RW in dynamic random environment generated by the reversal of discrete time contact process

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RW in dynamic random environment generated by the reversal of discrete time contact process Andrej Depperschmidt joint with Matthias Birkner, Jiří Černý and Nina Gantert Ulaanbaatar, 07/08/2015

Motivation Theoretical population genetics tries to explain variability observed in nature by elementary evolutionary mechanisms such as genetic drift (= change in type frequency due to random sampling), mutation, selection, recombination, migration,... present

Motivation Theoretical population genetics tries to explain variability observed in nature by elementary evolutionary mechanisms such as genetic drift (= change in type frequency due to random sampling), mutation, selection, recombination, migration,... present past

Motivation Theoretical population genetics tries to explain variability observed in nature by elementary evolutionary mechanisms such as genetic drift (= change in type frequency due to random sampling), mutation, selection, recombination, migration,... present past Good understanding of variability requires good understanding of genealogical relationship of individuals (cf. Amaury Lambert s talk). In the spatial setting one needs to study coalescing random walks.

Introduction Aim: Study ancestral lineages in locally regulated populations 1 with fluctuating population size. We consider the discrete-time contact process without types. Problem: Pick an individual from the upper invariant distribution and denote by X n the position of the ancestor of that individual n generations ago. Describe the behaviour of X n. Do LLN and CLT for X n hold? Note: X n is a random walk in a Markovian random environment given by the time reversal of the original population process. 1 locally regulated populations are supercritical in sparsely populated and subcritical in crowded regions

Oriented percolation on Z d Z ω(x, n), (x, n) Z d Z i.i.d. Ber(p) (x, n) is open if ω(x, n) = 1 and closed if ω(x, n) = 0 for n m write (x, n) (y, m) if there is x n = x, x n+1,..., x m = y with ω(x k, k) = 1 and x k+1 x k 1 time Z space Z d

Oriented percolation on Z d Z ω(x, n), (x, n) Z d Z i.i.d. Ber(p) (x, n) is open if ω(x, n) = 1 and closed if ω(x, n) = 0 for n m write (x, n) (y, m) if there is x n = x, x n+1,..., x m = y with ω(x k, k) = 1 and x k+1 x k 1 time Z space Z d

Oriented percolation on Z d Z ω(x, n), (x, n) Z d Z i.i.d. Ber(p) (x, n) is open if ω(x, n) = 1 and closed if ω(x, n) = 0 for n m write (x, n) (y, m) if there is x n = x, x n+1,..., x m = y with ω(x k, k) = 1 and x k+1 x k 1 time Z Theorem There is p c (0, 1) s.th. for p > p c P p ( (0, 0) Z d {+ } ) > 0 (and = 0 for p p c ). space Z d In what follows we fix p > p c.

Discrete time contact process time Z space Z d Starting with some initial set A Z d at time m Z, for n m set A n := {y Z d : x A, s.th. (x, m) (y, n)} (here we artificially set ω(, m) = 1 A ( )) Let p > p c, A = Z d and m. Then (η n ) n Z with η n = 1 An the stationary contact process with L(η n ) = upper invariant law. Interpretation: η n is the set of wet sites if water flows up from Z d { } through open sites. is

Discrete time contact process time Z space Z d Starting with some initial set A Z d at time m Z, for n m set A n := {y Z d : x A, s.th. (x, m) (y, n)} (here we artificially set ω(, m) = 1 A ( )) Let p > p c, A = Z d and m. Then (η n ) n Z with η n = 1 An the stationary contact process with L(η n ) = upper invariant law. Interpretation: η n is the set of wet sites if water flows up from Z d { } through open sites. is

Discrete time contact process time Z space Z d Starting with some initial set A Z d at time m Z, for n m set A n := {y Z d : x A, s.th. (x, m) (y, n)} (here we artificially set ω(, m) = 1 A ( )) Let p > p c, A = Z d and m. Then (η n ) n Z with η n = 1 An the stationary contact process with L(η n ) = upper invariant law. Interpretation: η n is the set of wet sites if water flows up from Z d { } through open sites. is

Discrete time contact process time Z space Z d Starting with some initial set A Z d at time m Z, for n m set A n := {y Z d : x A, s.th. (x, m) (y, n)} (here we artificially set ω(, m) = 1 A ( )) Let p > p c, A = Z d and m. Then (η n ) n Z with η n = 1 An the stationary contact process with L(η n ) = upper invariant law. Interpretation: η n is the set of wet sites if water flows up from Z d { } through open sites. is

