing , down the tilted potential.
In the low-temperature regime, the particle rapidly equilibrates near a minimum and only rarely crosses a neighboring maximum. Applying Laplace's method to the exact current formula gives the Kramers escape rates
Each right or left escape changes position by , hence
The reduced continuous-time random walk on minima has off-diagonal transition rates
and diagonal generator entry . Its residence time in each well is exponentially distributed with rate , and the next jump is right with probability .
An exact Gillespie algorithm for one particle is:
  • Set the current well and time .
  • If is absorbing, stop.
  • Set and draw .
  • Move to if , and otherwise to .
  • Set and repeat, stopping if the jump crosses an absorbing end.
For , simulate particle identities independently and maintain a priority queue of their next event times. For , store occupation numbers and use aggregate event rates and for each well; one population-level Gillespie event then decrements one and increments its neighbor. This replaces work proportional to particle number by work proportional to the number of occupied wells.

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