Exploring the science of lake effect snow
KANSAS CITY, Mo. (KCTV) - Lake effect snow develops when frigid Arctic air masses sweep across the unfrozen expanse of a large lake. This setup occurs most often during late fall and early winter.Exploring the science of lake effect snow.(KCTV5)As this cold, dry air races over the warmer water, it eagerly siphons heat and moisture from the lake’s surface. This injection of warmth and humidity causes the lowest layer of air to become significantly warmer and less dense than the air above it, prompting it to rise in buoyant plumes or bubbles—a process known as convection. Exploring the science of lake effect snow.(KCTV5)As these warm, moist air parcels ascend, they encounter cooler temperatures. This cooling causes the water vapor to condense, forming clouds, and as the air continues to cool...