Discrete time contact process time Z space Z d Starting with some initial set A Z d at time m Z, for n m set A n := {y Z d : x A, s.th. (x, m) (y, n)} (here we artificially set ω(, m) = 1 A ( )) Let p > p c, A = Z d and m. Then (η n ) n Z with η n = 1 An the stationary contact process with L(η n ) = upper invariant law. Interpretation: η n is the set of wet sites if water flows up from Z d { } through open sites. is

Alternative local construction of (η n ) Conditioned on η n the distribution of η n+1 is P(η n+1 (x) = 1 η n ) = p 1 { y, x y 1,ηn(y)=1}. Interpretation: with prob. p at (x, n + 1) there are enough resources for one individual if occupied sites in the neighbourhood in the previous generation exist, then choose a parent at random otherwise (x, n + 1) remains vacant with prob. 1 p at (x, n + 1) no resources are available (x, n + 1) remains vacant irrespective of the neighbourhood

Contact process as locallly regulated population Contact process is locally regulated: Expected offspring number is n + 1 n 3p > 1 in empty neighbourhoods p = p < 1 in crowded neighbourhoods 3 1 3

Backbone: cluster of percolating sites Define the cluster of percolating sites on Z d Z by C := {(x, n) Z d Z : (x, n) Z {+ }}. p = 0.8 time of ancestry 0 100 200 200 100 0 100 200 space Interpretation: C is the set of all wet sites if water flows down from Z d {+ } through open sites. When time is running upwards, the process of configurations of occupied (green) sites is time-reversal of the discrete time contact process. Note: C is not the usual percolation cluster.

Backbone: cluster of percolating sites Define the cluster of percolating sites on Z d Z by C := {(x, n) Z d Z : (x, n) Z {+ }}. p = 0.6 time of ancestry 0 100 200 200 100 0 100 200 space Interpretation: C is the set of all wet sites if water flows down from Z d {+ } through open sites. When time is running upwards, the process of configurations of occupied (green) sites is time-reversal of the discrete time contact process. Note: C is not the usual percolation cluster.

Backbone: cluster of percolating sites Define the cluster of percolating sites on Z d Z by C := {(x, n) Z d Z : (x, n) Z {+ }}. p = 0.535 time of ancestry 0 100 200 200 100 0 100 200 space Interpretation: C is the set of all wet sites if water flows down from Z d {+ } through open sites. When time is running upwards, the process of configurations of occupied (green) sites is time-reversal of the discrete time contact process. Note: C is not the usual percolation cluster.

Random walk on C Define the neighbourhood of (x, n) by U(x, n) := {(y, n + 1) : x y 1}. On B := {(0, 0) C} define the directed random walk (X n ) n=0,1,... on C by X 0 = 0, and for (y, n + 1) C U(x, n) P ( X n+1 = y X n = x, C ) = 1 C U(x, n). Interpretation: (X n ) is the ancestral lineage of an individual located at space-time origin. Remark: More general finite and symmetric U s, leading to different p c and geometry of clusters, can be considered, e.g. U(x, n) := {(y, n + 1) : x y = 1}.

Possible paths for the RW p = 0.8 time of ancestry 0 100 200 200 100 0 100 200 space

Possible paths for the RW p = 0.6 time of ancestry 0 100 200 200 100 0 100 200 space

Possible paths for the RW p = 0.535 time of ancestry 0 100 200 200 100 0 100 200 space

Annealed and quenched LLN and CLT P ω law of RW with transition probab. P(X n+1 = y X n = x, ω) E ω corresponding expectation Theorem (LLN) (i) P ( X n /n 0 B ) = 1, (ii) P ω ( Xn /n n 0 ) = 1 for P( B)-a.a. ω. Theorem (annealed and quenched CLT) For f C b (R d ) (i) E [ f ( X n / n ) B ] n Φ(f ), (ii) E ω [ f (Xn / n) ] n Φ(f ) for P( B)-a.a. ω. Here Φ(f ) = f (x)φ(dx) and Φ is a non-trivial centred d-dimensional normal law. Note: (i) (ii) in LLN; (ii) (i) but (i) (ii) in CLT.

Key steps of the proofs For LLN and annealed (averaged) CLT we need to identify a suitable regeneration structure and obtain moment estimates on regeneration times and corresponding spatial increments. For quenched CLT using two inedependent RW s on the same [( [ ( cluster show that E E ω f Xn / n )] ) 2 ] B Φ(f ) summable. Note: The steps are common in the RWRE literature but the details highly depend on the particular processes.

