ArticleslgStudy

earth science

Icelandic Low

Icelandic Low 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 Icelandic Low rather than just read about it. In short: The Icelandic Low is a semi-permanent centre of low atmospheric pressure found between Iceland and southern Greenland and extending in the Northern Hemisphere winter into the Barents Sea. In the summer, it weakens and splits into two centres, one near Davis Strait, Labrador, and the other west of Iceland.

Icelandic Low — main illustration
Icelandic Low — illustration

Key takeaways

  • Icelandic Low 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 Icelandic Low to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Icelandic Low from memory before moving on to harder problems.

Reference excerpt

The Icelandic Low is a semi-permanent centre of low atmospheric pressure found between Iceland and southern Greenland and extending in the Northern Hemisphere winter into the Barents Sea. In the summer, it weakens and splits into two centres, one near Davis Strait, Labrador, and the other west of Iceland. It is a principal centre of action in the atmosphere circulation of the Northern Hemisphere, associated with frequent cyclone activity. It forms one pole of the North Atlantic oscillation, the other being the Azores High.

See also Kona low Aleutian low

References National Snow and Ice Data Center, retrieved 19 May 2005.

Illustrations

Icelandic Low: An Icelandic cyclone on September 4, 2003
An Icelandic cyclone on September 4, 2003

Worked examples

Example 1 — a first encounter with Icelandic Low

Start with the simplest possible case. Write down what Icelandic Low 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 Icelandic Low 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 Icelandic Low 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 Icelandic Low

In research
Icelandic Low 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 Icelandic Low 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
Icelandic Low is common in secondary-school and first-year university syllabi. It links to neighbouring topics Atlantic Ocean, Barents Sea, Climate of Canada, so understanding it makes those chapters shorter.
In everyday life
Look for Icelandic Low 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.
Ask Teacher Smith questions about this articleOpens your AI tutor with a question about “Icelandic Low” →

Affiliate

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

How to study Icelandic Low in 20 minutes

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

Frequently asked questions

What is Icelandic Low in simple terms?

The Icelandic Low is a semi-permanent centre of low atmospheric pressure found between Iceland and southern Greenland and extending in the Northern Hemisphere winter into the Barents Sea. In the summer, it weakens and splits into two centres, one near Davis Strait, Labrador, and the other west of I…

Why does Icelandic Low 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 Icelandic Low?

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 Icelandic Low.

Tags

  • Atlantic Ocean
  • Barents Sea
  • Climate of Canada
  • Climate of Iceland
  • Climatology stubs
  • Geography of Greenland
  • Regional climate effects
  • Types of cyclone

Keep exploring