Read here. (h/t Greenie Watch) The Mediterranean Sea basin is considered one ot the more vulnerable to climate change, which is a major concern since the IPCC climate models predict that global warming will result in more frequent storm activity. To test this prediction, EU researchers analyzed 7,000 years of data from sediment cores from southern France's coastal region.
Sabatier et al. analysis establishes the history of severe storm activity, which firmly indicates that severe stroms were more frequent during global cooling (ie. The Little Ice Age) than during global warming spans, such as the Medieval Warming Period.
As is often the case, the empirical evidence refutes the IPCC climate model predictions.
"This paper present a high resolution record of paleostorm events in the French Mediterrannean coast over the past 7000 years based on a long sediment core from lagoonal environment in Gulf of Lions...we have recorded seven periods of increase in storm activity at 6200, 5400, 4600-4200, 3600-3100, 2600, 1900-1500 yr cal B.P. and over the Little Ice Age...Whereas the Medieval Warm Period (1200-700 yr cal B.P.) is characterized by a low storm activity. These evidences of changes in coastal hydrodynamic are in phase with those observed over the North Atlantic and correspond to Holocene cooling evidenced associated to decreases of SST in the North Atlantic." [Pierre Sabatier, Laurent Dezileau, Christophe Colin, Louis Briqueu, Philippe Martinez, Giuseppe Siani, Frédérique Bouchette, Olivier Raynal, Ulrich Von Grafenstein 2011: International Union for Quaternary Research]