Chapter 9. Natural Resources and Economic Growth. Instructor: Dmytro Hryshko

Similar documents
Chapter 9. Natural Resources and Economic Growth. Instructor: Dmytro Hryshko

One-Sector Models of Endogenous Growth. Instructor: Dmytro Hryshko

Solow Growth Model. Michael Bar. February 28, Introduction Some facts about modern growth Questions... 4

Economic Growth

From Difference to Differential Equations I

Modelling Production

Rice University. Fall Semester Final Examination ECON501 Advanced Microeconomic Theory. Writing Period: Three Hours

Aggregate Production Function. Production. Mark Huggett. Georgetown University. January 11, 2018

Equating output per worker to GDP per capita, the growth rate of GDP per capita

Chapter 5. The Engine of Growth. Instructor: Dmytro Hryshko

Growth. Growth Theory. Mark Huggett 1. 1 Georgetown. January 26, 2018

Economic Growth: Lecture 8, Overlapping Generations

Practice Questions for Mid-Term I. Question 1: Consider the Cobb-Douglas production function in intensive form:

ECON 582: The Neoclassical Growth Model (Chapter 8, Acemoglu)

14.461: Technological Change, Lecture 4 Technology and the Labor Market

Input-biased technical progress and the aggregate elasticity of substitution: Evidence from 14 EU Member States

Econ 7110 slides Growth models: Solow, Diamond, Malthus. January 8, 2017

The Heckscher-Ohlin Model: Brief Review

QED. Queen s Economics Department Working Paper No Oil Stock Discovery and Dutch Disease

Generic Analysis of Endogenous Growth Models

14.05: Section Handout #1 Solow Model

On the Dynamic Implications of the Cobb- Douglas Production Function

Solution to Homework 2 - Exogeneous Growth Models

4.4 The functional distribution of income

Analysis of the speed of convergence

The Solow Model in Discrete Time Allan Drazen October 2017

Online Appendix The Growth of Low Skill Service Jobs and the Polarization of the U.S. Labor Market. By David H. Autor and David Dorn

ECON 581: Growth with Overlapping Generations. Instructor: Dmytro Hryshko

Department of Economics Queen s University. ECON435/835: Development Economics Professor: Huw Lloyd-Ellis

New Notes on the Solow Growth Model

Equilibrium in a Production Economy

ECON Answers Homework #4. = 0 6q q 2 = 0 q 3 9q = 0 q = 12. = 9q 2 108q AC(12) = 3(12) = 500

Lecture 5: The neoclassical growth model

Growth Theory: Review

ECON 402: Advanced Macroeconomics 1. Advanced Macroeconomics, ECON 402. New Growth Theories

Neoclassical Business Cycle Model

Advanced Microeconomics

Master 2 Macro I. Lecture 2 : Balance Growth Paths

Growth: Facts and Theories

Economic Growth: Lecture 9, Neoclassical Endogenous Growth

Assumption 5. The technology is represented by a production function, F : R 3 + R +, F (K t, N t, A t )

Internation1al Trade

General motivation behind the augmented Solow model

EC9A2 Advanced Macro Analysis - Class #1

Part A: Answer question A1 (required), plus either question A2 or A3.

Addendum to: New Trade Models, Same Old Gains?

Macroeconomics II Dynamic macroeconomics Class 1: Introduction and rst models

Factor Substitution, Income Distribution, and Growth in a Generalized Neoclassical Model

Markov Perfect Equilibria in the Ramsey Model

The Solow Model. Prof. Lutz Hendricks. January 26, Econ520

Intermediate Macroeconomics, EC2201. L2: Economic growth II

Structural change in a multi-sector model of the climate and the economy

Lecture 1: Ricardian Theory of Trade

The Ramsey Model. (Lecture Note, Advanced Macroeconomics, Thomas Steger, SS 2013)

Macroeconomics IV Problem Set I

Business Cycles: The Classical Approach

ECON 582: Dynamic Programming (Chapter 6, Acemoglu) Instructor: Dmytro Hryshko

Growth Theory: Review

Chapter 2. The Solow Growth Model

Economic Growth: Lecture 7, Overlapping Generations

Lecture 04 Production Theory

RBC Model with Indivisible Labor. Advanced Macroeconomic Theory

DEPARTMENT OF ECONOMICS Fall 2015 P. Gourinchas/D. Romer MIDTERM EXAM

Topics in Trade: Slides

ECON 5118 Macroeconomic Theory

Dynamic Macroeconomics: Problem Set 4

Lecture 1: The Classical Optimal Growth Model

z = f (x; y) f (x ; y ) f (x; y) f (x; y )

Lecture 3 - Solow Model

The Contribution Rate of Thrice Industrial Agglomeration to Industrial Growth in Ningxia The Calculate Based on Cobb-Douglas Function.

