Dynamic sea level changes following changes in the thermohaline circulation

Using the coupled climate model CLIMBER-3α, we investigate changes in sea surface elevation due to a weakening of the thermohaline circulation (THC). In addition to a global sea level rise due to a warming of the deep sea, this leads to a regional dynamic sea level change which follows quasi-instantaneously any change in the ocean circulation. We show that the magnitude of this dynamic effect can locally reach up to ~1m, depending on the initial THC strength. In some regions the rate of change can be up to 20-25 mm/yr. The emerging patterns are discussed with respect to the oceanic circulation changes. Most prominent is a south-north gradient reflecting the changes in geostrophic surface currents. Our results suggest that an analysis of observed sea level change patterns could be useful for monitoring the THC strength.

Trade, Politics, and Democratization: The 1997 Global Agreement between the European Union and Mexico

Mexico and the European Union signed a new Political and Economic Association Agreement in December 1997 and ultimately a free-trade agreement in March 2000, aiming to establish a new model of relations with a more dynamic trade and investment component. This article analyzes the 1997 agreement as background to the final accord. Economic and political changes in the 1990s modified both parties' participation in the international political economy, helping to overcome some of the structural obstacles to the relationship. The policy toward Latin America adopted by the EU in 1994 was influential. The negotiation process revealed divergences over the scope of the liberalization process and the so-called democracy clause.