3,056 research outputs found

    "Macroeconomic Market Incentive Plans: History and Theoretical Rationale"

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    This paper explores the contemporary debate among economists on the means to move the economy toward high employment without inflation-beyond the traditional instruments of monetary and fiscal policy. The authors pay particular attention to the Market Anti-Inflation Plan (MAP), submitted by Lerner and Colander in 1980. The reasons economists have searched for alternative measures relate to the problems associated with wage and price controls. MAP is an anti-inflation plan that allows relative prices to adjust: The scheme increases costs to firms that raise prices, and contains an added incentive to lower prices. Since MAP is designed to fight macroeconomic inflation by changing the incentives of individual price setters, the relationship between microeconomic behavior and macroeconomic outcomes must be addressed. The theoretical justification for MAP is that there is a macroeconomic externality, and MAP can mitigate the ramifications of the externality. However, efforts to more clearly define the nature of this externality require a better understanding of transaction costs. Consequently, there will be the need for a mechanism to integrate such costs into microeconomic and macroeconomic models.

    The Natural Rate in a Share Economy

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    Will the natural rate 0f unemployment be lower in the share economy described by Martin Weitzman than in a wage economy? We examine this question for a search economy with an equilibrium unemployment rate, a version 0f Salop's (1979) quits model. Equilibrium unemployment is the same in both economies. We also examine firms' short-run adjustment to shocks. Share-economy firms adjust output less than wage-economy firms for both demand shocks and labor-supply shocks. Depending on whether rapid output adjustment is stabilizing, a share economy may be more or less stable than a wage economy

    Application of Market Anti-inflation Plans in the Transition to a Market Economy

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    How can the former socialist countries' transition to a market economy be made less painful and more effective? We propose the use of incentive policies to stabilize prices and output. This would reduce former planned economies' tendency for output to fall and prices to rise as firms and workers take advantage of their market power. The policy allows firms individual pricing freedom while giving assurance that the price level will be stable. It also can break the vicious circle of reduced aggregate output by setting fixed level of output.Socialists

    The Natural Rate in a Share Economy

    Get PDF
    Will the natural rate 0f unemployment be lower in the share economy described by Martin Weitzman than in a wage economy? We examine this question for a search economy with an equilibrium unemployment rate, a version 0f Salop's (1979) quits model. Equilibrium unemployment is the same in both economies. We also examine firms' short-run adjustment to shocks. Share-economy firms adjust output less than wage-economy firms for both demand shocks and labor-supply shocks. Depending on whether rapid output adjustment is stabilizing, a share economy may be more or less stable than a wage economy

    Intracrystalline site preference of oxygen isotopes in goethite: A single-mineral paleothermometer

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    The crystal structure of goethite, FeO(OH), has two distinct oxygen sites, one with exclusively Fe-O bonds, the other with bonds to both iron and hydrogen. We developed a method to assess the oxygen isotope contrast between these sites by measuring both the bulk goethite and the oxygen released in the conversion of goethite to hematite. The method involves collecting the water released by dehydroxylation, fluorinating that population of extracted atoms, and measuring the resulting oxygen isotope composition (extracted δO¹⁸). Then, on a separate aliquot, all structural oxygen is fluorinated and measured (bulk δO¹⁸). Using synthetic goethite precipitates grown under controlled environmental conditions, we found significant temperature-dependent fractionation, ε_(bulk-extracted)=(5.51±0.26)×(10⁶/T²)−(44.5±2.8); T in Kelvin). This intracrystalline fractionation forms the basis of a single-phase paleothermometer with an estimated uncertainty of ∼2-3°C. The temperature dependence appears to be independent of the isotopic composition of the parent fluid from which the goethite formed and the pH of that fluid. This intracrystalline thermometer can be used to simultaneously determine the formation temperature of a goethite and the isotopic composition of the water from which it formed. Natural goethites analyzed with this technique yield geologically reasonable formation temperatures of between 15 and 41°C
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