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{{Dimensions
{{Dimensions
|nd        = 1
|nd        = 1
|nx        = 1
|nx        = 3
|nw        = 1
|nw        = 2
}}
}}


The '''Ocean problem''' describes fossil fuel consumption and sequestration into the ocean [169]. It is a
The '''Ocean problem''' describes fossil fuel consumption and sequestration into the ocean [[#PersonalComm | [1]]]. It is a
two box model where <math>S</math> describes the carbon stock in the atmosphere and upper layer ocean,
two box model where <math>S</math> describes the carbon stock in the atmosphere and upper layer ocean,
<math>R</math> describes the carbon stock in fossil reserve and <math>D_L</math> the carbon stock in the deeper layer. The dynamics are given by an [[:Category:ODE model|ODE model]].
<math>R</math> describes the carbon stock in fossil reserve and <math>D_L</math> the carbon stock in the deeper layer. The dynamics are given by an [[:Category:ODE model|ODE model]].
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<math>
<math>
  \begin{array}{lll}
  \begin{array}{lll}
  \displaystyle \min_{w} && y(t_f) \\
  \displaystyle \min_{w} && -y(t_f) \\
  \text{subject to} \\
  \text{subject to} \\
\quad \dot{y}(t) & = &  \exp(-\rho \cdot t) \cdot (U(t)- A(t) - u_1(t) \cdot C(t) - D(t)),\\
\quad \dot{y}(t) & = &  \exp(-\rho \cdot t) \cdot (U(t)- A(t) - u_1(t) \cdot C(t) - D(t)),\\
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\quad y(0) &=& 0, \\
\quad y(0) &=& 0, \\
\quad S(0) &=& 2 \cdot 10^3, \\
\quad S(0) &=& 2 \cdot 10^3, \\
\quad R(0) &=& 10^4  
\quad R(0) &=& 10^4 \\
\quad S(t), R(t) & \in & [0,10^5], \\
\quad u_1(t), u_2(t) & \in & [0,40] \\
   \end{array}
   \end{array}
</math>
</math>
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  \begin{align}
  \begin{align}
   &U(t) = b \cdot u_1(t) - \mu \cdot u_1(t)^2, \quad \quad  
   &U(t) = b \cdot u_1(t) - \mu \cdot u_1(t)^2, \quad \quad  
   & D(t) = \nu \cdot (0.3 \cdot S(t) - S_{\text{preind}})^2, \\
   && D(t) = \nu \cdot (0.3 \cdot S(t) - S_{\text{preind}})^2, \\
   &A(t) = a_1 \cdot u_2(t) + a_2 \cdot u_2(t)^2, \quad \quad
   &A(t) = a_1 \cdot u_2(t) + a_2 \cdot u_2(t)^2, \quad \quad
   & D_L(t) = D_{L, 0} + R_0 + S_0 - R(t) - S(t), \\
   && D_L(t) = D_{L, 0} + R_0 + S_0 - R(t) - S(t), \\
   &C(t) = c_1 - c_2 \cdot R(t). &
   &C(t) = c_1 - c_2 \cdot R(t). &
  \end{align}
  \end{align}
</math>
</math>
</p>
</p>
== Parameters ==
{| class="wikitable"
|+Parameters
|-
|Symbol
|Value
|-
|<math>t_f</math>
|<math>400</math>
|-
|<math>\rho</math>
|<math>0.03</math>
|-
|<math>\gamma</math>
|<math>0.001</math>
|-
|<math>\omega</math>
|<math>0.1</math>
|-
|<math>b</math>
|<math>50</math>
|-
|<math>\mu</math>
|<math>0.5</math>
|-
|<math>a_1</math>
|<math>2</math>
|-
|<math>a_2</math>
|<math>2</math>
|-
|<math>\nu</math>
|<math>1</math>
|-
|<math>c_1</math>
|<math>50</math>
|-
|<math>c_2</math>
|<math>0.004</math>
|-
|<math>S_{\text{preind}}</math>
|<math>600</math>
|-
|<math>S_0</math>
|<math>2000</math>
|-
|<math>R_0</math>
|<math>10^4</math>
|-
|<math>D_{L,0}</math>
|<math>2.3 \cdot 10^4</math>
|}


== Reference Solutions ==
== Reference Solutions ==
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Here is one local solution to the above control problem.
Here is one local solution to the above control problem.


