exit times and the generalised dispersion problem benjamin devenish and david thomson met office, uk
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Exit times and the generalised dispersion problem
Benjamin Devenish and
David Thomson
Met Office, UK
Ballistic vs diffusive process
T̂B » (½¡ 1)r¾u
» (½¡ 1)r 2=3
"1=3
T̂D » (½¡ 1)2r 2
K (r )
» (½¡ 1)2r 2=3
"1=3
For ½¡ 1¿ 1
Outline of talk
• Theoretical results for exit times for a diffusive process
• Kinematic simulation
• DNS
• Lagrangian stochastic model
Exit time pdf for diffusive process
• Exit time pdf
• Absorbing boundary at r = R
• Constant flux at r = 0
• Initial separation
• Transformed diffusion equation
r0 = R=½
@h@t =
@2h@t2
¡ f (m;d)@@»
µh»
¶
f (m;d) = (d¡ 1+ m=2)=(1¡ m=2)
pE (t) = ¡ddt
Z
jr j<Rp(r; t) dr
h(»;t) = rd¡ 1+m=2p(r;t)
»= r1¡ m=2=(1¡ m=2)
K (r) / rm
Exit time pdf II
• Exit time pdf (following Boffetta & Sokolov 2002)
• Lagrangian relative velocity decorrelation time scale
• Closed form solutions only for special cases
pE (t) =1
2~T(2¡ m)2½¡ (1¡ d=2¡ m=2)
1X
k=1
j º;kJ º (j º;k=½1¡ m=2)
J º+1(j º;k)exp
µ¡
14j 2º;k(2¡ m)2 t
~T
¶
one dimensional problem in (»;t) space
for d = 3, m = ¡ 4 ) f (m;d) = 0di®usivity balances curvature of sphere
Special case d=3, m=-4
Jacobi’s transformation for theta functions
µ1(z;t) = ¡ iei z+¼it=4µ3(z + ¼2 + ¼t
2 )
µ3(z;t) = (¡ it)¡ 1=2ez2=¼itµ3
¡zt ; ¡ 1
t
¢
pE (t) =9
2~T
s~T
9¼t@@¹
1X
k=¡ 1
(¡ 1)k exp
Ã
¡µ
¹ ¡12
+k¶2 ~T
9t
!
pE (t) = ¡9~T
@@¹
X
k
(¡ 1)k sin· µ
k ¡12
¶2¼¹
¸exp
Ã
¡ 9µ
k ¡12
¶2 ¼2t~T
!
pE (t) =9
2~T
@@¹
µ1
µ¹ ;
9t~T
¶¹ = 1=½3
Express pE (t) in terms of theta function of ¯rst kind
Exit time pdf for : small times I
½¡ 1¿ 1
Let ½= 1+±and consider limit ±! 0 for ¯xed t ¿ ~T
pE (t) = ¡
s~T
9¼t3
X
k
(¡ 1)k
µk ¡
3±2
¶exp
Ã
¡19
µk ¡
3±2
¶2 ~Tt
!
+O(±2)
pE (t) »
sT̂D
2¼t3exp
Ã
¡12
T̂D
t
!