Factor-Eliminating Technical Change

Aggregate Supply. Econ 208. April 3, Lecture 16. Econ 208 (Lecture 16) Aggregate Supply April 3, / 12

Toulouse School of Economics, M2 Macroeconomics 1 Professor Franck Portier. Exam Solution

problem. max Both k (0) and h (0) are given at time 0. (a) Write down the Hamilton-Jacobi-Bellman (HJB) Equation in the dynamic programming

Macroeconomics Field Exam. August 2007

THE SOLOW-SWAN MODEL WITH A NEGATIVE LABOR GROWTH RATE

On Stollery s Maximin Model of Global Warming

Two-Level CES Production Technology in the Solow and Diamond Growth Models

Advanced Macroeconomics

TOBB-ETU - Econ 532 Practice Problems II (Solutions)

Simple New Keynesian Model without Capital

Economic Growth: Lecture 13, Directed Technological Change

Problem 1 (30 points)

3 GROWTH AND CAPITAL ACCUMULATION: THE SOLOW MODEL

Indivisible Labor and the Business Cycle

The Solow Growth Model

Mathematics Review Revised: January 9, 2008

Endogenous Growth: AK Model

Exercise Problems for Economic Growth

Lecture 2: Factor Proportions Theory of Trade

CROSS-COUNTRY DIFFERENCES IN PRODUCTIVITY: THE ROLE OF ALLOCATION AND SELECTION

NBER WORKING PAPER SERIES ENERGY-SAVING TECHNICAL CHANGE. John Hassler Per Krusell Conny Olovsson

Chapter 9 Solow. O. Afonso, P. B. Vasconcelos. Computational Economics: a concise introduction

A Global Economy-Climate Model with High Regional Resolution

The Solow Growth Model

R&D Policy in Economies with Endogenous Growth and Non-Renewable Resources

Introductory Microeconomics

Closed economy macro dynamics: AD-AS model and RBC model.

Economics 202A Lecture Outline #3 (version 1.0)

Transcription:

Chapter 9. Natural Resources and Economic Growth Instructor: Dmytro Hryshko

Motivation We want to understand growth in the presence of the earth's nite supply of arable land and nonrenewable natural resources (e.g., oil and natural gas). In the Solow model, the presence of natural resources reduces the long-run growth rate of the economy. Perhaps, the size of this reduction was not that big, at 0.3%.

Land in the Solow model Let T be the (xed) amount of land available for production in each period. Aggregate production function is: Y = BK T L 1 ; where 0 < < 1 and + < 1. B is an index of technological progress. Production function is constant returns to scale in K, L, and T (replication argument). Furthermore, _B B = g B; _L L = n; _K = sy K: Along a balanced growth path, the growth rates of K=L and Y =L are constant and equal. Thus, K=Y should be constant.

Balanced growth path with land in the Solow model Dividing production function through by Y, we obtain Y 1 = B K 1 Y T L 1, and so Y = B 1 K 1 Y T 1 L 1 1. Since we assumed that T is constant, along the balanced growth path, when K=Y is constant, total output grows at the rate g Y = g B 1 + (1 1 )n. The growth rate of output per worker, therefore, is g y = g B 1 1 n = g n, where g g B 1 and 1. The long-run growth rate of the economy now depends on population growth, n, and the importance of land in production,. There is a \race" between technological progress and the diminishing returns due to the xed amount of land. There are decreasing returns to K and L in the presence of a xed supply of land. Absent technological progress, when g = 0, the growth rate of output per worker is negative, and output per worker will approach zero in the very long run. The growth rate in B may potentially oset the pressure of population on the xed resource and lead to sustained growth in output per worker. The more important is land in production (the higher is ), the lower the long-run growth will be: in this case, the diminishing returns to capital and labor are stronger.

Nonrenewable resources Land was in xed supply but not subject to depletion. Introduce natural resources used in production that can be depleted (e.g., natural gas, coal, oil). Suppose the aggregate production function is constant returns to scale in E, L and K: Y = BK E L 1 ; where E is the amount of energy used in production, and + < 1. Let the initial amount of resource be R(0). The stock of resource is depleted as: _R = E. Assume that a constant fraction of the remaining stock of resource is used for energy production each period: E = s E R, 0 < s E < 1. Thus, _R = E = s R R E, and R(t) = R(0) exp( s E t). Since E(t) = s E R(t), E(t) = s E R(0) exp( s E t) the stock of remaining energy and the amount of energy used in production decline over time at the rate s E.

