부산대학교 도서관

Pollen evidence suggests that the paleoclimate of the Mediterranean during the Last Glacial Maximum was semi-arid while geomorphological data suggest high lake levels. Using a water-balance model to predict runoff catchment and a biome model to predict vegetation, type the paleoenvironment of Lake Ioannina may be reconstructed. The reconstruction features wet winters and dry summers. Several atmospheric models have the jet stream shifted to the south and the summer drying effects of the cold North Atlantic may have been seasonally reversed by increased storm frequency.