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A new variational technique for direct and inverse problems of - - PowerPoint PPT Presentation

A new variational technique for direct and inverse problems of atmospheric chemistry V.V. Penenko Institute of Computational Mathematics and Mathematical Geophysics SB RAS 630090, Novosibirsk Goal to derive effective and concordant


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A new variational technique for direct and inverse problems

  • f atmospheric chemistry

V.V. Penenko

Institute of Computational Mathematics and Mathematical Geophysics SB RAS 630090, Novosibirsk

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SLIDE 2

Goal

to derive effective and concordant algorithms for realization of both the direct and adjoint problems for analysis of comprehensive chemical mechanisms, parameter estimation techniques, data assimilation, etc.

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Flux Corrected Transport (FCT) Schemes/ Monotony algorithms

  • The mesh refinement schemes
  • The monotone interpolation routines
  • Overlapping and moving grids
  • Richardson extrapolation
  • Romberg’s method
  • “Mother” domain- “daughter” domain interactions
  • Averager procedures
  • “Smoother-dismoother”
  • Non-linear renormalization
  • “Lagrangian-type” monotonization
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SLIDE 4

Flux Corrected Transport (FCT) Schemes

  • Richardson (1910)
  • Romberg (1955)
  • Godunov S.K. (1959)
  • Gol’din V.Ya, Kalitkin, Shishova (1965)
  • Van Leer (1974-79) self-limiting diffusion, Taylor’s series

expansion

  • A.Harten et al (1978-87) TVD, ENO
  • Tremback et al (1987) Non-linear renormalization
  • A.Bott ( 1989) Non-linear renormalization
  • Smolarkiewicz and Grell (1992)
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Critique of FCT schemes

  • non-linear with respect to the state function;
  • explicit ( in most cases);
  • non-differential in classical sense ( flux

correction, logical operators)

  • self-diffusive;
  • each component of the state function

defines own character of approximating

  • perator
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SLIDE 6

grad div = − − + − + ∂ ∂ ≡

i i i i c i i

r t f S c c t c L

i

) (x, ) ( ) u ( ϕ ϕ µ π π

i

f - source term

i

S ) ( ϕ - operator of transformation, } ; { D x t t Dt ∈ ≤ ≤ = r

.

} , {

,

m i ci 1 = = ϕ

  • state function

Boundary and initial conditions

Model of transport and transformation of pollutants

( )

, ( , ) ( ,0) ( )

i t i

R q t = ∈Ω = x x x ϕ ϕ ϕ

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SLIDE 7

( ) ( )

i i i i

L P Q t ϕ ϕ ϕ ∂ + − = ∂ r r

1

ˆ ( ) , , ( )

j j j j t

t t t t Q D ϕ ϕ ϕ

+

= ≤ ≤ ∈ r r r

{ }

, 1, , 1

i i

n n ϕ ϕ = = ≥ r , 0

j

t t t τ τ = + ≤ ≤ ∆ ( )

i

L ϕ r

loss operators

( )

i

P ϕ r

production operators

i

Q sources and sinks of pollutants

The space co-ordinates are parametrically taken

t

x D ∈ r

Splitting stage: transformation

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SLIDE 8

Properties of operators and functions

0, ( ) 0, ( ) 0, ( ) ( ) , ( ) ( ), ( )

i i i i i i i i

L P L L L ϕ ϕ ϕ ϕ ϕ ϕ α ϕ ϕ α ϕ ≥ ≥ ≥ = = ≥ r r r r r r r r % %

Monotony is qualifying standard: the state functions have to be positive if

i

Q ≥ .

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SLIDE 9

S-stage Runge-Kutta method

1 1 1

, , , ( , , , )

s j j j j j j j j s j j j j jq q j q

t b k T t c t t a k k F Y T ϕ ϕ ϕ

+ = =

= + ∆ = + ∆ Ψ = + ∆ = Ψ

∑ ∑

x %

, ,

jq j j

a b c

parameters

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SLIDE 10

S-stage Rosenbrock methods

1 1 1 1 1 1

, , , 1 ( , , , ) ( , , , ) ( , , , ), , , , , , parameters

s j j j j j j j j j j j jq q q j j j j j jj j jq j q j q j jq jq j jj j

t b k T t c t t a k E J t Y k F Y T t c k t F Y T t t b a c c ϕ ϕ ϕ ϕ γ γ ϕ γ γ

+ = − = − =

= + ∆ = + ∆ Ψ = + ∆   − = Ψ +   ∆   ∂ + ∆ ∆ ∂ −

∑ ∑ ∑

x x x % %

J

Jacobian matrix of derivative functions of F

%

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SLIDE 11

Variational form of the model

( ) ( , , ) F t Q t ϕ α ϕ ϕ ϕ ∂ + = ∂ r

( )

* * * * *

( ) ( )

t t t

F d t F d t ϕ α ϕ ϕ ϕ τ ϕ α ϕ ϕ ϕ ϕ τ ϕϕ

∆ ∆ ∆

∂   + − =   ∂       ∂ − + − +     ∂    

∫ ∫

r r

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SLIDE 12

Local adjoint problem

* * * * 1

( ) 0, 1

j t t

t ϕ α ϕ ϕ ϕ ϕ

+ =∆

∂ − + = ≡ = ∂ r

The function

*( )

ϕ τ is chosen from the conditions:

* * 1 ( )

( )

j t

e α

τ

ϕ τ ϕ

+ − ∆ −

=

t τ ≤ ≤ ∆

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Balance relations

( )

1

* *

( , , ) ( )

j j

t t t

F t Q d ϕ ϕ τ τ ϕϕ

+

+ =

1 * *

( , , ) ( )

t j j j

F t Q d ϕ ϕ ϕ ϕ ϕ τ τ

∆ + =

+∫

( )

( ) ( , , ) , 0

j

e e F Q d t

τ ατ α τ τ

ϕ τ ϕ τ ϕ τ τ

′ − − −

′ ′ = + ≤ ≤ ∆

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The second order monotonic scheme

( )

/ 2 1 / 2 1 2 / 2 1 1 2 1 / 2 1 1 / 2

1 2 ( , , ), ( , ) 1

t j j t t t j j j j j t j j t t

e t e f e f f F t Q f F t e e f t

α α α α α α α

ϕ ϕ ϕ ϕ ϕ ϕ

− ∆ + − ∆ − ∆ ∆ + + − ∆ + − ∆ ∆

− ∆ = + + = = − = + ∆ % %

Монотонный характер схемы при

α ≥

непосредственно следует из свойств неотрицательности всех сомножителей слагаемых.

