Wagner Projection
The Wagner Projection is a modified azimuthal projection developed by Winkel in 1921. It is essentially a projection of a sphere on a plane, designed to minimize three types of distortion: area, direction, and distance. The projection is neither equal-area nor conformal, and its main feature is that all latitudes are curved except for the poles and the equator, which are straight lines. Its design is achieved through graphic design rather than mathematical equations, and it has certain characteristics in terms of visual balance and global deformation, but it has disadvantages such as non-equal areas and non-conformal angles. In local areas or specific applications, characteristics such as area, shape, and angle may be significantly distorted.
2025-09-16 14:47:01Gauss–Krüger Projection
Gauss–Krüger projection is a map projection based on the Transverse Mercator projection, developed by the German geographers Carl Friedrich Gauss and Johann Heinrich Krüger. It is widely used for large-scale topographic maps and precision surveying, and is adopted as part of the national coordinate system by many countries, notably Germany, Russia, and China.
2025-09-16 14:47:00Lambert Azimuthal Equal-Area Projection
Lambert Azimuthal Equal-Area Projection is an equal-area azimuthal projection proposed by German mathematician Johann Heinrich Lambert in 1772. This projection maps points on the earth’s surface onto a plane through spherical projection, keeping the projection area unchanged, that is, the area ratio of the area before and after the projection is strictly equal. There is no deformation at the center of the projection, and as the distance from the center increases, the angle and shape deformation gradually increase, but the area deformation is always zero.
2025-09-16 14:47:00UTM (Universal Transverse Mercator)
UTM projection (Universal Transverse Mercator) is a coordinate system that divides the earth’s surface into zones and applies the Transverse Mercator projection to each zone. By dividing the earth into 60 zones, each zone is 6 degrees longitude apart, and projecting independently in each zone, high-precision plane rectangular coordinates can be obtained.
2025-09-16 14:46:59Web Mercator (Pseudo Mercator, EPSG:3857)
Pseudo Mercator projection is a sphere-based conformal cylindrical projection. It converts longitude and latitude coordinates into plane rectangular coordinates by approximating the earth as a sphere and using a tangent cylindrical projection. It is widely used in global Web map services (such as Google Maps and OpenStreetMap) and supports seamless splicing and layered tile loading.
2025-09-16 14:46:59Transverse Mercator Projection
Transverse Mercator projection is a conformal cross-cylindrical projection that cuts the Earth ellipsoid along the meridian (central meridian) and unfolds it into a plane. It is widely used in large-scale topographic mapping and national coordinate systems (such as the UTM coordinate system) in mid-latitude regions.
2025-09-16 14:46:59Mercator Projection
Mercator Projection is one of the most famous map projections. It was first proposed by Franz Walter Mercator (Gerardus Mercator) in 1569 and is mainly used for drawing nautical charts. Mercator projection is a kind of orthogonal cylindrical projection, also known as “standard cylindrical projection”. Its characteristic is that it can project the longitude and latitude coordinates of the earth onto a plane, keeping the angle unchanged, so it is very useful in navigation and aviation.
2025-09-16 14:46:58Longitude / Latitude Projection
Longitude / Latitude Projection uses the longitude and latitude coordinate system of the earth, usually in degrees. The basic principle is to imagine a cylinder that is consistent with the direction of the earth’s axis and cuts or severing the earth, project the longitude and latitude grid onto the cylindrical surface according to the equiangular condition, and then unfold the cylindrical surface into a plane to obtain a plane longitude and latitude grid. After projection, the meridians are a set of vertical equidistant parallel straight lines, and the latitudes are a set of parallel straight lines perpendicular to the meridians. The interval between adjacent latitudes increases from the equator to the poles.
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