Skip to content
  • Home
  • Categories
    • Geology
    • Geography
    • Space and Astronomy
  • About
    • Privacy Policy
  • About
  • Privacy Policy
Our Planet TodayAnswers for geologist, scientists, spacecraft operators
  • Home
  • Categories
    • Geology
    • Geography
    • Space and Astronomy
  • About
    • Privacy Policy
on April 25, 2022

What does the Goode Homolosine projection distort?

Space and Astronomy

Contents:

  • What distortions does Goode’s projection minimize?
  • What does the Goode homolosine projection show us?
  • What are the qualities of the Goode’s interrupted Homolosine projection?
  • What does a projection map distort?
  • What are the advantages and disadvantages of Goode homolosine projection?
  • What does the Robinson projection distort?
  • Where is most distortion found on a Robinson projection?
  • Where is most distortion found on the Robinson?
  • What does Mercator projection distort?
  • Does the Mercator projection distort direction?
  • Does the Mercator projection distort distance?
  • What does the Mollweide projection distortion?
  • What is the Mollweide projection useful for?
  • Why is Mollweide projection called elliptical?
  • What is sinusoidal projection in geography?
  • What is sinusoidal motion?
  • Who invented sinusoidal projection?
  • What is sinusoidal physics?
  • Where are sinusoidal waves used?
  • What are sinusoidal waves What are its types?
  • What does Lambda mean in physics?
  • What does an upside down Y mean?
  • What is λ in statistics?

What distortions does Goode’s projection minimize?

Goode’s homolosine map projection is designed to minimize distortion for the entire world. It is an interrupted pseudocylindrical equal-area projection. John Paul Goode developed the projection in 1925.

What does the Goode homolosine projection show us?

The Goode homolosine projection (or interrupted Goode’s homolosine projection) is a pseudo- cylindrical, 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.

What are the qualities of the Goode’s interrupted Homolosine projection?

The Interrupted Goode Homolosine projection (Goode’s) is an interrupted, pseudocylindrical, equal-area, composite map projection that can present the entire world on one map. Global land masses are presented with their areas in proper proportion, with minimal interruption, and minimal overall distortion.

What does a projection map distort?

For example, map projections distort distance, direction, scale, and area. Every projection has strengths and weaknesses. All in all, it is up to the cartographer to determine what projection is most favorable for its purpose.

What are the advantages and disadvantages of Goode homolosine projection?

Goode’s Homolosine Interrupted Projection

The advantage of this projection is each of the continents are the correct size and in proportion to one another. The disadvantage is distance and direction are not accurate.

What does the Robinson projection distort?

The Robinson projection is neither conformal nor equal-area. It generally distorts shapes, areas, distances, directions, and angles. The distortion patterns are similar to common compromise pseudocylindrical projections. Area distortion grows with latitude and does not change with longitude.

Where is most distortion found on a Robinson projection?

The Robinson projection is not conformal; shapes are distorted more than they would be in a truly conformal projection. However, shapes are not distorted very badly within about 45° north or south of the equator or within about 45° of the map’s central meridian.

Where is most distortion found on the Robinson?

Robinson (1963)

Directions true along all parallels and along central meridian. Distances constant along the equator and other parallels, but scales vary. All points have some distortion but it is very low along the equator and within 45° of centre. Distortion greatest near the poles.

What does Mercator projection distort?

Although the linear scale is equal in all directions around any point, thus preserving the angles and the shapes of small objects, the Mercator projection distorts the size of objects as the latitude increases from the equator to the poles, where the scale becomes infinite.



Does the Mercator projection distort direction?

Distortion. Mercator is a conformal map projection. Directions, angles, and shapes are maintained at infinitesimal scale. Any straight line drawn on this projection represents an actual compass bearing.

Does the Mercator projection distort distance?

The images below show that the popular Mercator projection distorts are and distance everywhere but near the equator. Distortion along the parallels and meridians (left), in area (center), and in form (right). Mercator preserves the form (shape) of areas but greatly exaggerates distance and area.

What does the Mollweide projection distortion?

The Mollweide projection is an equal-area map projection. It preserves the size of figures, but heavily distorts the shapes when getting nearer to the edge of the map. Mollweide maps are especially used for global maps where its equal-area property helps to display global distributions.

What is the Mollweide projection useful for?

Usage. Mollweide projection is commonly used in small-scale mapping and thematic maps to illustrate accurate area characteristics. Thus, it is used mainly on maps that require accurate areas as opposed to those requiring accurate shapes and angles. It can also be used to show distributions of global data.

Why is Mollweide projection called elliptical?

In 1805, Karl Brandan Mollweide (1774–1825) announced an equal-area world map projection that is aesthetically more pleasing than the sinusoidal because the world is placed in an ellipse with axes in a 2:1 ratio and all the meridians are equally spaced semiellipses.



What is sinusoidal projection in geography?

Description. The sinusoidal projection is a pseudocylindrical equal-area projection displaying all parallels and the central meridian at true scale. The boundary meridians bulge outward excessively producing considerable shape distortion near the map outline.

What is sinusoidal motion?

