I NTERMEDIATE M ACROECONOMIC T HEORY L ECTURE 2 Simon Fraser University Instructor: Marieh Azizirad Summer 2023 Our plan in this lecture Long-run economic growth Production functions Solow growth model ECON 305 D100 Summer 2023, Lecture 2 2 Long-run economic growth some facts: No growth in the long history. Modern economic growth only emerges in the most recent three centuries. ’The great divergence’. ECON 305 D100 Summer 2023, Lecture 2 3 Long-run economic growth some facts: A growth rate in some variable x is the percentage change in that variable between time t and t + 1: gx = xt+1 −xt xt Examples: Yt+1 −Yt , or Yt Lt+1 −Lt n = Lt , Output growth: gY = Yt+1 = Yt (1 + gY ) Population growth: or Lt+1 = Lt (1 + n) At a constant growth rate, Yt = Y0 (1 + gY )t Lt = L0 (1 + n)t ECON 305 D100 Summer 2023, Lecture 2 4 Long-run economic growth some facts: Ratio scale (or log scale): start with Lt = L0 (1 + n)t in natural logs (ln, sometimes economists write it as log), ln (Lt ) = ln (L0 ) + t ∗ ln (1 + n) for small growth rates n, ln (1 + n) ≈ n therefore: ln (Lt ) = ln (L0 ) + n ∗ t ECON 305 D100 Summer 2023, Lecture 2 5 Long-run economic growth some facts: Ratio scale (or log scale): Rule of 70 → If a variable x is growing at a constant rate equal to gx then it takes variable x to be doubled. 70 gx years for the → The time it takes for income to double depends only on the growth rate, not on the current level of income. ECON 305 D100 Summer 2023, Lecture 2 6 Long-run economic growth some facts: Ratio scale (or log scale): a: Lt = L0 (1 + n)t b: ln (Lt ) = ln (L0 ) + n ∗ t ECON 305 D100 Summer 2023, Lecture 2 7 Long-run economic growth some facts: Ratio scale (or log scale): Some important growth rate rules: Suppose there are three variables x and y with constant growth rates given by gx and gy , then: if z = x ∗ y, then gz = gx + gy ; if z = xy , then gz = gx − gy ; if z = xa , then gz = a ∗ gx ; what if z = a? Note These are easily derived from the log growth equations. ECON 305 D100 Summer 2023, Lecture 2 8 Our plan in this lecture Long-run economic growth Production functions Solow growth model ECON 305 D100 Summer 2023, Lecture 2 9 A model of production ECON 305 D100 Summer 2023, Lecture 2 10 A model of production Production function: Y = F(K, L). A reasonable production function has the following properties so that it fits the real-world production better: More is better: Y increases in K and L (holding the other argument constant); dY MPK = dK > 0 and MPL = dY dL > 0. 2 2 Concavity: Diminishing MPK and MPL; ∂∂ KY2 < 0, ∂∂ LY2 < 0. Duplicable: Constant returns to scale (CRS): for any parameter c > 0, F(cK, cL) = cF(K, L). → Learn the difference between IRS and CRS in the textbook. ECON 305 D100 Summer 2023, Lecture 2 11 A model of production A frequently used example: Cobb-Douglas production function Y = AK α L1−α parameters: A > 0, 0 < α < 1. Exogenous variable: L: labor input (the total number of person-hours worked). K: capital input (the real value of all machinery, equipment, and other capital input). Endogenous variable: Y: total production/output (the real value of all goods produced). Question: Does it satisfy the three properties above? ECON 305 D100 Summer 2023, Lecture 2 12 A model of production Cobb-Douglas production function: Y = AK α L1−α A = 1; α = 0.5 ECON 305 D100 Summer 2023, Lecture 2 13 A model of production Cobb-Douglas production function: Y = AK α L1−α refers to the aggregate variables. Sometimes we use the per capita version of the production function by dividing both sides of the equation by L (why?): L1−α Y = AK α L L → y = Akα y = YL : output per capita or ’living standard’. k = KL : capital per capita. ECON 305 D100 Summer 2023, Lecture 2 14 A model of production Cobb-Douglas production function: What is A? Y = AK α L1−α A is called "Total factor productivity". It is interpreted as efficiency or productivity. It measures how productive countries are using their K and L. There is no measures to collect data on A, therefore it is also referred to as "the residual" or "a measure of our ignorance". ECON 305 D100 Summer 2023, Lecture 2 15 A model of production Cobb-Douglas production function: What is A? y = Akα ECON 305 D100 Summer 2023, Lecture 2 16 A model of production Cobb-Douglas production function: What is α in Y = AK α L1−α ? If input markets are characterized by perfect competition, then profit maximization conditions are: MPL = w → − (1 − α)AK α L−α = w MPK = r → − αAK α−1 L1−α = r w ∗ L = (1 − α)AK α L−α Therefore, ∗ L = (1 − α)Y. So, (1 − α) is the share of total income going to workers, or the labor share of income. Similarly, α is the capital share of income. Empirically, α ≈ 1/3. ECON 305 D100 Summer 2023, Lecture 2 17 Our plan in this lecture Long-run economic growth Production functions Solow growth model ECON 305 D100 Summer 2023, Lecture 2 18 Solow growth model Goal: Study how capital accumulates over time, and how the limitations of capital accumulations leave long-run economic growth unexplained. The