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Optimum forest program when the carbon sequestration service of a forest has value

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Abstract

This paper develops an optimum forest program for even-aged and multi-age forest management when the carbon sequestration service of a forest has value. It is shown that for even-aged forest management, the optimum rotation might be longer or shorter than when the carbon sequestration service is not considered. For multi-age forest management, it is shown that the optimum steady state is characterized by the optimum rotation for an even-aged forest. The optimum rotation is affected by how to evaluate the carbon release after harvesting, which is a central concern for the issue of “harvested wood products” in the United Nations Framework Convention on Climate Change.

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Notes

  1. We abstract from uncertainty in this study. For a stochastic version of the Faustmann formula, see Miller and Voltaire (1983). Some comparative statics results can be found in Akao (1996). Kitabatake (2002) takes into account the fluctuations of the revenues from logging and the recreational activities in the real option analysis of the forest road construction project.

  2. As seen in the proof of Lemma 5 in the Appendix, the maximand of the right hand side of Eq. (6) is unique.

  3. See, for example, Akao (2003).

  4. For a more accurate conclusion, we have to take into account the carbon left at harvest sites and the carbon stored in wooden wastes.

  5. A continuous time model for a multi-age forest was studied by Heaps (1984) as an optimum control problem with delay. If we employed the continuous time counterpart of our model, we would have to deal with a system of functional differential equations, which is rather technical (Aniţa et al. 1998; Feichtinger et al. 2003).

  6. Formally, we just need a state space with a finite dimension. Thus, we can alternatively assume, for example, that the value of F i begins to decline at a certain age as Mitra and Wan (1985) assumed.

  7. In this section, we assume that part of the sequestered carbon is released immediately at the moment of harvesting but the remainder is never to be released. We have discussed the alternative assumption that all of the sequestered carbon is released in the future with its impact being discounted as a result of elapse of time between harvesting and carbon release. The two assumptions are certainly equivalent in the static model with the stationary assumption made in previous sections, but not in this dynamic model.

  8. Also see Wan (1993) and Nishimura and Yano (1995).

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Acknowledgments

I am grateful to Nobuyuki Yamamoto, the participants of the GIARI workshop at Waseda University, the Association for Public Economic Theory at Hanyang University, and the seminar at University of Hawaii at Manoa, and an anonymous referee of the Journal for their helpful comments. Partial financial support from JSPS Grants-in-Aid for Scientific Research (GCOE-E11, 18078004, 19530161) is gratefully acknowledged.

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Correspondence to Ken-Ichi Akao.

Appendix: Proof of Proposition 1

Appendix: Proof of Proposition 1

To prove the proposition, we prepare a series of lemmas. Define:

$$ \Upphi(T;\beta)=r^{-1}( 1-{\text{e}}^{-rT}) (1-\beta)g(T)+\beta G(T)-\int\limits_{0}^{T}g(t)\,{\text{e}}^{-rt}\,{\text{d}}t. $$
(48)

Lemma 1

The sign of dV C(T)/dT is the same as the sign of \(\Upphi(T;\beta)\).

Proof

This follows from:

$$ \frac{{\text{d}}V^{{\text{C}}}(T)}{{\text{d}}T}=\frac{r\,{\text{e}}^{-rT}}{( 1-{\text{e}}^{-rT}) ^{2}} \Upphi(T;\beta). $$
(49)

\(\square\)

Let:

$$ k=-\lim_{t\rightarrow\infty}g^{\prime}(t)/g(t)\in(0,\infty]. $$
(50)

Lemma 2

The graph \(\left( T,\Upphi(T;\beta)\right) \) is either strictly increasing or unimodal. If β ≥ k/(r + k), then \(\partial\Upphi(T;\beta)/\partial T>0\) for all T > 0. If β < k/(r + k), then there exists T o > 0 such that T o > T I and \(\partial\Upphi (T;\beta)/\partial T\,\gtrless\, 0\) if \(T\,\lessgtr\, T^{o}\).