Sinusoidal motion is basically a periodic motion. Every fixed amount of radians or time, the cycle repeats. This is seen if the graph is plotted.

Who invented sinusoidal projection?

Gerardus Mercator, Nicolas Sanson, and John Flamsteed – mathematicians who developed the technique.

What is sinusoidal physics?

The sine or sinusoidal wave is a curve that describes a smooth repetitive oscillation. We can define the sine wave as “The wave form in which the amplitude is always proportional to sine of its displacement angle at every point of time”. All waves can be made by adding up sine waves.



Where are sinusoidal waves used?

Sine waves are used in technical analysis and trading to help identify patterns and cross-overs related to oscillators.

What are sinusoidal waves What are its types?

1: Two basic types of waves. (a) Longitudinal wave, where the oscillatory motion of the particles is in the same direction as that of the wave. (b) Transverse wave, where the oscillatory motion of the particles is perpendicular to that of the wave.

What does Lambda mean in physics?

Wavelength

Wavelength is usually denoted by the Greek letter lambda (λ); it is equal to the speed (v) of a wave train in a medium divided by its frequency (f): λ = v/f.

What does an upside down Y mean?

So the relationship between speed, frequency and wavelength is: Incidentally, the funny upside-down y is a greek letter called “lamda”.



What is λ in statistics?

Wilks’ lambda (Λ) is a test statistic that’s reported in results from MANOVA , discriminant analysis, and other multivariate procedures. Other similar test statistics include Pillai’s trace criterion and Roy’s ger criterion.

Recent

  • Exploring the Geological Features of Caves: A Comprehensive Guide
  • What Factors Contribute to Stronger Winds?
  • The Scarcity of Minerals: Unraveling the Mysteries of the Earth’s Crust
  • How Faster-Moving Hurricanes May Intensify More Rapidly
  • Adiabatic lapse rate
  • Exploring the Feasibility of Controlled Fractional Crystallization on the Lunar Surface
  • The Greenhouse Effect: How Rising Atmospheric CO2 Drives Global Warming
  • Examining the Feasibility of a Water-Covered Terrestrial Surface
  • What is an aurora called when viewed from space?
  • Measuring the Greenhouse Effect: A Systematic Approach to Quantifying Back Radiation from Atmospheric Carbon Dioxide
  • Asymmetric Solar Activity Patterns Across Hemispheres
  • Unraveling the Distinction: GFS Analysis vs. GFS Forecast Data
  • The Role of Longwave Radiation in Ocean Warming under Climate Change
  • Esker vs. Kame vs. Drumlin – what’s the difference?

Categories

  • English
  • Deutsch
  • Français
  • Home
  • About
  • Privacy Policy

Copyright Our Planet Today 2025

We use cookies on our website to give you the most relevant experience by remembering your preferences and repeat visits. By clicking “Accept”, you consent to the use of ALL the cookies.
Do not sell my personal information.
Cookie SettingsAccept
Manage consent

Privacy Overview

This website uses cookies to improve your experience while you navigate through the website. Out of these, the cookies that are categorized as necessary are stored on your browser as they are essential for the working of basic functionalities of the website. We also use third-party cookies that help us analyze and understand how you use this website. These cookies will be stored in your browser only with your consent. You also have the option to opt-out of these cookies. But opting out of some of these cookies may affect your browsing experience.
Necessary
Always Enabled
Necessary cookies are absolutely essential for the website to function properly. These cookies ensure basic functionalities and security features of the website, anonymously.
CookieDurationDescription
cookielawinfo-checkbox-analytics11 monthsThis cookie is set by GDPR Cookie Consent plugin. The cookie is used to store the user consent for the cookies in the category "Analytics".
cookielawinfo-checkbox-functional11 monthsThe cookie is set by GDPR cookie consent to record the user consent for the cookies in the category "Functional".
cookielawinfo-checkbox-necessary11 monthsThis cookie is set by GDPR Cookie Consent plugin. The cookies is used to store the user consent for the cookies in the category "Necessary".
cookielawinfo-checkbox-others11 monthsThis cookie is set by GDPR Cookie Consent plugin. The cookie is used to store the user consent for the cookies in the category "Other.
cookielawinfo-checkbox-performance11 monthsThis cookie is set by GDPR Cookie Consent plugin. The cookie is used to store the user consent for the cookies in the category "Performance".
viewed_cookie_policy11 monthsThe cookie is set by the GDPR Cookie Consent plugin and is used to store whether or not user has consented to the use of cookies. It does not store any personal data.
Functional
Functional cookies help to perform certain functionalities like sharing the content of the website on social media platforms, collect feedbacks, and other third-party features.
Performance
Performance cookies are used to understand and analyze the key performance indexes of the website which helps in delivering a better user experience for the visitors.
Analytics
Analytical cookies are used to understand how visitors interact with the website. These cookies help provide information on metrics the number of visitors, bounce rate, traffic source, etc.
Advertisement
Advertisement cookies are used to provide visitors with relevant ads and marketing campaigns. These cookies track visitors across websites and collect information to provide customized ads.
Others
Other uncategorized cookies are those that are being analyzed and have not been classified into a category as yet.
SAVE & ACCEPT