<gallery caption="Reference solution plots" widths="180px" heights="140px" perrow="1">
<gallery caption="Reference solution plots" widths="500px" heights="300px" perrow="1">
  Image:Rao_Mease.png| States and discretized control for a local optimum.
  Image:Ocean.png| States and discretized control for a local optimum. Due to the explicit time dependence the time <math>t</math> was added as an additional state.
</gallery>
</gallery>


== Miscellaneous and Further Reading ==
== Miscellaneous and Further Reading ==
The problem description and further references can be found in the PhD thesis of Michael Ernst Geiger [[#GeigerPhD|[1]]].
The problem description and further references can be found in the PhD thesis of Dennis Janka [[#JankaPhD|[2]]].


== References ==
== References ==
<span id="GeigerPhD">[1]</span> "Adaptive Multiple Shooting for Boundary Value Problems and Constrained Parabolic Optimization Problems" by M. E. Geiger  <br>
<span id="PersonalComm">[1]</span> W. Rickels and S. Sager. Personal communication. 2015. <br>
<span id="JankaPhD">[2]</span> Janka, D.: Sequential quadratic programming with indefinite Hessian approximations for nonlinear optimum experimental design for parameter estimation in differential-algebraic equations. Ph.D. thesis, Ruprecht-Karls-Universität Heidelberg (2015). URL https://mathopt.de/publications/Janka2015.pdf <br>




[[Category:MIOCP]]
[[Category:MIOCP]]
[[Category:Sensitivity-seeking arcs]]
[[Category:Sensitivity-seeking arcs]]

Latest revision as of 10:50, 29 January 2026

Ocean
State dimension: 1
Differential states: 3
Discrete control functions: 2


The Ocean problem describes fossil fuel consumption and sequestration into the ocean [1]. It is a two box model where S describes the carbon stock in the atmosphere and upper layer ocean, R describes the carbon stock in fossil reserve and DL the carbon stock in the deeper layer. The dynamics are given by an ODE model.

The optimal control function exhibits a singular arc.

Mathematical formulation

minwy(tf)subject toy˙(t)=exp(ρt)(U(t)A(t)u1(t)C(t)D(t)),S˙(t)=u1(t)u2(t)γ(S(t)ωDL(t)),R˙(t)=u1(t)y(0)=0,S(0)=2103,R(0)=104S(t),R(t)[0,105],u1(t),u2(t)[0,40]

with auxiliary functions

U(t)=bu1(t)μu1(t)2,D(t)=ν(0.3S(t)Spreind)2,A(t)=a1u2(t)+a2u2(t)2,DL(t)=DL,0+R0+S0R(t)S(t),C(t)=c1c2R(t).

Parameters

Parameters
Symbol Value
tf 400
ρ 0.03
γ 0.001
ω 0.1
b 50
μ 0.5
a1 2
a2 2
ν 1
c1 50
c2 0.004
Spreind 600
S0 2000
R0 104
DL,0 2.3104

Reference Solutions

Here is one local solution to the above control problem.

Miscellaneous and Further Reading

The problem description and further references can be found in the PhD thesis of Dennis Janka [2].

References

[1] W. Rickels and S. Sager. Personal communication. 2015.
[2] Janka, D.: Sequential quadratic programming with indefinite Hessian approximations for nonlinear optimum experimental design for parameter estimation in differential-algebraic equations. Ph.D. thesis, Ruprecht-Karls-Universität Heidelberg (2015). URL https://mathopt.de/publications/Janka2015.pdf