Solow model allows us to consider the accumulation of capital as a possible engine of long-run economic growth. Features: Take A (TFP) and L (labor) as given, and endogenize the accumulation of K (capital). Base on the Cobb-Douglas production function. K can be produced through "investment", but also depreciates over time. ECON 305 D100 Summer 2023, Lecture 2 19 Solow growth model Model setup: Assume a closed economy with no government. NX = 0 and G = 0. So, Yt = Ct + It . Assume a constant saving rate at every time period, s ∈ (0, 1). It = s ∗ Yt . Ct = (1 − s) ∗ Yt . Assume a constant depreciation rate, δ ∈ (0, 1). So that total depreciation at time t is δ Kt . ECON 305 D100 Summer 2023, Lecture 2 20 Solow growth model Dynamics of K: Change in K over time; ∆Kt+1 ≡ Kt+1 − Kt = It − δ Kt A side note: flow v.s. stock variables: A flow variable is an economic variable that is measured per period of time. → E.g. Investment, output/income/GDP. A stock variable is an economic variable that is measured at a particular point of time. → E.g. Capital, wealth. ECON 305 D100 Summer 2023, Lecture 2 21 Solow growth model Dynamics of K: Change in K over time; ∆Kt+1 ≡ Kt+1 − Kt = It − δ K t = sYt − δ Kt = sAKtα Lt1−α − δ Kt = [sALt1−α ]Ktα − δ Kt → now we have a dynamic model of capital accumulation: ∆K is a function of K. ECON 305 D100 Summer 2023, Lecture 2 22 Solow growth model Solving the model: The Solow diagram. ECON 305 D100 Summer 2023, Lecture 2 23 Solow growth model Solving the model: The Solow diagram. There is only one point where this dynamic system becomes stable (i.e., K does not change over time anymore). It is when investment equals depreciation and is called the "Steady State" shown by K ∗ . ECON 305 D100 Summer 2023, Lecture 2 24 Solow growth model How about output and consumption? Recall that, It = s ∗ Yt , and Ct = (1 − s) ∗ Yt . There is a steady state Y ∗ and C∗ accordingly. ECON 305 D100 Summer 2023, Lecture 2 25 Solow growth model Solving for K ∗ , I − δ K∗ = 0 sAK ∗α L1−α − δ K ∗ = 0 sAL1−α = K ∗(1−α) δ → K∗ = ECON 305 D100 Summer 2023, Lecture 2 1 1 s 1−α · A 1−α · L δ 26 Solow growth model Solving for Y ∗ and C∗ , Plug K ∗ in the production function, Y ∗ =AK ∗α L1−α s α α 1−α · A 1−α · Lα L1−α =A δ α 1 s 1−α =A 1−α L δ Exercise: Using C = (1 − s)Y solve for C∗ . ECON 305 D100 Summer 2023, Lecture 2 27 Solow growth model Lessons about the steady state: Why does the Solow model eventually reaches a constant level of K ∗ and Y ∗ , no matter where the initial state is? → Diminishing MPK! Diminishing returns to capital accumulation means that each increment of K increases production (and investment) by less and less, but the amount of depreciation rises one-for-one with K. ECON 305 D100 Summer 2023, Lecture 2 28 Solow growth model Lessons about the steady state: y∗ = Y∗ L 1 = A 1−α s δ α 1−α living standards = efficiency * capital intensity ∗ capital intensity: At the S.S.,sY ∗ = δ K ∗ , and thus KY ∗ = δs . power of A, rewrite the equation as, α Y∗ s 1−α = A· A· L δ the direct productivity effect on Y ∗ ; the indirect effect on Y ∗ through K ∗ . (Recall that K ∗ = ECON 305 D100 Summer 2023, Lecture 2 s δ 1 1−α 1 · A 1−α · L) 29 Solow growth model Lessons about the long-run economic growth: There is NO long-run growth via capital accumulation. → Every variable (K, Y, C) eventually converges to a constant level or ’steady state’. Long-run living standards depend on A, s, and δ , not on initial capital or the size of the population. Recall, α 1 s 1−α y∗ = A 1−α δ All long-term growth comes from a constant growth in TFP (A), not even a one time increase in A. ECON 305 D100 Summer 2023, Lecture 2 30 Solow growth model Lessons about the long-run economic growth: Some experiments on A, s, and δ , and their effect on the economy. A permanent increase in s: ECON 305 D100 Summer 2023, Lecture 2 31 Solow growth model Lessons about the long-run economic growth: Some experiments on A, s, and δ , and their effect on the economy. A permanent increase in s increases the level of income permanently, but affect income growth only temporarily. The long-run economic growth eventually goes back to 0. Exercise: Change other parameters and see what happens. ECON 305 D100 Summer 2023, Lecture 2 32 Solow growth model Lessons about the short-run economic growth (transition dynamics): When K < K ∗ , there is a short-run growth before the economy hits the steady state. The further away K is from K ∗ , the faster this growth will be. This is called "catch-up" growth. ECON 305 D100 Summer 2023, Lecture 2 33 Solow growth model Limitations of the Solow Model: Assumptions are too strict. e.g. People choose and change their saving rate all the time in the real world. It does not explain the long-run economic growth endogenously, → It all contributes to this mysterious A. ECON 305 D100 Summer 2023, Lecture 2 34 Readings Jones: Ch3, Ch4.1-4.3, Ch5 Andolfatto: Ch9.1, 9.7, Appendix 9.1 https://www.pitt.edu/ mgahagan/Solow.htm ECON 305 D100 Summer 2023, Lecture 2 35