Pangea was immense and possessed a great degree of climatic variability, with its interior exhibiting cooler and more arid conditions than its edge. Some paleoclimatologists report evidence of short rainy seasons in Pangea’s dry interior. Climatic patterns of the entire globe were affected by the presence of Pangea as well, since it stretched from far northern latitudes to far southern latitudes. The equatorial waters of Panthalassa—the superocean that surrounded Pangea—were largely isolated from cold ocean currents because the Paleo Tethys and Tethys seas, which together formed an immense warm water sea surrounded by various parts of Pangea, also affected the supercontinent’s climate, bringing humid tropical air and rain downwind. Pangea’s breakup might have also contributed to an increase in temperatures at the poles, as colder waters mixed with warmer waters.