Gibraltar Dam Unnecessary
The salty outflow from the Mediterranean, caused by the high evaporation rates there, is a prominent feature of the present ocean circulation. It creates a tongue of exceptionally salty water stretching westward across the Atlantic at around 1,000 m below the surface. Rahmstorf used a global ocean circulation model to investigate the effects of this salty water on the Atlantic currents and surface climate. His computer simulations show that the present outflow from the Mediterranean enhances the Gulf Stream, heating the surface temperatures in the northern North Atlantic by a few tenths of a degree.
However, the change in the salty outflow that could arise from the diversion of fresh water by the Aswan dam is very small. Rahmstorf's simulations showed that this change is too small to have a noticeable effect on the surface climate in the Atlantic. "There's no way you could trigger an Ice Age in this way", he said. "Building a dam across the Strait of Gibraltar to prevent climatic change would be a complete waste of time, quite apart from the negative side-effects that such a massive project would undoubtedly have".
Rahmstorf stressed that there is serious reason for concern that global warming could disrupt Atlantic ocean currents. But this would be caused by temperature and rainfall changes over the Atlantic, and has nothing to do with the Mediterranean outflow.
The full article ("Influence of Mediterranean Outflow on Climate") with illustrations is available at https://www.pik-potsdam.de/~stefan
For further information, contact Dr. Stefan Rahmstorf, +49-331-2882688 (office) or 331-715429 (home), email mailto:Stefan.Rahmstorf@pik-potsdam.de