Elasticity “eta” Lectures in Microeconomics-Charles W. Upton Four demand functions P P D D Q P Q P D D Q Elasticity Q Four demand functions P P D D Q P Q P D D Q Elasticity Q Four demand functions P P D D Q P Q P D D Q Elasticity Q Four demand functions P P D D Q P Q P D D Q Elasticity Q The notion of elasticity • The critical question: how responsive is the quantity demanded to changes in price? Elasticity The notion of elasticity • The critical question: how responsive is the quantity demanded to changes in price? • And how do we measure that? Elasticity A Definition, Sort of • We represent that by the price elasticity of demand the ratio of the percentage change in quantity demanded to the percent change in price Elasticity An Illustration P 50 100 Q Elasticity Q = 100 – 2P P Q = 100 – 2(20) = 60 50 Q = 100 – 2(18) =64 20 18 60 64 Q 100 Elasticity New v. Old P = 100 2(20) = 60 But which isQthe new– price and which is the old price? And does it make a Q = 100 – 2(18) =64 difference? 50 20 18 60 64 Q 100 Elasticity New v. Old P 50 20 18 = 100 2(20) = 60 But which isQthe new– price and which is the old price? And does it make a Q =calculation 100 – 2(18) =64 Yes. Lets do the difference? assuming the price goes from 20 to 18 and then from 60 64 100 18 to 20? Q Elasticity Going from 20 to 18 P PercentChangeinQuant ity PercentChangein Pr ice 50 New Pr ice Old Pr ice 18 20 2 10% Old Pr ice 20 20 20 18 60 64 Q 100 Elasticity Going from 20 to 18 P PercentChangeinQuant ity PercentChangein Pr ice 50 20 18 New Pr ice Old Pr ice 18 20 2 10% Old Pr ice 20 20 NewQuantity OldQuantit y 64 60 4 6.7% OldQuantit y 60 60 60 64 Q 100 Elasticity Going from 20 to 18 P 6.7% 0.67 10% 50 20 18 New Pr ice Old Pr ice 18 20 2 10% Old Pr ice 20 20 NewQuantity OldQuantit y 64 60 4 6.7% OldQuantit y 60 60 60 64 Q 100 Elasticity Going from 18 to 20 P PercentChangeinQuant ity PercentChangein Pr ice 50 20 18 60 64 Q 100 Elasticity Going from 18 to 20 P PercentChangeinQuant ity PercentChangein Pr ice New Pr ice Old Pr ice 20 18 2 11.1% Old Pr ice 18 18 50 20 18 60 64 Q 100 Elasticity Going from 18 to 20 P PercentChangeinQuant ity PercentChangein Pr ice New Pr ice Old Pr ice 20 18 2 11.1% Old Pr ice 18 18 50 20 18 NewQuantity OldQuantit y OldQuantit y 60 64 Q 100 Elasticity 60 64 4 6.25% 64 64 Going from 18 to 20 P 6.25% 0.563 11.1% New Pr ice Old Pr ice 20 18 2 11.1% Old Pr ice 18 18 50 20 18 NewQuantity OldQuantit y OldQuantit y 60 64 Q 100 Elasticity 60 64 4 6.25% 64 64 So what is it? 6.7% 6.25% 0.563 0.67 11.1% 10% Elasticity Two computational methods • Point Elasticity of Demand • Arc Elasticity of Demand Elasticity Point Elasticity of Demand • Defined by Pr ice Slope Quantity where Slope is the slope of the demand function Elasticity Point Elasticity of Demand • Defined by In the case of a linear Pr ice demand function Slope Q = aQuantity – bP where Slope is the slope of the demand The slope is -b function Elasticity P Computing the Point Elasticity Pr ice Slope Quantity 50 20 18 60 64 Q 100 Elasticity P Computing the Point Elasticity Pr ice Slope Quantity Slope 2 50 20 18 60 64 Q 100 Elasticity Computing at Q = 60 P Pr ice Slope Quantity Slope 2 50 20 18 20 (2) 0.67 60 60 64 Q 100 Elasticity Computing at Q = 64 P Pr ice Slope Quantity Slope 2 50 20 18 18 (2) 0.5625 64 60 64 Q 100 Elasticity A Problem P Pr ice Slope Quantity Slope 2 50 20 18 Compute the point price elasticity of demand at P = 25 and P = 35 60 64 100 Q Elasticity A Problem P Pr ice Slope Quantity Slope 2 50 20 18 Compute the point price elasticity of demand at When P = 25 and P =P35= 25, = -1 60 64 100 When P = 35, = -2.333 Q Elasticity P along the Demand Function Pr ice Slope Quantity 100 Q • For a straight line demand curve will vary over the demand curve Elasticity P along the Demand Function Pr ice = - Slope Quantity • When the curve hits the price axis, = - 100 Q Elasticity P along the Demand Function Pr ice = 0 Slope Quantity • When the curve hits the quantity axis, = 0 100 Q Elasticity P along the Demand Function Pr ice = -1 Slope Quantity • At the midpoint, = -1 100 Q Elasticity Next Lecture • Arc Elasticity • Extensions Elasticity End ©2004 Charles W. Upton Elasticity