An atmospheric river is a narrow corridor in the atmosphere that transports large amounts of water vapor from the tropics to other regions. These weather phenomena can result in heavy rainfall and can extend over thousands of kilometers. Atmospheric rivers are crucial for replenishing water resources and can contribute significantly to precipitation events, particularly in coastal and mountainous regions.Why and How it Happens
Atmospheric rivers occur when there is a strong and persistent flow of moisture-laden air from the tropics toward higher latitudes. This flow is driven by the temperature and pressure differences between different regions of the atmosphere. Atmospheric rivers typically form in association with large-scale weather patterns, such as low-pressure systems or the jet stream, and can result in prolonged periods of heavy rainfall or snowfall when they make landfall.