Polar Stereographic (Elliptical) Projection
Jun 18,2026
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Introduction
Polar Stereographic (Elliptical) Projection is a conformal projection centered on the poles, formed by orthographically projecting the Earth's surface from the pole onto a plane. The meridians appear as radiating straight lines, and the parallels appear as concentric circles (or circular arcs). By employing elliptical parameters, it more accurately matches the Earth's ellipsoidal shape, maintaining relatively low distortion in polar regions. It is commonly used for polar map production and navigation.
Projection Basic
The Polar Stereographic (Elliptical) Projection is a conformal projection. Its projection method involves projecting the Earth's surface onto a plane tangent to the Earth's ellipsoid at or near the pole, with the projection plane tangent or secant to the Earth near the pole. The projection maintains angular accuracy, with meridians and parallels appearing as intersecting straight lines or curves on the projection plane. Meridians converge at the pole, and parallels appear as concentric circles. It is suitable for high-accuracy polar mapping, capable of accurately preserving direction and local shape.
Pros
- Conformal property: As a conformal projection, it maintains local angular accuracy in polar regions, ensuring precise directional and positional relationships.
- Straight, perpendicular meridians and parallels: Meridians and parallels appear as straight lines that intersect perpendicularly on the projection plane, forming a regular rectangular grid. This property makes coordinate transformation and data mapping intuitive, facilitating positioning and measurement. It is widely used in digital maps and geographic information systems (GIS).
- Suitable for small-scale polar mapping: Within small areas, the Polar Stereographic (Elliptical) Projection maintains good shape and directional accuracy, meeting the needs of local mapping in polar regions, such as polar scientific expeditions and resource exploration.
Cons
- Severe polar distortion: As latitude increases, area and distance exaggeration becomes very pronounced. In polar regions, the projection stretches the Earth's surface to an infinite plane, leading to loss or deformation of geographic information in those areas.
- Unsuitable for global-scale data analysis: Due to severe polar distortion, this projection is unsuitable for global-scale data analysis, area statistics, and other tasks. In global maps, the area distortion in polar regions can mislead the understanding and analysis of geographic phenomena, affecting decision-making accuracy.
- Inaccurate distance measurement at high latitudes: In high-latitude regions, distances are exaggerated with latitude, leading to inaccurate distance measurements. This introduces significant errors in applications requiring precise distance measurement, such as polar transportation planning and resource logistics.
Application Scenario
The Polar Stereographic (Elliptical) Projection, due to its conformal properties and regular graticule grid, is commonly used in polar scientific expeditions for producing local high-accuracy maps to support precise navigation and positioning. It aids in analyzing polar resource distribution during resource exploration, provides reliable geographic information support for military activities in polar regions, and meets the needs of digital maps and GIS for intuitive polar data visualization and processing.
Example
1. A polar projection map displayed in OpenLayers is shown below.
2. The Polar Stereographic Projection is illustrated.
Related GIS Projections
Vertical Near-side Perspective Projection
Two-point Equidistant Projection
Times Projection
Wagner IV Projection
References
- https://en.wikipedia.org/wiki/Universal_polar_stereographic_coordinate_system
- https://en.wikipedia.org/wiki/Stereographic_map_projection
- https://www.bluemarblegeo.com/knowledgebase/calculator/projections/Polar_Stereographic.htm