Object-based classification in remote sensing

Object-based classification in remote sensing is a method of image analysis that involves grouping pixels into distinct objects or features based on their characteristics, such as shape, size, and texture. The goal of object-based classification is to identify and map specific features or land covers, such as buildings, roads, or vegetation types, within an image.

The process of object-based classification typically involves several steps:

Segmentation: The image is divided into smaller, homogeneous regions or segments, based on characteristics such as color, texture, and shape.

Feature extraction: Characteristics such as size, shape, and texture are extracted from the segments, creating a set of features that can be used to differentiate one segment from another.

Classification: The segments are then classified into different classes or categories, such as buildings, roads, or vegetation, based on the extracted features.

Post-classification: The classified segments are then combined to create a final map of the study area, where each object is labeled with its corresponding class.

An example of object-based classification in remote sensing is the use of high-resolution satellite images to map and monitor urban areas. In this application, the image is first segmented into smaller regions, such as buildings, roads, and parks. Then, features such as size, shape, and texture are extracted from each segment. Finally, the segments are classified into different classes, such as residential, commercial, or industrial areas.

In summary, Object-based classification in remote sensing is a method of image analysis that involves grouping pixels into distinct objects or features based on their characteristics, such as shape, size, and texture, with the goal of identifying and mapping specific features or land covers within an image. The process typically involves segmentation, feature extraction, classification, and post-classification steps.

Comments

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

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

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

Vineesh V, Geography

Search This Blog