Skip to main content

Geometric Correction


Geometric Correction:


- Geometric correction is a critical process in remote sensing and digital image processing. It involves adjusting and aligning an image so that it accurately represents the Earth's surface in terms of scale, orientation, and spatial accuracy. This correction compensates for various geometric distortions and errors introduced during image acquisition and sensor characteristics, ensuring that the image can be used for precise geospatial analysis and mapping.


Source of Geometric Error:


- Geometric errors in remote sensing arise from various sources, including inaccuracies in sensor characteristics, platform movement, Earth's curvature, terrain relief, atmospheric conditions, and other factors. These errors can lead to distortions, misalignments, and inaccuracies in the positioning and representation of objects within an image.


Types of Geometric Error:


- Geometric errors can manifest in different ways, including:

  1. Scale Error: Inaccurate representation of distances in the image.

  2. Positional Error: Errors in the location of objects within the image.

  3. Angular Error: Errors in the orientation or rotation of objects.

  4. Distortion: Misrepresentation of object shapes or sizes.

  5. Parallax Error: Discrepancies in object positions due to elevation differences.

  6. Relief Displacement: Displacements of objects due to variations in terrain elevation.

  7. Atmospheric Refraction: Errors due to the bending of light in the atmosphere.

  8. Satellite Ephemeris Errors: Errors in satellite position data.

  9. DEM Errors: Inaccuracies in the Digital Elevation Model used for terrain correction.

  10. Time-Dependent Errors: Errors that change over time.

  11. Resampling Error: Errors introduced during pixel value interpolation.

  12. Control Point Error: Errors in the accuracy of ground control points.


Types of Geometric Correction:


- Geometric correction techniques are used to rectify or mitigate these errors. Common types include:

  1. Image-to-Map Transformation: Matching control points to align the image with a map.

  2. Rubber Sheet Transformation: Non-linear correction using polynomial functions.

  3. Affine Transformation: Linear correction for basic distortions.

  4. Projective Transformation (Homography): Correcting complex distortions, including perspective.

  5. Orthorectification: Comprehensive correction accounting for terrain and Earth's curvature.

  6. Bundle Adjustment: Simultaneous adjustment of multiple images for 3D mapping.

  7. Sensor Model-Based Correction: Using detailed sensor models for correction.

  8. Resampling: Interpolating pixel values after correction.


Each type of geometric correction is chosen based on the specific nature of the errors in the imagery and the desired level of accuracy for the application at hand.

Comments

Popular posts from this blog

Groundwater – Porosity and Permeability

Groundwater refers to the water that resides beneath the Earth's surface in the pores and crevices of rock, sediment, and soil. Two key properties that influence the movement and storage of groundwater are porosity and permeability: 1. Porosity:    - Definition: Porosity refers to the volume percentage of void spaces (pores or openings) in a geological material, such as soil or rock.    - Role: Porosity determines how much water a subsurface material can hold. It is a measure of the material's capacity to store water.    - Factors: Porosity is influenced by the size and arrangement of particles within the material. Highly porous materials have more void spaces, while less porous materials have fewer.    - Units: Porosity is expressed as a percentage, with 0% indicating complete solidity (no pore spaces) and 100% indicating complete void space. 2. Permeability:    - Definition: Permeability refers to the ability of a geological material to transmit fluids, such as water. It meas

Ground Water

Groundwater Terminology, Concepts, and Facts Key Terms Aquifer: A geological formation that can store and transmit significant quantities of water. Water Table: The upper surface of the saturated zone in an aquifer. Recharge: The process of replenishing groundwater through precipitation or other sources. Discharge: The process of groundwater flowing out of an aquifer, typically into surface water bodies or through wells. Hydraulic Gradient: The slope of the water table. Darcy's Law: A law that describes the flow of groundwater through porous media. Permeability: The ability of a material to transmit water. Porosity: The amount of void space in a material. Concepts Groundwater Flow: Groundwater moves from areas of higher hydraulic head to areas of lower hydraulic head. Groundwater Contamination: The introduction of pollutants into groundwater. Groundwater Depletion: The excessive extraction of groundwater, leading to a decline in water table levels. Saltwater Intrusion:

Artisan Wells Basins

Artisan Wells and Basins Artesian wells are a type of well that harnesses the natural pressure of water trapped underground to force water to the surface without pumping. This phenomenon occurs in specific geological formations known as artesian basins . Key Terminologies and Concepts Aquifer: A geological formation that can store and transmit water. It is typically made up of porous rocks or sediments like sandstone or gravel. Confined Aquifer: An aquifer that is sandwiched between two impermeable layers (like clay or shale) that prevent water from escaping. Artesian Basin: A geological structure where a confined aquifer is tilted and has a recharge area at a higher elevation than the discharge area. This creates a pressure gradient that forces water to flow upwards. Potentiometric Surface: The theoretical level to which water would rise in a well drilled into an artesian aquifer if there were no restrictions. It is determined by the pressure head in the aquifer. Flowing Artesian

Watershed. Catchment. Basin

A watershed, also known as a river basin or drainage basin, is a fundamental concept in geohydrology and hydrology. It refers to a specific geographic area or region of land where all the surface water, including rainfall, snowmelt, and runoff, drains into a common outlet, such as a river, lake, or ocean. Here's an explanation of each term: 1. Watershed: A watershed is essentially a natural hydrological unit defined by the topography of the land. It represents the entire area from which all precipitation and surface water flow eventually gathers at a single point. This point is typically where the main river or stream within the watershed exits into a larger body of water, such as an ocean. Watersheds come in various sizes, from small ones that encompass a few square miles to enormous ones that cover entire continents. 2. River/Drainage Basin: A river basin or drainage basin is another way to describe a watershed. It's the land area that collects and channels water into a river

Discrete Detectors and Scanning mirrors Across the track scanner Whisk broom scanner.

Multispectral Imaging Using Discrete Detectors and Scanning Mirrors (Across-Track Scanner or Whisk Broom Scanner) Multispectral Imaging:  This technique involves capturing images of the Earth's surface using multiple sensors that are sensitive to different wavelengths of electromagnetic radiation.  This allows for the identification of various features and materials based on their spectral signatures. Discrete Detectors:  These are individual sensors that are arranged in a linear or array configuration.  Each detector is responsible for measuring the radiation within a specific wavelength band. Scanning Mirrors:  These are optical components that are used to deflect the incoming radiation onto the discrete detectors.  By moving the mirrors,  the sensor can scan across the scene,  capturing data from different points. Across-Track Scanner or Whisk Broom Scanner:  This refers to the scanning mechanism where the mirror moves perpendicular to the direction of flight.  This allows for t