+O(±2)
For½¡ 1¿ 1, T̂D » ±2~T
pE (t) »(½¡ 1)R
½
r1
2¼K t3exp
µ¡
(½¡ 1)2
½2
R2
2K t
¶Since T̂D » (½¡ 1)2R2=2½2K
Restrict t ¿ T̂D ; leading order term governed by minkjk ¡ 3±=2j
Exit time pdf for : small times II
½¡ 1¿ 1
pE (t) »(½¡ 1)R
½
r1
2¼K t3exp
µ¡
(½¡ 1)2
½2
R2
2K t
¶
² 1-D Brownian motion
² Modeof pdf is T̂D
² For ¯xed ½, pE (t) ! 0 as t ! 0
² For t À T̂D , pE (t) ! 1=t3=2
Exit time pdf for : intermediate times
Consider T̂D ¿ t ¿ ~T for limit ±! 0
pE (t) »±~T
X
k
j 2º;k exp
µ¡ j 2
º;kt~T
¶+ O(j 2
º;k±2)
Exponential term becomes negligible when j º;k À ( ~T=t)1=2
Need to ensure that error is bounded when j º;k » ( ~T=t)1=2
Require j 2º;k±2 ¿ 1 ) t À ±2 ~T ) t À T̂D since T̂D » ±2 ~T
½¡ 1¿ 1
Taylor expansion of Bessel function
Let s = j º;k
qt=~T
In limit ds ! 0 (corresponds to t ¿ ~T)
pE (t) »±~T
Ã~Tt
! 3=2 Z 1
0s2 exp(¡ s2) ds +O(j 2
º;k±2)Independent of d and m
pE (t) »±~T
1X
s=1;ds
s2dsexp(¡ s2)
Ã~Tt
! 3=2
+ O(j 2º;k±2)
Exit time pdf for
½À 1
For small argument
pE (t) »1~T
X
k
j º+1º;k
J º+1(j º;k)exp
µ¡ j 2
º;kt~T
¶+ O(j º+3
º;k ½m¡ 2)
J º (x) » xº + O(xº +2) as x ! 0
pdf is independent of ½at leading order
Positive moments of exit time pdf
r 2C0 = ¡ p(r;0); r 2Cn = ¡ nCn¡ 1 for n > 1
Closed form expressions derivable from hierarchy of Poisson equations:
For ½¡ 1¿ 1
htn i » (½¡ 1) ~TnX
k
j ¡ 2nº;k + O(j ¡ (2n¡ 1)
º ;k ±2)
) htn i / (½¡ 1) for all nFor ½À 1
htn i » ~TnX
k
j ¡ (2n+1)+ºº;k
J º +1(j º ;k)+ O(j ¡ 2n+º +1
º;k ½m¡ 2)
independent of ½
Cn(r) = nZ 1
0p(r;t)tndt htn i = n
Z
jr j<RCn(r) dr:
Negative moments of exit time pdf
For ½¡ 1¿ 1
ht¡ n i »1~Tn
µ½
½¡ 1
¶2n 2n¡ (n + 1=2)p
¼
) ht¡ n i / (½¡ 1)¡ 2n
Analytical expressions only possible for special case d = 3, m = ¡ 4
Kinematic simulation I
• Linear superposition of random Fourier modes
• Prescribed energy spectrum
• Possible to represent wide range of scales
• Includes turbulent-like structures e.g.– eddying, straining and streaming regions
Kinematic simulation II• No coupling of modes in k.s.
• Particles are swept through the small eddies by the large eddies
• Decreased correlation time of small eddies• Particles have less time to be affected
by the smaller eddies
) no sweeping of small scales by large scales
) pairs will separate more slowly
Kinematic simulation: phenomenology
U
r
2/3
1/3
rr
U
1/3 1/3 r
¿(r) » rU
~T » r 1=3U"2=3
hti » Ur 1=3
"2=3
Separation statistics
K (r) » ¾2u¿(r)
»"2=3r5=3
U
Exit time statistics
) hr2i »"4t6
U6
‘take off’ time
for t À ~T
Lagrangian relative velocity time scale
• Inertial range • 1200 modes• Unidirectional mean flow
• Adaptive time step based on local decorrelation time scale
Separation statistics
Exit time statistics
U(10;0;0) À ¾u = 1
L=́ = 106 ¡ 108
Direct numerical simulation
• Homogeneous isotropic turbulence• cubic lattice• Taylor-scale Reynolds number • Two million Lagrangian particles• Sampling rate • • Data available from Cineca supercomputing
centre, Bologna, Italy
07.0
31024
280R
¿́ = 3:3¢10¡ 2, TL = 1:2, ´ = 5¢10¡ 3, L = 3:14, " = 0:81, C0 = 5:2
DNS exit time pdfs
• No power law scaling for • Mean exit time lies within power law scaling
range for – relative velocity of average pair decreases faster than
decorrelation time scale – majority of pairs separate diffusively
