Europe's nations and regions

Harald Benink, Harry Huizinga, 16 May 2015

QE in the Eurozone is unusual in that the risks of sovereign debt defaults are shared between the ECB and the national central banks. This column argues that if such risk sharing were applied to the Outright Monetary Transactions programme, it could potentially create insolvency problems for countries with large public debts, especially in a low-growth scenario.

Jan Hanousek, Anna Kochanova, 04 May 2015

The evidence about the effect of bribery on economic growth is mixed. Some find it harmful while others believe it helps via a ‘grease the wheels’ effect. This column argues that the ambiguity can be explained by divergent effects of the mean and dispersion of corruption. A high bribery-mean retards productivity growth of firms, but a high bribery-dispersion facilitates performance of weak firms.

Marco Buti, Alessandro Turrini, 17 April 2015

An oft expressed view is that the Eurozone is a straitjacket on periphery members and income convergence has slowed, halted or reversed.  This column argues that EZ convergence never stopped. What changed was the type of convergence. Today’s convergence is neither nominal nor real, it is structural.  Structural convergence presents a basis for renewed real convergence. However, for this to happen, the right institutions and policies need to be in place at both European and national levels.

Carlos Cantú, KeyYong Park, Aaron Tornell, 12 April 2015

The wisdom of structural reform during a crisis is a subject of heated debate. This column compares Greece’s experience to that of Mexico during the debt crisis of the 1980s. Mexico did not receive a haircut until seven years into the crisis – after structural reform was already underway. In Mexico that reform was the outcome of an internal conversation – not a diktat from the outside – and it happened during the height of the crisis.

Morgan Kelly, Cormac Ó Gráda, 28 March 2015

The Little Ice Age is generally seen as a major event in European history. Analysing a variety of recent weather reconstructions, this column finds that European weather appears constant from the Middle Ages until 1900, and that events like the freezing of the Thames and the disappearance of English vineyards have simpler explanations than changing climate. It appears instead that the European Little Ice Age is a statistical artefact, where the standard climatological practice of smoothing what turn out to be white noise data prior to analysis gives the spurious appearance of irregular oscillation – a Slutsky Effect.

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