Proof

The statement follows from:

$$ \frac{\partial\Upphi(T;\beta)}{\partial T}=\frac{1-{\text{e}}^{-rT}}{r}(1-\beta )g(T)\left[ \frac{g^{\prime}(T)}{g(T)}+\frac{r\beta}{1-\beta}\right]. $$
(51)

Note that \(\Upphi(0;\beta)=0\) and \(\partial\Upphi(T;\beta)/\partial T>0\) for all \(T\in\lbrack0,T_{I}]\) because \(g^{\prime}(T)\geq0\) in the interval. Furthermore, note that \(g^{\prime}(T)/g(T)\) is strictly decreasing and converges to −k as \(T\rightarrow\infty\) by assumption A2(d). Finally, \(k\leq r\beta/\left( 1-\beta\right)\) is equivalent to β ≥ k/(r + k). \(\square\)

Recall \(\tilde{\Upphi}\) defined in Eq. (5) in the main text.

Lemma 3

(a) If the carbon release factor β satisfies \(\beta\geq\tilde{\Upphi}\) , then dV C(T)/aT > 0 for all T > 0 and \(T^{C}=\infty\) . (b) If \(\beta\in\lbrack0,\tilde{\Upphi})\) , then there is a unique carbon forest rotation \(T^{\text{C}}\in(T_{I},\infty)\) such that \({\text{d}}V^{{\text{C}}}(T)/{\text{d}}T\,\gtrless\, 0\) if \(T\,\lessgtr\, T^{{\text{C}}}.\)

Proof

By Lemmas 1 and 2 and since \(\Upphi(0;\beta)=0, \) the existence of T C depends on the sign of:

$$ \lim_{T\rightarrow\infty}\Upphi=\beta\lim_{T\rightarrow\infty}G(T)-\int\limits_{0}^{\infty}g(t)\,{\text{e}}^{-rt}\,{\text{d}}t=\lim_{T\rightarrow\infty}G(T)( \beta -\tilde{\Upphi}). $$
(52)

That is, if \(\lim_{T\rightarrow\infty}\Upphi\geq0,\) then dV C(T)/sT > 0 and \(T^{\text{C}}=\infty.\) If \(\lim_{T\rightarrow\infty}\Upphi<0,\) then there is \(T^{\text{C}}\in(T_{\text{I}},\infty)\) such that \(\Upphi(T;\beta)\,\gtrless\, 0\) if \(T\,\lessgtr\, T^{\text{C}}.\) Note that \(\lim_{T\rightarrow\infty}G(T)>0\) by Assumption A2.\(\square\)

Define function \(\Uppsi(T)\) by:

$$ \Uppsi(T)=r\frac{\partial\Upphi(T;\beta)}{\partial\beta}=-g(T)(1-{\text{e}}^{-rT})+rG(T). $$
(53)

Lemma 4

(a) The carbon forest rotation T C as a function of β is continuously differentiable on \(\beta\in\lbrack0,\tilde{\Upphi})\) . (b) The sign of T C/∂β is the same as the sign of \(\Uppsi(T^{{\text{C}}})\) for all \(\beta\in\lbrack0,\tilde{\Upphi})\).

Proof

Fix \(\beta\in\lbrack0,\tilde{\Upphi}). \) Then, there is unique T C(>T I) by Lemma 3. By the total derivative of the first-order condition:

$$ \frac{{\text{d}}V^{{\text{C}}}(T^{{\text{C}}})}{{\text{d}}T}=\frac{{\text{e}}^{-rT^{{\text{C}}}}}{\left( 1-{\text{e}}^{-rT^{{\text{C}}}}\right) ^{2}}\Upphi(T^{{\text{C}}};\beta)=0, $$
(54)

we have:

$$ \frac{{\text{d}}^{2}V^{{\text{C}}}(T^{{\text{C}}})}{{\text{d}}T^{2}}{\text{d}}T^{{\text{C}}}+\frac{{\text{e}}^{-rT^{{\text{C}}}}}{\left( 1-{\text{e}}^{-rT^{{\text{C}}}}\right) ^{2}}\Uppsi(T^{{\text{C}}})\,{\text{d}}\beta=0. $$
(55)

Because d2 V C(T C)/dT 2 ≠ 0, we have statement (a) by the implicit function theorem. Furthermore, ∂T C/∂β satisfies:

$$ \frac{\partial T^{\text{C}}}{\partial\beta}=-\frac{[ {\text{e}}^{-rT^{\text{C}}}/( 1-{\text{e}}^{-rT^{\text{C}}}) ^{2}] \Uppsi(T^{\text{C}})}{\text{d}^{2}V^{\text{C}}(T^{\text{C}})/\text{d}T^{2}}. $$
(56)

Because d2 V C(T C)/dT 2 < 0, we have statement (b).\(\square\)

Recall T L defined in Eq. (6) in the main text.

