ArticleslgStudy

engineering

Thermal

Thermal is a engineering topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Thermal rather than just read about it. In short: A thermal column (or thermal) is a rising mass of buoyant air, a convective current in the atmosphere, that transfers heat energy vertically. Thermals are created by the uneven heating of Earth's surface from solar radiation, and are an example of convection, specifically atmospheric convection.

Thermal — main illustration
Thermal — illustration

Key takeaways

  • Thermal belongs to engineering; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Thermal to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Thermal from memory before moving on to harder problems.

Reference excerpt

A thermal column (or thermal) is a rising mass of buoyant air, a convective current in the atmosphere, that transfers heat energy vertically. Thermals are created by the uneven heating of Earth's surface from solar radiation, and are an example of convection, specifically atmospheric convection.

Thermals on Earth The Sun warms the ground, which in turn warms the air directly above. The warm air near the surface expands, becoming less dense than the surrounding air. The lighter air rises and cools due to its expansion in the lower pressure at higher altitudes. It stops rising when it has cooled to the same temperature, thus density, as the surrounding air. Associated with a thermal is a downward flow surrounding the thermal column. The downward-moving exterior is caused by colder air being displaced at the top of the thermal. The size and strength of thermals are influenced by the properties of the lower atmosphere (the troposphere). When the air is cold, bubbles of warm air are formed by the ground heating the air above it and can rise like a hot air balloon. The air is then referred to as unstable, as it's suitable for forming thermals. If there is a warm layer of air higher up, an inversion can prevent thermals from rising high and the air is said to be stable, as mature thermals can't form. Thermals are often indicated by the presence of visible isolated cumulus clouds at the top of the thermal. Cumulus clouds are formed by the rising air in a thermal as it ascends and cools, until the water vapor in the air begins to condense into visible droplets. When a steady wind is present, thermals and their respective cumulus clouds can align in rows oriented with wind direction, sometimes referred to as "cloud streets" by soaring and glider pilots. The condensing water releases latent heat energy allowing the air to rise higher. Very unstable air can reach the level of free convection (LFC), rising to great heights, condensing large quantities of water and forming convective clouds causing showers or even thunderstorms. The latter are dangerous to any aircraft flying through or nearby. Thermals are one of the many sources of lift used by soaring birds and gliders to soar.

Thermals beyond Earth Thermals are also seen elsewhere in the Solar System. On Mars, for example, thermals are often seen in the form of dust devils, carrying dust instead of water vapor. Thermals are also seen on the Sun, typically forming hexagonal convective prisms (Bénard cells).

See also Air current Atmospheric thermodynamics Cumulus cloud Gliding Hang gliding Thermal energy

References

External links What do thermals look like? - Thermal Structure and Behavior by Wayne M. Angevine Time-lapse video of clouds caused by thermals forming and decaying

Illustrations

Thermal: Example of a thermal column between the ground and a cumulus
Example of a thermal column between the ground and a cumulus
Thermal illustration
Thermal illustration
Thermal: Thermal cross section with stronger lift (rising air) in darker shades of green, while red is sink (descending air).
Thermal cross section with stronger lift (rising air) in darker shades of green, while red is sink (descending air).

Worked examples

Example 1 — a first encounter with Thermal

Start with the simplest possible case. Write down what Thermal claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In engineering, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Thermal before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Thermal ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Thermal

In research
Thermal appears in engineering research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Thermal in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Thermal is common in secondary-school and first-year university syllabi. It links to neighbouring topics Atmospheric thermodynamics, Aviation meteorology, Gliding technology, so understanding it makes those chapters shorter.
In everyday life
Look for Thermal outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.

Affiliate

Preply — study more efficiently by working with a personal tutor. 50% off.

How to study Thermal in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Thermal means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Thermal out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Thermal in simple terms?

A thermal column (or thermal) is a rising mass of buoyant air, a convective current in the atmosphere, that transfers heat energy vertically. Thermals are created by the uneven heating of Earth's surface from solar radiation, and are an example of convection, specifically atmospheric convection.

Why does Thermal matter?

Because it connects several engineering ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Thermal?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Thermal.

Tags

  • Atmospheric thermodynamics
  • Aviation meteorology
  • Gliding technology
  • Severe weather and convection

Keep exploring