Use of regeneration structure for LLN T Mn+1 n T Mn T 2 T 1 T 0 X 0 X Mn X Mn+1 Let T 0 = 0 < T 1 < T 2 <... be a sequence of regeneration times, at which the process starts anew. Define M n so that T Mn n < T Mn+1. Then X n = (X n X Mn ) + M n k=1 (X Tk X Tk 1 ) } {{ } sum of i.i.d. r.v. s

Use of regeneration structure for LLN T Mn+1 n T Mn T 2 T 1 T 0 X 0 X Mn X Mn+1 Let T 0 = 0 < T 1 < T 2 <... be a sequence of regeneration times, at which the process starts anew. Define M n so that T Mn n < T Mn+1. Then 1 n X n = 1 n (X n X Mn ) + M n n 1 M n M n k=1 (X Tk X Tk 1 ) } {{ } sum of i.i.d. r.v. s

Remarks regarding regeneration times The random walk cannot be constructed by local rules. At regeneration times not only the walk, but also the environment have start anew. We construct preliminary paths of the RW by local rules using ω s and some auxiliary randomness. These will become segments of the real path at regeneration times.

A local construction of the walk For (x, n) Z d Z let ω(x, n) be an independent uniform ordering of elements of U(x, n). For (x, n) define a (directed) path γ (x,n) k of k steps that begin on open sites, choosing directions according to ω: (x,n) γ k (0) = (x, n), (x,n) γ k (j) = (y, n + j) then γ (x,n) k (j + 1) = (z, n + j + 1), where (z, n + j + 1) is the element of { (z, n + j + 1) U(y, n + j) : (z, n + j + 1) Z d {n + k 1} } with the smallest index in ω(y, n + j) Construction is local because only ω s and ω s in time slices {n,..., n + k 1} are used. ω(x, n)[2] (x, n) ω(x, n)[1] k = 1 k = 2 k = 3 k = 4

From local to global construction ω(x, n)[2] (x, n) ω(x, n)[1] k = 1 k = 2 k = 3 k = 4 γ (x,n) k (k) = endpoint of the local k-step construction If (x, n) C then γ (x,n) (j) := lim k γ(x,n) k (j) exists for all j. If γ (x,n) k (k) C then γ (x,n) k (j) = γ (x,n) (j) for all j k. On B = {(0, 0) C} (X k, k) := γ (0,0) (k), k = 0, 1, 2,... is a space-time version of the path of the directed RW on C. If γ (0,0) k (k) C then (X j, j) = γ (0,0) k (j) for all j k.

Regeneration times T 0 := 0, Y 0 := 0, T 1 := min { k > 0 : γ (0,0) k (k) C }, Y 1 := X T1 := γ (0,0) T 1 (T 1 ), T 2 := T 1 + min { k > 0 : γ (Y1,T1) k (k) C }, Y 2 := X T2 :=..... T 6 T 3 T 2 T 1 T 0 Randomised version of Kuczek s (1989) construction Cont. time versions appeared in Neuhauser (1992) and Valesin (2010)

Main result towards LLN and annealed CLT Proposition Under P( B) the sequence ( (Y i Y i 1, T i T i 1 ) ) is i.i.d., i 1 Y 1 is symmetrically distributed. Furthermore there are c, C (0, ) s.th. P( Y 1 > n B), P(T 1 > n B) Ce cn for n N. Proof sketch. For tail bounds use the fact that finite clusters are small. Symmetry follows from the symmetric construction of the paths. i.i.d. property holds because the local path construction uses disjoint time-slices.

Proof ideas for the quenched case [ ( [ ( Need to show that E E ω f Xn / n )] ) ] 2 B Φ(f ) is summable. We prove this first along a subsequence and then use concentration arguments. For estimates we take independent RW s (X n ) and (X n) on the same cluster C, i.e. they use the same ω, but independent ω resp. ω. One can define joint regeneration times and prove a proposition analogous to the one walk case. With high probability (X n ) and (X n) can be coupled with two independent walks on two independent clusters. In case d 2 walks spend enough time away from each other. In case d = 1 we use a martingale decomposition of the difference.

Outlook & references Problem: From population genetics point of view the joint behaviour of N ancestral lineages, i.e. N coalescing RW s is interesting. References and generalisations: Birkner, Černý, D. and Gantert (2013), Directed random walk on the backbone of an oriented percolation cluster. Electron. J. Probab. Birkner, Černý and D. (2015), Random walks in dynamic random environments and ancestry under local population regulation http://arxiv.org/abs/1505.02791 Miller (2015), Random walks on weighted, oriented percolation clusters, http://arxiv.org/abs/1506.01879