Skip to main content

LiDaR Principles and applications

LIDAR, which stands for Light Detection and Ranging, is a remote sensing technology that uses laser light to measure distances and create detailed three-dimensional representations of objects and environments. Here are the fundamental principles of LIDAR remote sensing:


1. Laser Emission: LIDAR systems emit laser pulses towards the target area. These laser pulses are typically in the form of short, intense bursts of light.


2. Propagation of Light: The emitted laser pulses travel through the atmosphere, where they may interact with particles or molecules, experiencing scattering and absorption. The laser light continues until it strikes an object or a surface.


3. Reflection or Scattering: When the laser pulse encounters an object or surface, a portion of the light is reflected back towards the LIDAR sensor. The time it takes for the laser pulse to travel to the target and return is measured.


4. Time-of-Flight Measurement: LIDAR calculates the distance to the target by precisely measuring the time it takes for the laser pulse to travel to the target and back. This is done using the speed of light as a constant.


5. Multiple Measurements: LIDAR systems typically emit thousands or even millions of laser pulses per second and record the return time and intensity of each pulse. This results in a dense cloud of points, often referred to as a "point cloud."


6. Data Processing: The collected data is processed to generate a detailed three-dimensional representation of the target area. This point cloud can be used to create digital elevation models, maps, or 3D models of objects and terrain.


7. Applications: LIDAR remote sensing is used in various applications, including topographic mapping, forestry management, urban planning, archaeology, autonomous vehicles, and more. Its ability to provide precise elevation and object information makes it invaluable for many industries.


LIDAR technology can be implemented in various ways, such as airborne LIDAR using aircraft or UAVs, terrestrial LIDAR for ground-based scanning, and even spaceborne LIDAR for planetary exploration. It has revolutionized the way we collect detailed geospatial information and has numerous practical applications in science, engineering, and environmental monitoring.



1. ICESat-2 (Ice, Cloud, and land Elevation Satellite-2): Launched in 2018 by NASA, ICESat-2 is designed for Earth science research, specifically to measure changes in ice sheet thickness and sea ice freeboard. It uses a LIDAR system called the Advanced Topographic Laser Altimeter System (ATLAS) to collect elevation data.


2. GEDI (Global Ecosystem Dynamics Investigation): Launched as part of the International Space Station (ISS) payload, GEDI is a LIDAR instrument that measures the three-dimensional structure of forests and ecosystems. It provides valuable data for understanding the Earth's carbon cycle.


3. LRO (Lunar Reconnaissance Orbiter): While primarily designed for lunar exploration, NASA's LRO carries a LIDAR instrument called the Lunar Orbiter Laser Altimeter (LOLA). LOLA measures the surface topography of the Moon with high precision.


4. TanDEM-X: This is a German radar satellite mission operated in conjunction with TerraSAR-X. Although it primarily uses radar technology, it also features a bistatic mode that, when combined with TerraSAR-X, can produce a global digital elevation model (DEM) with unprecedented accuracy.


5. ISAT (Indian Satellite for Antarctic Observation): ISAT-1, an Indian remote sensing satellite, was equipped with a LIDAR altimeter. It was used for monitoring ice sheet dynamics and elevation changes in the polar regions.


6. ATLAS (Advanced Topographic Laser Altimeter System): ATLAS is a LIDAR instrument onboard the Earth, Science, and Climate Pathfinder satellite, which is part of NASA's Earth System Science Pathfinder Program. It's used to monitor ice sheet elevation changes.





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