North Atlantic warming hole impacts jet stream
The North Atlantic warming hole (NAWH), a region of reduced warming located in the North Atlantic Ocean, significantly affects the North Atlantic jet stream in climate simulations of the future, according to a team of researchers.
Sea surface temperatures (SST) are projected to increase in most of the world’s oceans as the result of global climate change. However, within an area of rotating ocean currents just south of Greenland an anomaly exists where colder sea-surface temperatures were documented in both global climate-model projections and in observations. It’s called a hole because there is a lack of ocean warming.
This region of the ocean is a really important place for forcing the jet stream that goes across the North Atlantic Ocean. Jet streams, high altitude currents of wind flowing above the Earth, transport air masses and drive weather patterns. The relationship between climate change and jet streams is complex and understanding the potential impact of climate change on jet streams is crucial for understanding changes in weather patterns and storm tracks.