Skip to main content

Geographical Projected Coordinate System

A Geographical Coordinate System (GCS) and a Projected Coordinate System (PCS) are two key types of coordinate systems used in mapping and geographic information systems (GIS). Here's an explanation of each:


 Geographical Coordinate System (GCS)


A Geographical Coordinate System is a system that uses a three-dimensional spherical surface to define locations on the Earth. 


Key Characteristics:

1. Coordinates: Locations are given in latitude and longitude.

   - Latitude: Measures north-south position, with values ranging from +90° (North Pole) to -90° (South Pole).

   - Longitude: Measures east-west position, with values ranging from +180° (east) to -180° (west).

2. Datum: A GCS is based on a datum, which defines the size and shape of the Earth and the origin and orientation of the coordinate system. Common datums include WGS84, NAD83, and NAD27.

3. Usage: Suitable for global data or when precision mapping is not critical (e.g., global maps, GPS).


Example:

- A location like New York City can be specified as (40.7128° N, 74.0060° W).


 Projected Coordinate System (PCS)


A Projected Coordinate System is a flat, two-dimensional representation of the Earth's surface. It is created by transforming the latitude and longitude coordinates from the GCS into planar coordinates.


Key Characteristics:

1. Coordinates: Locations are given in Cartesian coordinates (x, y), typically in meters or feet.

2. Projection: The transformation from the spherical surface of a GCS to a flat surface is done using a map projection. There are many types of projections, each with different properties and uses.

   - Types of Projections: Common ones include Mercator, Transverse Mercator, Lambert Conformal Conic, and Albers Equal-Area.

3. Distortion: All projections distort some aspect of reality (area, shape, distance, or direction), but they can minimize distortion in specific regions or aspects.

4. Usage: More accurate for detailed, localized mapping (e.g., city planning, engineering, detailed topographic maps).


Example:

- A PCS might project New York City coordinates to (x = 583960, y = 4507520) meters in a particular projection like UTM (Universal Transverse Mercator) Zone 18N.


 Comparison


1. Accuracy and Use:

   - GCS is better for representing large areas like continents or the entire globe.

   - PCS is better for small areas where high accuracy and detailed maps are needed.


2. Representation:

   - GCS uses a spherical representation (latitude and longitude).

   - PCS uses a flat, two-dimensional plane (x and y coordinates).


3. Distortion:

   - GCS does not distort distances and areas on the globe but is not suitable for detailed maps.

   - PCS distorts distances, areas, or angles depending on the projection used but is essential for accurate, localized mapping.


 Practical Example


When using GPS coordinates, you're using a GCS. When you take those GPS coordinates and put them on a detailed city map for navigation or planning, you're converting them to a PCS to ensure accuracy and usability in that specific area.


Let's delve deeper into the Geographical Coordinate System (GCS) and Projected Coordinate System (PCS), exploring their components, usage, and the process of projection transformation.


 Geographical Coordinate System (GCS)


Components:


1. Latitude and Longitude:

   - Latitude: Measures how far north or south a point is from the Equator. It ranges from +90° (North Pole) to -90° (South Pole). Each degree of latitude is approximately 111 kilometers apart.

   - Longitude: Measures how far east or west a point is from the Prime Meridian, which is set at 0°. It ranges from +180° east to -180° west. Longitude lines converge at the poles and are widest at the Equator.


2. Datum:

   - A datum defines the position of the spheroid relative to the center of the Earth. Different datums fit the Earth's shape better in different regions. Examples include:

     - WGS84 (World Geodetic System 1984): A global datum used by GPS.

     - NAD83 (North American Datum 1983): Common in North America.

     - NAD27 (North American Datum 1927): Older, used in the USA.


3. Prime Meridian and Equator:

   - The Prime Meridian (0° longitude) runs through Greenwich, England.

   - The Equator (0° latitude) divides the Earth into the Northern and Southern Hemispheres.


Usage:


- Global Mapping: Used in global positioning systems (GPS) and for mapping large areas where detailed precision is less critical.

- Navigation: Essential for air and sea navigation.


Example:


- Coordinates for the Statue of Liberty: 40.6892° N latitude, 74.0445° W longitude.


 Projected Coordinate System (PCS)


Components:


1. Cartesian Coordinates (x, y):

   - These coordinates are used in a two-dimensional plane, typically measured in meters or feet. The origin (0,0) can vary depending on the projection.


2. Projection:

   - A mathematical formula that transforms the spherical coordinates (latitude, longitude) onto a flat plane.

   - Types of Projections:

     - Mercator: Preserves angles and shapes but distorts distances and areas, especially near the poles. Used for nautical navigation.

     - Transverse Mercator: Minimizes distortion along a central meridian. Used in the UTM system.

     - Lambert Conformal Conic: Preserves shapes and angles, used for aeronautical charts.

     - Albers Equal-Area Conic: Preserves area, used for statistical maps.


3. Coordinate Systems within Projections:

   - UTM (Universal Transverse Mercator): Divides the world into 60 zones, each 6° of longitude wide, with a central meridian. Minimizes distortion within each zone.

   - State Plane Coordinate System (SPCS): Used in the United States, divides the country into zones to minimize distortion for detailed mapping.


Usage:


- Local and Regional Mapping: Ideal for city planning, engineering, and detailed maps where high accuracy is essential.

- GIS Applications: Used in geographic information systems to overlay various types of data accurately.


Example:


- Coordinates for the Statue of Liberty in UTM Zone 18N: approximately x = 580,000 meters, y = 4,505,000 meters.


 Projection Transformation


Process:


1. Selection of Projection: Choose a projection based on the area of interest and the purpose of the map. For example, UTM for local mapping, Mercator for navigation.


