Now that the Eurozone crisis is heating up again, I thought it worthwhile to revisit an earlier post of mine that discussed the key lessons I see from the Eurozone crisis:
(1) The optimal currency area (OCA) criteria should be taken seriously ex-ante. Before any country joins a currency union it should make sure it has met some combination of the OCA criteria. These criteria tells us that members of currency union should (1) share similar business cycles or (2) have in place some combination of economic shock absorbers including flexible wages and prices, factor mobility, fiscal transfers, and diversified economies. In the former case, similar business cycles among the regions mean that a common monetary policy, which targets the aggregate business cycle, will be stabilizing for all regions. In the latter case, dissimilar business cycles among the regions make a common monetary policy destabilizing—it will be either too stimulative or too tight—for regions unless they have in place some of the economic shock absorbers. In short, if a region's economy is not in sync with the currency union's business cycle and the above listed shock absorbers are absent then it does not makes sense for a country to be a part of the currency union. Instead, the country should keep its own currency which itself will act as a shock absorber. This understanding can be graphically represented as follows (click to enlarge):As shown in this recent post of mine and by others, several of the Eurozone countries fell inside the OCA boundary, Greece being one of them. This is not a surprise to most folks including the Euro optimists, but many hoped that these criteria would be met ex-post as the economies integrated. This leads to the second lesson.
(2) Don't hang your hope on becoming a successful currency union by meeting the OCA criteria ex-post. Some observers argued around the time of the Eurozone's inception that looking at the OCA criteria ex-ante was not warranted since the criteria themselves would emerge once a currency union was formed. This "endogenous" view of the OCA gave hope to the Euro optimists and lent support to their cause. Now there is evidence that joining a currency union does stimulate trade as transactions costs are lowered. One study found currency unions more than tripled trade among members. It is apparent now, though, that some of the Eurozone periphery did not integrate enough to justify the cost of being a member in the currency union. It is best not to base the survival of a currency union on hope.
As an aside, it is worth nothing that even if a region does endogenously meet the OCA criteria further problems can arise from being a part of the currency union. The increased trade flows and economic activity within the currency union can over time lead to regional specialization that makes the regions more susceptible to economic shocks. Paul Krugman first made this point in 1998 and the idea has become known as the "Krugman Specialization Hypothesis" (KSH). I think the best example of KSH is the United States. Despite being a currency union for many years, the United States did not become an OCA until the 1930s according to Hugh Rockoff. One reason is because there was so much regional specialization and until the New Deal reforms, many of the economic shock absorbers necessary to offset the lack of regional economic diversification were simply missing. So even if the Eurozone were a functioning OCA there is no guarantee it would stay that way.
(3) Take the real exchange rate seriously. A summary measure of a country's external competitiveness is its real exchange rate. If a country's real exchange rate is appreciating then its goods are becoming more expensive to the rest of the world. And, as a result, it will begin losing foreign earnings and the ability to meet external obligations. In a time of crisis for a country dependent on foreign funding this problem becomes more pronounced. As seen in the next figure, most of the Eurozone periphery has had a real appreciation on average since the inception of the Euro!
Now to understand why the periphery has had the real appreciation, one has to look at the three components of the real exchange rate: domestic prices, foreign prices, and the exchange rate. For Greece the problem was twofold. First, because of wage pressures domestic prices rose, more so than in the core Eurozone countries. Second, given its membership in the Eurozone, Greece had a fixed exchange rate and, thus, no chance for its currency to depreciate. To get out of this bind Greece can either have painful deflation or end its use of the Euro. Given where Greece is now, leaving the Euro may seem like lesser of two evils for Greek leaders. (Just to be clear, a depreciation will not solve Greece structural problems, but it make it easier to address them.) Any country joining a currency union should consider the implications of membership on its real exchange rate.
(4.) The central bank contributes most to macroeconomic stability by stabilizing aggregate demand (i.e. total current euro spending). I have made this point before for the United States, but it applies just as well to the Eurozone. And based on the following figure, the European Central Bank (ECB) has not done a very good stabilizing total current euro spending during this crisis:
As Nick Rowe notes, the sharp decline in the Eurozone's aggregate demand was avoidable had the ECB really tried to stabilize it. Instead, the ECB mistakenly looked to low short-term interest rates as an indicator of loose monetary policy and became convinced it was doing enough. A better indicator of the stance of monetary policy I have discussed before is to look at the growth rate of aggregate demand relative to the policy interest rate. Using this metric, the ECB policy rate should not deviate too far from the aggregate demand growth rate otherwise monetary policy is either too loose (the policy rate is significantly below the total spending growth rate) or too tight (the policy rate is significantly above the total spending growth rate). This next figure shows this measure for the Eurozone:
I am reminded of Hume's argument about gold flows.ReplyDelete
If there is an excess demand for money in locality A, and monetary equilibrium in locality B, then money will flow from B to A. Unless the excess demand for money is offset with an increased supply of money, the general level of prices will fall across both localities. However, if there is an offsetting increase in the supply of money, then money will still flow toward locality B but without a change in the general level of prices.
Why does this process seem to work for the U.S. but not the eurozone? Is it just that euros do not flow so easily among localities?
Surely the European Central Bank needs only one monetary policy for the eurozone, just as the Federal Reserve has one policy for the United States, and the market will allocate money wherever sellers get the best prices -- towards localities with an excess demand for money?
I suppose I do not understand why sticky prices are much of an issue. Supposing locality A has downwardly stickier prices than B, so what? That just means that a greater increase in the money supply will be necessary that otherwise, because prices will not fall much.
Do you know how up-to-date chart 3 is? I think Ireland is more competitive than that now.ReplyDelete