Lothar and Martin were violent European windstorms which swept across western and central Europe during a period of 36 hours in December 1999. The storms caused major damage in France, southern Germany, Switzerland, and Italy. Throughout the affected region, 140 people were killed and damage was estimated at €9.9 billion. Both of these storms were associated with an intense jet stream aloft and benefitted from latent heat release through atmosphere-ocean exchange processes. Lothar and Martin together left 3.4 million customers in France without electricity, and forced EdF to acquire all the available portable power generators in Europe, with some even being brought in from Canada. These storms brought down a quarter of France's high-tension transmission lines and 300 high-voltage transmission pylons were toppled. It was one of the greatest energy disruptions ever experienced by a modern developed country.
Meteorological history
December 1999 saw a series of heavy winter storms cross the North Atlantic and western Europe. In early December, Great Britain and Denmark were hit by Cyclone Anatol which caused severe damage in Denmark. A second storm then crossed Europe on 12 December. A very deep and sizeable depression moved across Britain on the night of 24–25 December, this set up a large area of westerly flow into Europe which brought Lothar. This highly unstable situation inevitably meant low predictability, and saw an unusually straight and strong jet stream. Storm Martin then struck France and central Europe from 26 to 28 December 1999. At the end of January 2000 two additional damaging storms crossed Denmark and the northern part of Germany.
Forecast
Windstorm Lothar was not well predicted, with one meteorologist later claiming that forecasts could be split into those that were poor and those that were very poor. According to some forecasts, the storm was predicted to pass through the United Kingdom, while others failed to predict significant intensification at all. The strong jet stream that was the chief cause of the instability was well predicted by the European Centre for Medium-Range Weather Forecasts 9 days earlier. Approximately 24 hoursbefore the storm hit France, Météo-France issued a warning of a strong storm with the correct path, but two hours before the storm hit Paris, inland windspeeds were still predicted to be between 90–130 km/h, rather than the 125–175 km/h range actually experienced. MeteoSwiss found the storm Lothar extremely difficult to predict, as even the large forecast models of international weather services initially overlooked the small disturbance above the Atlantic Ocean which formed the storm. Consequently, the power and extent of the storm was only recognized in the early morning of 26 December, which resulted in shorter warning times in Switzerland. In a number of places, officials failed to realize the importance of the warnings, so they were not passed on to the public as they should have been. It is presumed that this occurred because of the holidays. The German Weather Service was criticised for not issuing a storm warning for Lothar in contrast to the weather services of other countries and private German services, apparently due to a software bug.
Lothar
During the first storm Lothar, wind speeds reached around in low-lying areas and more than on some mountains. In less than half a day the storm tore across France, Belgium and Germany, only finally beginning to weaken as it crossed Poland. The storm's compact internal pressure gradients generated winds which were comparable to those of a Category 2 hurricane. The Paris region was strongly affected by the storm during the early morning. The Palace of Versailles and its monumental park were considerably damaged. Other cultural heritage, forests and public gardens throughout the area were as severely affected by the hurricane-force winds. Public life was disrupted due to power outages and blocked infrastructure. Besides buildings and infrastructure, forests, such as the Black Forest in Germany, suffered major damage resulting in substantial economic loss.
Lothar successor
A case study of the Manual of Synoptic Satellite Meteorology featured by the Austrian Meteorological Institute identified an area of secondary cyclogenesis which brought gusts in excess of 90 km/h to Northern France, Belgium and Southwestern Germany. The system formed in the wake of Lothar, and crossed Europe before the arrival of the later storm Martin. The identification of this secondary area and its frontal systems contrasts with the analysis of the German Weather Service which suggested that solely a 'trough line' crossed Germany.