2. Transformation Formula: Apply the mathematical formulas that define the projection to convert GCS coordinates (latitude, longitude) into PCS coordinates (x, y). Each projection has specific formulas.


3. Minimizing Distortion: Understand that each projection has inherent distortions. Select the one that minimizes the type of distortion most critical for the map's purpose (area, shape, distance, direction).


Example Transformation:


- To convert 40.6892° N, 74.0445° W (GCS) to UTM coordinates:

  - Determine the UTM zone (18N in this case).

  - Apply the Transverse Mercator projection formula to get x and y coordinates.


 Practical Applications


GCS:


- Global Positioning System (GPS): Uses WGS84 to provide precise locations worldwide.

- Global Data Analysis: Climate models, global demographic studies.


PCS:


- Urban Planning: Detailed city maps, infrastructure development.

- Environmental Management: Mapping forests, watersheds for conservation.

- Engineering Projects: Designing and constructing buildings, roads, bridges.


A Geographical Coordinate System is essential for understanding positions on the Earth on a global scale, using latitude and longitude. However, for detailed and precise mapping, especially over smaller areas, a Projected Coordinate System is crucial as it transforms the Earth's surface onto a flat plane, minimizing distortions in specific regions or for specific uses. Understanding both systems and their appropriate applications is fundamental for accurate geographic representation and analysis.


Comments

Popular posts from this blog

Photogrammetry – Types of Photographs

In photogrammetry, aerial photographs are categorized based on camera orientation , coverage , and spectral sensitivity . Below is a breakdown of the major types: 1️⃣ Based on Camera Axis Orientation Type Description Key Feature Vertical Photo Taken with the camera axis pointing directly downward (within 3° of vertical). Used for maps and measurements Oblique Photo Taken with the camera axis tilted away from vertical. Covers more area but with distortions Low Oblique: Horizon not visible High Oblique: Horizon visible 2️⃣ Based on Number of Photos Taken Type Description Single Photo One image taken of an area Stereoscopic Pair Two overlapping photos for 3D viewing and depth analysis Strip or Mosaic Series of overlapping photos covering a long area, useful in mapping large regions 3️⃣ Based on Spectral Sensitivity Type Description Application Panchromatic Captures images in black and white General mapping Infrared (IR) Sensitive to infrared radiation Veget...

Photogrammetry – Geometry of a Vertical Photograph

Photogrammetry is the science of making measurements from photographs, especially for mapping and surveying. When the camera axis is perpendicular (vertical) to the ground, the photo is called a vertical photograph , and its geometry is central to accurate mapping.  Elements of Vertical Photo Geometry In a vertical aerial photograph , the geometry is governed by the central projection principle. Here's how it works: 1. Principal Point (P) The point on the photo where the optical axis of the camera intersects the photo plane. It's the geometric center of the photo. 2. Nadir Point (N) The point on the ground directly below the camera at the time of exposure. Ideally, in a perfect vertical photo, the nadir and principal point coincide. 3. Photo Center (C) Usually coincides with the principal point in a vertical photo. 4. Ground Coordinates (X, Y, Z) Real-world (map) coordinates of objects photographed. 5. Flying Height (H) He...

Raster Data Structure

Raster Data Raster data is like a digital photo made up of small squares called cells or pixels . Each cell shows something about that spot — like how high it is (elevation), how hot it is (temperature), or what kind of land it is (forest, water, etc.). Think of it like a graph paper where each box is colored to show what's there. Key Points What's in the cell? Each cell stores information — for example, "water" or "forest." Where is the cell? The cell's location comes from its place in the grid (like row 3, column 5). We don't need to store its exact coordinates. How Do We Decide a Cell's Value? Sometimes, one cell covers more than one thing (like part forest and part water). To choose one value , we can: Center Point: Use whatever feature is in the middle. Most Area: Use the feature that takes up the most space in the cell. Most Important: Use the most important feature (like a road or well), even if it...

Photogrammetry

Photogrammetry is the science of taking measurements from photographs —especially to create maps, models, or 3D images of objects, land, or buildings. Imagine you take two pictures of a mountain from slightly different angles. Photogrammetry uses those photos to figure out the shape, size, and position of the mountain—just like our eyes do when we see in 3D! Concepts and Terminologies 1. Photograph A picture captured by a camera , either from the ground (terrestrial) or from above (aerial or drone). 2. Stereo Pair Two overlapping photos taken from different angles. When seen together, they help create a 3D effect —just like how two human eyes work. 3. Overlap To get a 3D model, photos must overlap each other: Forward overlap : Between two photos in a flight line (usually 60–70%) Side overlap : Between adjacent flight lines (usually 30–40%) 4. Scale The ratio of the photo size to real-world size. Example: A 1:10,000 scale photo means 1 cm on the photo...

Solar Radiation and Remote Sensing

Satellite Remote Sensing Satellite remote sensing is the science of acquiring information about Earth's surface and atmosphere without physical contact , using sensors mounted on satellites. These sensors detect and record electromagnetic radiation (EMR) that is either emitted or reflected from the Earth's surface. Solar Radiation & Earth's Energy Balance Solar Radiation is the primary source of energy for Earth's climate system. It originates from the Sun and travels through space as electromagnetic waves . Incoming Shortwave Solar Radiation (insolation) consists mostly of ultraviolet, visible, and near-infrared wavelengths . When it reaches Earth, it can be: Absorbed by the atmosphere, clouds, or surface Reflected back to space Scattered by atmospheric particles Outgoing Longwave Radiation is the infrared energy emitted by Earth back into space after absorbing solar energy. This process helps maintain Earth's thermal bala...