To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Goode homolosine projection

From Wikipedia, the free encyclopedia

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

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. Its equal-area property makes it useful for presenting spatial distribution of phenomena.

YouTube Encyclopedic

  • 1/5
    Views:
    155 562
    646 415
    22 639
    67 555
    886
  • Types of Map Projections [AP Human Geography]
  • Why every world map is wrong - Kayla Wolf
  • Map Projections & Types of Maps [AP Human Geography Unit 1 Topic 1] (1.1)
  • How do Map Projections Work?
  • Map Projections- Popular Maps You Need To Know: Part 2

Transcription

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.[1]

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".[2] 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

References

  1. ^ Snyder, John Parr (1993). Flattening the earth : two thousand years of map projections. Chicago: University of Chicago Press. pp. 167–168. ISBN 9780226767475. OCLC 26764604.
  2. ^ Monmonier, Mark S. (2015). Mapping It Out: Expository Cartography for the Humanities and Social Sciences. University of Chicago Press. p. 40. ISBN 9780226217857. OCLC 905918505.

Further reading

External links

This page was last edited on 21 March 2023, at 08:34
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.