What Causes a Heatwave? — Reading Comprehension

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This engaging educational resource, 'What Causes a Heatwave?', offers an insightful reading passage designed for Grade 6 students. It delves into the scientific principles behind heatwaves, focusing on concepts like air masses, high-pressure systems, and atmospheric conditions that lead to extreme heat events. The passage defines key terms, making complex ideas accessible, and is complemented by a variety of activities including multiple-choice questions, a glossary, and short answer questions. These activities reinforce understanding of weather changes and how air masses interact, aligning directly with NGSS standard MS-ESS2-5. The content is audio integrated to support diverse learning styles and enhance comprehension of weather phenomena and climate science.

CONTENT PREVIEW

Students view how heatwaves form under a high-pressure dome trapping warm air. — Diagram of heatwave formation from high pressure and sinking warm air.

The air around us is always on the move, carrying different temperatures and moisture levels. Sometimes, this movement stops or slows down in just the right way to create extremely hot conditions. This is what we call a heatwave – a period of unusually hot weather that lasts for several days.

One of the main causes of a heatwave is a high-pressure system. Imagine a large dome of air pushing down on the Earth's surface. This dome prevents air from rising. When air sinks, it warms up. This warming effect, combined with clear skies that allow more sunlight to reach the ground, traps heat close to the surface. It's like putting a lid on a pot, keeping the heat inside.

Normally, weather systems move across the globe, bringing changes in temperature, wind, and precipitation. However, during a heatwave, these high-pressure systems can become 'stuck' or stagnant over a region. This means the hot air stays put, building up heat day after day. This is often linked to the behavior of the jet stream, a fast-moving current of air high in the atmosphere. The jet stream usually guides weather systems. If it takes a large loop or becomes weaker, it can allow high-pressure systems to linger.

Another factor is the type of air mass involved. An air mass is a large body of air that has similar temperature and humidity throughout. For a heatwave, we typically see a large, warm, and dry air mass move into a region. This air mass might originate from a desert area or simply heat up as it sits over land under the high-pressure dome.

The interaction of these factors – a strong, stagnant high-pressure system, a specific air mass, and the influence of the jet stream – creates the perfect recipe for a heatwave. Understanding these complex interactions helps meteorologists predict when and where a heatwave might occur, giving people time to prepare for the extreme summer heat and ensure public safety. These events are crucial for understanding global climate patterns and their effects on local weather conditions.

Interesting Fact: The deadliest heatwave in U.S. history occurred in 1980, causing an estimated 1,700 deaths across the central and eastern United States.

What is a heatwave?

Period of hot weatherHeavy rainfallStrong windsCold temperatures

What prevents air from rising during a heatwave?

Low-pressure systemHigh-pressure systemStrong windsJet stream

How does a high-pressure system warm the air?

It pulls air upIt adds moistureIt causes air to sinkIt creates clouds

What happens if a high-pressure system becomes 'stuck'?

Causes cold weatherPrevents heat build-upHot air stays putIncreases rainfall

What is the jet stream's role in weather systems?

Makes air colderCreates high pressureGuides weather systemsCauses thunderstorms

What kind of air mass is typically involved in a heatwave?

Cold and wetWarm and dryCool and moistFast-moving