The balanced growth path We can express the production function as Y = B 1 1 K 1 E 1 Y L 1 1, or Y = B 1 1 K 1 (s Y E R(0) exp( s E t)) 1 L 1 1. Along the balanced growth path, Y grows at the rate g B s 1 E + n 1. Thus, the growth rate of output 1 1 per worker, along the balanced growth path, is g y = g B (s 1 1 E + n) = g (s E + n), where g = g B and 1 = 1. Higher population growth leads to increased pressure on the nite resource stock and reduces the growth in output per worker. An increase in the depletion rate, s E, reduces the long-run growth rate of the economy.

Quantifying the importance of natural resources The accumulation of capital and labor runs into diminishing returns since land and nonrenewable resources are in limited supply. For a model with both xed land and nonrenewable resources, the growth rate in output per capita is: g y = g ( + )n + s E : {z } growth \drag" Nordhaus (1992): = 0:1, = 0:1, = 0:2, n = 0:01, and s E = 0:005, where, for example, is the land's share of output (payments to land as a share of GDP). Thus, the growth \drag" is estimated at about 0.0031 annual per capita growth of output in the U.S. is about 0.31% lower due to the presence of a xed supply of land and depletable resources.

The importance of natural resources Is the annual \loss" of 0.31% large or small? A quantity, growing at 0.31%, will double in about 225 years. Consider the following question: If you start with income y 0, how much would you be willing to pay annually to have your income growing at 2.1% instead of 1.8%? For an interest rate r = 0:06, you will be willing to pay at most 7.1% of annual income.

Prices as indicators of scarcity Suppose the production function is Y = K T E L 1. In competitive factor markets, each factor is paid its marginal product. For example, R = F K = Y. The share of output K paid to capital is v K = RK =. Similarly, v Y T =, v E =, v L = 1. The Cobb-Douglas function implies that all shares are constant over time. However, in the data, v T and v E are falling over time. Note that a factor scarce in supply but high in demand will have a high price. v E v L = P EE=Y = P EE. Thus, P E = v E=v L. As wl=y wl w E=L L grows and E gets depleted, E becomes relatively scarce and, for constant income shares v E and v L, the price of nonrenewable resources should rise relative to the price of labor. The same applies to the relative price of land, P T =w.

Data surprises In the U.S. data for fossil fuels (oil, natural gas and coal), P E =w is falling, perhaps, because v E is falling, and E=L is rising (maybe, world continues to discover new deposits of fossil fuels).

Implications and explanations of declining factor shares To explain the declining resource share in output, we will use the Constant Elasticity of Substitution (CES) production function. With only two factors of production, capital and energy, the production function is: Y = F (K; E) = (K + (BE) ) 1= ; where B is an index of technology.

Elasticity of substitution Elasticity of substitution is dened as ( K E )=( K E ) T RS=T RS, where T RS is the technical rate of substitution (the slope of isoquant). Note that Y F K K + F E E, and dene K + (BE) z. Thus, Y = z 1= 1 K 1 K + z 1= 1 B E 1 E. Along the isoquant, Y = 0, and so T RS = K E = B K 1. E The percentage change in T RS can be calculated from d ln jt RSj, and the percentage change in K E as d ln K E. ln jt RSj = B 1 + (1 ) ln K E, or ln K E = 1 1 ln jt RSj 1 B 1. Since ( K E )=( K E ) T RS=T RS = d ln( K E ) d ln jt, the elasticity of substitution,, is equal to RSj 1 1. Note that if = 0, jt RSj = K E, and the elasticity of substitution is equal to 1. The elasticity of substitution is greater than 1 if 0 < < 1 and less than 1 if < 0. Higher values of imply greater substitutability between the factors of production: e.g., when = 1, = 1.

Energy's share The share of energy in output, provided the markets are competitive, is v E = F EE Y. FE = 1 B E 1 (K + (BE) ) 1 1. And so v E = F EE Y = B E (K +(BE) 1 ) 1 B 1 = E 1 = BE. Y Empirically, (K +(BE) ) (K +(BE) ) E Y is falling over time. If > 0 and B is not growing rapidly, the share of energy will decline over time: _v E v E = _B B {z} + _E Y +. E=Y {z } Intuition: if > 0, energy and capital become more substitutable; when energy becomes relatively more expensive, more capital is used to produce the same amount of output; the output share of a more plentiful factor will increase; and energy is not a necessary input into production. However, it might be hard to use capital instead of energy, and energy must be a necessary input. If < 0, factors are less substitutable; energy is a necessary input; the share of the relatively scarce factor should increase but...the things turn around if energy-specic technological change, B, changes energy from an \increasingly scarce factor" to an \increasingly plentiful factor."

Energy's share, contd. In the U.S. data, the ratio E Y declined by a factor of 2 between E 1949 and 1999, implying that an annual growth rate of Y was about {1.4%. If < 0, for v E to be falling over time, the energy-specic technological change should have been increasing at a rate higher than 1.4%. It sounds quite plausible, taking into account that, in the presence of depletable resources, energy-saving research would be particularly protable.