ArticleslgStudy

earth science

Meiyu front

Meiyu front is a earth science 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 Meiyu front rather than just read about it. In short: The meiyu front, also known as baiu front, is a persistent nearly stationary weak baroclinic zone in the lower troposphere. It is located over the east coast of China and Taiwan at its western end, and over the Pacific Ocean south of Japan at its eastern end.

Meiyu front — main illustration
Meiyu front — illustration

Key takeaways

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

Reference excerpt

The meiyu front, also known as baiu front, is a persistent nearly stationary weak baroclinic zone in the lower troposphere. It is located over the east coast of China and Taiwan at its western end, and over the Pacific Ocean south of Japan at its eastern end. The term meiyu (mei-yu) is Chinese for "plum rains", pronounced baiu (bai-u) in Japanese (Chinese and Japanese: 梅雨).

Description The meiyu front stretches from the Tibetan Plateau to Japan along a confluent jet stream that separates Arctic circulation to the north from tropical circulation to the south. During mid-spring to mid-summer, the upper circulation is typically west–east and the front is mostly stationary. Along this boundary, mesoscale convective complexes (MCCs) or mesoscale convective systems (MCSs) tend to form and propagate eastward, giving a series of heavy downpours. The system extracts moisture from the South China Sea and sometimes the Bay of Bengal. The low-level warm air is lifted by the low level jet on the equator side of the baroclinic zone. The deep vertical motion giving birth to organized MCCs/MCSs is especially strong when the low-level warm air enters the area situated beneath the jet entrance region aloft. Rainfall along this boundary tends to be particularly heavy in post-El Niño summers, such as the summer of 2016.

See also East Asian rainy season

References

Illustrations

Meiyu front: Clouds associated with the meiyu during the 2016 Jiangsu tornado
Clouds associated with the meiyu during the 2016 Jiangsu tornado

Worked examples

Example 1 — a first encounter with Meiyu front

Start with the simplest possible case. Write down what Meiyu front claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, 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 Meiyu front 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 Meiyu front 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 Meiyu front

In research
Meiyu front appears in earth science 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 Meiyu front 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
Meiyu front is common in secondary-school and first-year university syllabi. It links to neighbouring topics Meteorological phenomena, Meteorology stubs, Severe weather and convection, so understanding it makes those chapters shorter.
In everyday life
Look for Meiyu front 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 Meiyu front in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Meiyu front 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 Meiyu front out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Meiyu front in simple terms?

The meiyu front, also known as baiu front, is a persistent nearly stationary weak baroclinic zone in the lower troposphere. It is located over the east coast of China and Taiwan at its western end, and over the Pacific Ocean south of Japan at its eastern end.

Why does Meiyu front matter?

Because it connects several earth science 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 Meiyu front?

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 Meiyu front.

Tags

  • Meteorological phenomena
  • Meteorology stubs
  • Severe weather and convection
  • Synoptic meteorology and weather
  • Weather fronts

Keep exploring