• Exponential decay of tail agrees with diffusive behaviour for – only slow separators are diffusive– observed with low probability
• Self-similarity of tail decreases with increasing • For tail of pdf affected by and L• Tail of pdf for is ‘stretched’ version of
tail for
2
075.1
2
075.12
075.1
Richardson’s constantScaling of exit time moments according to K41
Since Cn(½) = Fn(½)k¡ n0 and g= 1144=81k3
0 weget
htn i = Cn(½)r2n=3="n=3
Require model to relate Cn(½) to g
Richardsons di®usion equation with K (r) = k0"1=3r4=3
g =114481
r2
"
µFn(½)htn i
¶3=n
Richardson’s constant II
• Finite duration of simulation– slowest separators do not have time to reach large r
• Statistical noise
• Intermittency
• Velocity memory– little impact on higher positive moments– likely to affect negative moments
² g calculated from mean exit timeappears to be independent of ½
² ´ and L e®ects
{ extent of plateau increases with decreasing ½
{ greater e®ect for ½À 1 than for ½¡ 1¿ 1
{ h1=t3i independent of mean dissipation rate{ small but a®ects ½¡ 1¿ 1 more than ½À 1
{ statistics for decreasing ½and r increasingly noisy
Richardson’s constant from negative moments
Cn(½) = An(½)g¡ n=3
Dimensional arguments ) Cn(½) / k¡ n0
g=r2
"
µht¡ n iA¡ n
¶3=n
A¡ n calculated from stochastic di®erential equationcorresponding to di®usion equation
Richardson’s constant from negative moments II
• Exit times for DNS larger (slower) than for diffusive process
• Inverse exit times for DNS smaller than for diffusive process
g will decreasewith decreasing ½
) h1=ti factor of ½¡ 1 too small
g» (½¡ 1)3 for ½¡ 1¿ 1
² Since T̂B is correct timescale for DN S for ½¡ 1¿ 1
² g calculated from h1=ti scales like
Lagrangian stochastic model
• Quasi-one-dimensional
• Magnitude of separation calculated from longitudinal relative velocity
• Treat r and vr jointly as continuous Markov process
• Assume infinite inertial subrange
• C0 enters model explicitly
– can study effects of velocity memory
Lagrangian stochastic model II
• Pdf of Eulerian velocity difference– weighted sum of three Gaussians– constructed such that first three
moments are consistent with K41
a0 = C0dlnf E
d»¡
73f E
Z »
¡ 1»0f E (»0) d»0
d»="1=3
r2=3a0(»)dt +
"1=6
r1=3
p2C0dW(t)
dr = ("r)1=3»dt
Drift term Diffusion term
»= (vr =r)1=3
² Error larger for smaller ½² Error decreases monotonically with n for ½= 2
² For ½= 1:075 error decreases monotonically only for n > 1
² Mean invariant to ½
² Error decreases with increasing C0
Richardson’s constantcalculated from positivemoments
² Error largest for second order moment for ½= 1:075
Richardson’s constant from positive moments II
g =114481
r2
"
µFn(½)htn i
¶3=n
Richardson’s constant calculated from
For di®usiveprocess Fn(½) and htn i scale like½¡ 1
) g» (½¡ 1)3(1¡ n)=n
For ½¡ 1¿ 1
For ballistic process htn i scales like (½¡ 1)n
Independent of ½for n = 1
Conclusions
• Physics of separation process intimately related to spacing of thresholds
• Kinematic simulation reaches its diffusive limit earlier than real turbulence
• In real turbulence velocity memory is important
• Spacing of thresholds and order of moment important for calculating Richardson’s constant
di®usive limit reached only for large½