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Goode homolosine projection

Goode homolosine projection is a 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 Goode homolosine projection rather than just read about it. In short: The Goode homolosine projection (or interrupted Goode homolosine projection) is a pseudocylindrical, equal-area, composite map projection used for world maps. Normally it is presented with multiple interruptions, most commonly of the major oceans.

Goode homolosine projection — main illustration
Goode homolosine projection — illustration

Key takeaways

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

Reference excerpt

The Goode homolosine projection (or interrupted Goode homolosine projection) is a pseudocylindrical, equal-area, composite map projection used for world maps. Normally it is presented with multiple interruptions, most commonly of the major oceans. Its equal-area property makes it useful for presenting spatial distribution of phenomena.

Development The projection was developed in 1923 by John Paul Goode to provide an alternative to the Mercator projection for portraying global areal relationships. Goode offered variations of the interruption scheme for emphasizing the world’s land and the world’s oceans. Some variants include extensions that repeat regions in two different lobes of the interrupted map in order to show Greenland or eastern Russia undivided. The homolosine evolved from Goode’s 1916 experiments in interrupting the Mollweide projection. Because the Mollweide is sometimes called the "homolographic projection" (meaning, equal-area map), Goode fused the two names "homolographic" and "sinusoidal" (from the sinusoidal projection) to create the name "homolosine". Common in the 1960s, the Goode homolosine projection is often called an "orange-peel map" because of its resemblance to the flattened rind of a hand-peeled orange. In its most common form, the map interrupts the North Atlantic, the South Atlantic, the South Pacific, the Indian Ocean, and the entire east/west meridian of the map.

Details Up to latitudes 40°44′11.8″N/S, the map is projected according to the sinusoidal projection’s transformation. The higher latitudes are the top sections of a Mollweide projection, grafted to the sinusoidal midsection where the scale of the two projections matches. This grafting results in a kink in the meridians along the parallel of the graft. The projection’s equal-area property follows from the fact that its source projections are themselves both equal-area.

See also List of map projections

References

Further reading Goode, J. P. (1925). "The Homolosine projection – a new device for portraying the Earth's surface entire". Annals of the Association of American Geographers. 15 (3): 119–125. doi:10.2307/2560812. JSTOR 2560812. Susan, Schulten (2001). The geographical imagination in America, 1880–1950. Chicago: University of Chicago Press. ISBN 0-226-74055-2. OCLC 44578714.

External links Table of examples and properties of all common projections, from radicalcartography.net. Non-interrupted Goode Homolosine example (PDF)

Illustrations

Goode homolosine projection: Goode homolosine projection of the Earth
Goode homolosine projection of the Earth
Goode homolosine projection: Tissot indicatrix on Goode homolosine projection, 15° graticule.
Tissot indicatrix on Goode homolosine projection, 15° graticule.

Worked examples

Example 1 — a first encounter with Goode homolosine projection

Start with the simplest possible case. Write down what Goode homolosine projection claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In 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 Goode homolosine projection 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 Goode homolosine projection 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 Goode homolosine projection

In research
Goode homolosine projection appears in 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 Goode homolosine projection 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
Goode homolosine projection is common in secondary-school and first-year university syllabi. It links to neighbouring topics Equal-area projections, so understanding it makes those chapters shorter.
In everyday life
Look for Goode homolosine projection 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.
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How to study Goode homolosine projection in 20 minutes

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

Frequently asked questions

What is Goode homolosine projection in simple terms?

The Goode homolosine projection (or interrupted Goode homolosine projection) is a pseudocylindrical, equal-area, composite map projection used for world maps. Normally it is presented with multiple interruptions, most commonly of the major oceans.

Why does Goode homolosine projection matter?

Because it connects several 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 Goode homolosine projection?

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 Goode homolosine projection.

Tags

  • Equal-area projections

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