Lemma 5

Assume \(\beta\in\lbrack0,\tilde{\Upphi}). \) Then, \(\Uppsi(T)\,\lessgtr\, 0\) if and only if \(T\,\lessgtr\, T_{L}.\)

Proof

Note that \(\Uppsi(0)=0, \lim_{T\rightarrow\infty}\Uppsi(T)>0,\) and:

$$ \Uppsi^{\prime}(T)=g(T)(1-{\text{e}}^{-rT})( r-g^{\prime}(T)/g(T)). $$
(57)

By assumption, A2(d) \(g^{\prime}(T)/g(T)\) is strictly decreasing. Therefore, if \(g^{\prime}(0)/g(0)\leq r,\) then \(\Uppsi^{\prime}(T)>0\) for all T > 0, which implies T L = 0 and \(\Uppsi(T)>0\) for all T > 0. Similarly, if \(g^{\prime }(0)/g(0)>r,\) then \(T_{\text{L}}\in(0,\infty],\) and \(\Uppsi(T)\ \lessgtr\ 0\) if and only if \(T\ \lessgtr\ T_{\text{L}}.\) The proof ends by gathering both cases. \(\square\)

Lemma 6

Assume \(\beta\in\lbrack0,\tilde{\Upphi}).\) Then, T C > max{T IT L}.

Proof

By Lemma 3(b), T C > T I. Then, we show T C > T L. The case of T L = 0 is obvious. For the case of T L > 0, use the fact that T C satisfies:

$$ 0=\Upphi(T^{\text{C}};\beta)=-r^{-1}(1-\beta)\Uppsi(T^{\text{C}})+G(T^{\text{C}})-\int\limits_{0}^{T^{\text{C}} }g(t)\,{\text{e}}^{-rt}\,{\text{d}}t. $$
(58)

Then, we have:

$$ r^{-1}(1-\beta)\Uppsi(T^{\text{C}})=G(T^{\text{C}})-\int\limits_{0}^{T^{C}}g(t)\,{\text{e}}^{-rt}\,{\text{d}}t>0. $$
(59)

Therefore, \(\Uppsi(T^{\text{C}})>0.\) This implies T C > T L by Lemma 5. Therefore, T C > max{T IT L}. \(\square\)

Lemma 7

T C/∂β > 0 for all \(\beta \in(0,\tilde{\Upphi})\) and \(\lim_{\beta\nearrow\tilde{\Upphi}}T^{C}(\beta)=\infty.\)

Proof

Assume \(\beta\in(0,\tilde{\Upphi}).\) Then, T C > T L by Lemma 6. Therefore, \(\Uppsi(T^{\text{C}})>0\) by Lemma 5, which implies ∂T C/∂β > 0 by Lemma 4. Denote by β(T C) the inverse function of T C(β). Using Eq. (48) and the first-order condition \(\Upphi(T^{\text{C}};\beta(T^{\text{C}}))=0,\) we have:

$$ \beta(T^{\text{C}})=\frac{\int\nolimits_{0}^{T^{\text{C}}}g(t)\,{\text{e}}^{-rt}\,{\text{d}}t-r^{-1}( 1-{\text{e}}^{-rT^{\text{C}} }) g(T^{\text{C}})}{G(T^{C})-r^{-1}( 1-{\text{e}}^{-rT^{\text{C}}}) g(T^{\text{C}})}. $$
(60)

Then, \(\beta(T^{\text{C}})\rightarrow\tilde{\Upphi}\) as \(T^{\text{C}}\rightarrow\infty.\) This implies \(\lim_{\beta\rightarrow\tilde{\Upphi}}T^{\text{C}}(\beta)=\infty.\) \(\square\)

Proof of Proposition 1

Propositions 1(a) and (b) follow from Lemma 3. Proposition 1(c) follows from Lemmas 4(a), 6, and 7.\(\square\)

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Akao, KI. Optimum forest program when the carbon sequestration service of a forest has value. Environ Econ Policy Stud 13, 323–343 (2011). https://doi.org/10.1007/s10018-011-0016-0

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