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Dynamic persistence in the unemployment rate of OECD countries

机译:经合组织国家失业率的动态持久性

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Previous studies use a variety of increasingly advanced unit root tests to determine whether Blanchard and Summers (1986) hysteresis theory of unemployment or the classical 'natural' rate theory of Friedman (1968) and Phelps (1967,1968) is most relevant for a given country. However these tests all specify a unit root under the null hypothesis against a stationary alternative, such as in the paper by Lee and Chang (2008), making the two theories of unemployment mutually exclusive over the sample period. This paper moves away from this dichotomy by allowing for switches between hysteresis and the natural rate theory using the recently developed test of Leybourne, Kim and Taylor (2007). We find that in countries like the United Kingdom, the natural rate theory is detected in the post-World War Two period of stabilisation: the time leading up to the seminal works of Friedman and Phelps. Hysteresis is found over the First World War and Great Depression periods, and in the period from the 1970s; a time characterised by rising trade union power. We also compute numerical measures of persistence using grid-bootstrap estimates of the autoregressive parameter, following Hansen (1999).
机译:先前的研究使用各种越来越先进的单位根检验来确定Blanchard和Summers(1986)的滞后磁滞理论或Friedman(1968)和Phelps(1967,1968)的经典“自然”利率理论是否与给定最相关。国家。然而,这些测试都在零假设下针对固定的替代条件指定了单位根,例如Lee和Chang(2008)的论文,使得两个失业理论在样本期内是互斥的。本文通过使用最近开发的Leybourne,Kim和Taylor(2007)的检验允许在磁滞和自然速率理论之间进行切换,从而摆脱了这种二分法。我们发现,在英国等国家/地区,自然费率理论是在第二次世界大战后的稳定时期发现的:即弗里德曼和菲尔普斯的开创性工作。在第一次世界大战和大萧条时期以及1970年代开始发现磁滞现象。以工会力量不断增强为特征的时期。根据Hansen(1999),我们还使用自回归参数的网格引导估计来计算持久性的数值度量。

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