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Titlebook: Markov-Switching Vector Autoregressions; Modelling, Statistic Hans-Martin Krolzig Book 1997 Springer-Verlag Berlin Heidelberg 1997 business

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Markov-Switching Models of the German Business Cycle,ested in the chronology of contraction and expansion epochs (cf. .. [1994]). This view is expressed in the primary descriptive definition of the ‘business cycle’ proposed by . [1946, p. 3] which is however compatible with most business cycle theories (cf. . [1995]):
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Cointegration Analysis of VAR Models with Markovian Shifts in Regime,erence with the foregoing analysis, as well as the previous literature, is the application of the MS-VAR model and the associated statistical procedures to . time series. Whereas the relevance of shifts in regimes of cointegrated time series has recently found a growing audience, the current state-o
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Epilogue,lated to the MS-VAR model but which have not been discussed in this presentation. If this study may have intended to develop an operational econometric approach for the statistical analysis of economic time series with MS-VAR models, then we can conclude that some progress has been made. Concerning
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. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 16 Geological change — the answers within, and without. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 18 Man on the Moon. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .
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Hans-Martin Krolzig To the contrary, determinations of these elements in meteorites yielded a Li/B ratio of about 5 [1]. Exposure to high neutron fluxes has been proposed to change the elemental and isotopic ratios of Li and B via the reaction .B(n, .).Li [2]. Recent measurements of the spallation cross-sections of Li
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Hans-Martin Krolzigctober 18-20, 1965, under the chairmanship of Professor J. Orce!‘ In addition to the Chairman the fol­ lowing were present: Dr. G. Harbottle, Dr. M. H. Hey, Dr. B. H. Mason, Dr. P. M. Millman, Professor K. I. Sztr6kay. Dr. E. M. Fournier d‘Albe represented the UNESCO Secretariat. Recommendation No.4
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