Extreme Heat and Snow: How Weather Extremes Reshape the Land
Heat waves and blizzards sit at opposite ends of the temperature spectrum, but both are driven by similar underlying atmospheric mechanics: large air masses becoming trapped or reinforced over a region for an extended period.
What Causes a Heat Wave
Extreme heat events are often driven by a phenomenon called a heat dome, a large area of high pressure that traps warm air beneath it like a lid, preventing cooler air or storms from moving through. As this trapped air compresses and sinks, it warms further, and reduced cloud cover lets more direct sunlight reach the ground, compounding the heat.
Why Heat Waves Are Becoming a Bigger Concern
Urban areas experience an amplified version of heat waves known as the urban heat island effect, where pavement, buildings, and reduced vegetation cause cities to retain significantly more heat than surrounding rural areas, especially overnight.
How Major Snowstorms and Blizzards Form
Lake-Effect Snow
Regions near large lakes can experience lake-effect snow, where cold air moving across relatively warmer lake water picks up moisture and heat, then dumps that moisture as heavy, localized snowfall once it reaches the colder land on the other side.
Why Both Extremes Matter for the Land
Extreme heat dries and stresses soil and vegetation, sometimes contributing to drought conditions that persist well after the heat wave ends. Heavy snowpack, meanwhile, plays an important role in seasonal water supply, since gradual snowmelt in spring recharges rivers, soil moisture, and groundwater.
Continue with How Weather Shapes the Soil Beneath Us, or read Understanding Hurricanes.