При

α ≡

получается аналог формулы Рунге-Кутта

2

( )

  • t

.

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SLIDE 15

The forth order monotonic scheme

( )

( )

1 / 2 1 2 3 4 / 2 1 1 1 / 2 2 1 2 2 / 2 3 2 3 3 4 3

2 6 ( , ), 2 ( , ), 2 2 ( , ), 2 ( , )

j j t t t j j t j j t j j t t j j

t e f e e f f f t f F t f e t t f F t e f t f F t e tf e f F t t

α α α α α α α

ϕ ϕ ϕ η ϕ η η ϕ η η ϕ η

+ − ∆ − ∆ − ∆ − ∆ − ∆ − ∆ − ∆

∆ = + + + + ∆   = = +     ∆ ∆ = + = + ∆ = + = + ∆ = + ∆

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Variational form of transformation model for multi-stage algorithms ( the 2nd order)

( )

{

( )

( )

( )

( )

}

1 * 1 * 1 1 2 1 1 * 1 * 1 1 2 1 2 * 1 * 1 / 2 / 2 / 2

( , , ) ( , ) ( , ) ( , ) 0, 1 , , 2 1

i i i i i

n J j j j tr i i i i i i i i i j j j i i j i i i j i j j i i p i i i i i i i t t i i i t t i

I Y H U f W f f F t f f F t f L H V f t e t W U W e e V

α α α α α

ϕ ϕ ϕ ϕ ϕ ϕ ϕ α ϕ κ α ϕ ϕ ϕ

− + + = = + + + − ∆ − ∆ ∆ − ∆

  ≡ − − +   + − + − + − + − − ∆ = − ∆ = = − =

∑∑

r r r r r % r r r % % % ,

i t

i t

t H e t

α − ∆ ∆

∆ = ∆

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SLIDE 17

Adjoint transformation problem

( )

* * 1 2 1 * 1 * 2 1 1 * * 1 * 1 1 * * 1 * 1 1 1 * * 1 * 1 * 1

, ( ) ( ) (

j i i i j n j k i k j k i j j i i i i i j j j j i i i i i i i i i i i i i i i i i j j j j j k k i i i i k j i

f W F f f U V H U W H V f f F L H f ϕ ϕ ϕ ϕ ϕ ϕ α ϕ ϕ ϕ ϕ α α α α α ϕ ϕ ϕ ϕ ϕ ϕ

+ + + + = + + + + + +

= ∂ = ∂ = +       ∂ ∂ ∂ ∂ ∂ = + + + +       ∂ ∂ ∂ ∂ ∂       ∂ ∂ = + + + ∂

r % % % % % r r % %

* 1

) 1,

n k j k i

i n α ϕ

=

    ∂   =

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Sensitivity relations for transformation problem

( )

* Y 1

( , , ) ( ) grad ( ),

N tr k k k

I Y Y Y Y ϕ ϕ δ ϕ δ ϕ δ

=

∂ Φ = = Φ ∂

r

r r r r %

{ } ( )

{ }

, 1, , , , 1, , 1, , 1,

j k i i q q

Y Y k N Q q n i n j J ϕ κ = = = = = = r

Feedback equation

k

Y

grad ( ), 1,

k

dY k N dt ϕ = Φ = r

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SLIDE 19

Sensitivity relations

}

}

1 * 1 1 1 * * 1 2 1 * * *0 1 2

( ) ( ) ( )

k k

q n J j i q i i j q q j j q i i q i q i q q q i i i i i i

L F F f f Q f Q f t δ ϕ δκ α κ ϕ ϕ δκ δκ κ κ δ δ δϕ δϕ

− = = = =

  ∂   Φ = − +   ∂       ∂ ∂ + + +     ∂ ∂   + ∆ +

∑ ∑ ∑ ∑

% r r r %

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HCOOH O HOCH O HOCH OH CH NO O CH O NO HO O CH HO NO CO CO HCO CO H CH O CH CH CH OH O h OH O NO NO HO O OH ONO CH OOH H C

→ → ↓ ↓ ↓ → → → → → → → ↑ ↑

2 2 2 3 2 2 3 2 2 2 2 2 2 2 3 2 3 3 4 2 2 2 2 2 2 3 3

, , ν

Methane transformation in the atmosphere

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Daily behavior of transformation products in methane-nitrogen-sulfur cycle

54 substances and 170 equations

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Conclusion

  • The universal technique for construction of algorithms

for direct and adjoint atmospheric chemistry problems is proposed.

  • The new schemes hold the properties of unconditional monotony

and are efficiently realized.

  • A new way for construction of variational principles

for multi-stage recursive algorithms is proposed. It gives the possibility of simple realization of adjoint problems and sensitivity studies.

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Acknowledgements

The work is supported by

  • RFBR

Grant 07-05-00673

  • Presidium of the Russian Academy of Sciences

Program 16

  • Department of Mathematical Science of RAS

Program 1.3.

  • European Commission

contract No 013427