Skip to main content

Digital image processing

Digital image processing in remote sensing involves the manipulation of satellite or aerial images to extract useful information about the Earth's surface. Here are the basic steps involved:

1. Image Acquisition: Remote sensing devices, such as satellites and aerial cameras, capture images of the Earth's surface. These images are usually in digital format and consist of pixels, each representing a small portion of the Earth's surface.

2. Preprocessing: This step involves the initial cleaning and enhancement of the raw image data. It includes tasks like radiometric calibration to correct for sensor-related distortions and atmospheric correction to account for the effects of the Earth's atmosphere on the image.

3. Image Enhancement: Enhancement techniques like contrast adjustment, histogram equalization, and filtering are used to improve the visual quality of the image and make important features more discernible.

4. Image Registration: Multiple images from different sources or times may need to be aligned or registered to ensure accurate analysis. This step involves geometric correction to match images to a common coordinate system.

5. Image Transformation: Spatial and spectral transformations may be applied to the image data to enhance specific features or extract relevant information. This can include techniques like image fusion, pan-sharpening, and principal component analysis (PCA).

6. Feature Extraction: This step involves identifying and isolating specific objects or features within the image. Techniques such as edge detection, classification, and object recognition are used to extract information about land cover, vegetation, water bodies, and more.

7. Image Analysis: Once features are extracted, various analytical methods are applied to interpret the data. This can involve measuring land cover changes, monitoring environmental conditions, or identifying patterns and trends.

8. Post-processing: After analysis, additional steps like noise reduction, mosaicking (combining multiple images), and creating thematic maps may be performed to produce final output products.

9. Interpretation and Decision Making: Remote sensing experts interpret the processed images and extract meaningful information for various applications, such as agriculture, forestry, urban planning, disaster management, and environmental monitoring. The results help in informed decision-making.

10. Reporting and Visualization: The final processed data and analysis results are often presented through maps, reports, and visualizations, making it easier for stakeholders to understand and utilize the information.

Digital image processing plays a crucial role in remote sensing by enabling the extraction of valuable insights from satellite and aerial imagery, which can be used for a wide range of scientific, environmental, and practical applications.

Comments

Popular posts from this blog

Geologic and tectonic framework of the Indian shield

  Major Terms and Regions Explained 1. Indian Shield The Indian Shield refers to the ancient, stable core of the Indian Plate made of hard crystalline rocks. It comprises Archean to Proterozoic rocks that have remained tectonically stable over billions of years. Important Geological Features and Regions ▪️ Ch – Chhattisgarh Basin A sedimentary basin part of the Bastar Craton . Contains rocks of Proterozoic age , mainly sedimentary. Important for understanding the evolution of central India. ▪️ CIS – Central Indian Shear Zone A major tectonic shear zone , separating the Bundelkhand and Bastar cratons . It records intense deformation and metamorphism . Acts as a suture zone , marking ancient tectonic collisions. ▪️ GR – Godavari Rift A rift valley formed due to stretching and thinning of the Earth's crust. Associated with sedimentary basins and hydrocarbon resources . ▪️ M – Madras Block An Archean crustal block in...

Geology and Tectonic. Indian Shield

1. Ch (Chattisgarh Basin): Chattisgarh Basin is a geological region in central India known for its sedimentary rock formations. It's important for its mineral resources, including coal and iron ore. 2. CIS (Central Indian Shear Zone): CIS is a tectonic boundary in central India where the Indian Plate interacts with the Eurasian Plate. It's characterized by significant faulting and seismic activity. 3. GR (Godavari Rift): The Godavari Rift is a geological feature associated with the rifting and splitting of the Indian Plate. It's located in the Godavari River basin in southeastern India. 4. M (Madras Block): The Madras Block is a stable continental block in southern India. It's part of the Indian Plate and is not associated with active tectonic processes. 5. Mk (Malanjkhand): Malanjkhand is known for its copper deposits and is one of the largest copper mines in India. 6. MR (Mahanadi Rift): The Mahanadi Rift is a geological feature related to the rifting of the Indian Pl...

Evaluation and Characteristics of Himalayas

Time Period Event / Process Geological Evidence Key Terms & Concepts Late Precambrian – Palaeozoic (>541 Ma – ~250 Ma) India part of Gondwana , north bordered by Cimmerian Superterranes, separated from Eurasia by Paleo-Tethys Ocean . Pan-African granitic intrusions (~500 Ma), unconformity between Ordovician conglomerates & Cambrian sediments. Gondwana, Paleo-Tethys Ocean, Pan-African orogeny, unconformity, granitic intrusions, Cimmerian Superterranes. Early Carboniferous – Early Permian (~359 – 272 Ma) Rifting between India & Cimmerian Superterranes → Neotethys Ocean formation. Rift-related sediments, passive margin sequences. Rifting, Neotethys Ocean, passive continental margin. Norian (210 Ma) – Callovian (160–155 Ma) Gondwana split into East & West; India part of East Gondwana with Australia & Antarctica. Rift basins, oceanic crust formation. Continental breakup, East Gondwana, West Gondwana, oceanic crust. Early Cretaceous (130–125 Ma) India broke fr...

Seismicity and Earthquakes, Isostasy and Gravity

1. Seismicity and Earthquakes in the Indian Subcontinent Key Concept: Seismicity Definition : The occurrence, frequency, and magnitude of earthquakes in a region. In India, seismicity is high due to active tectonic processes . Plate Tectonics 🌏 Indian Plate : Moves northward at about 5 cm/year. Collision with Eurasian Plate : Causes intense crustal deformation , mountain building (Himalayas), and earthquakes. This is an example of a continental-continental collision zone . Seismic Zones of India Classified into Zone II, III, IV, V (Bureau of Indian Standards, BIS). Zone V = highest hazard (e.g., Himalayas, Northeast India). Zone II = lowest hazard (e.g., parts of peninsular India). Earthquake Hazards ⚠️ Himalayas: prone to large shallow-focus earthquakes due to active thrust faulting. Northeast India: complex subduction and strike-slip faults . Examples: 1897 Shillong Earthquake (Magnitude ~8.1) 1950 Assam–Tib...

Vector geoprocessing - Clipping, Erase, identify, Union & Intersection

Think of your vector data (points, lines, polygons) like shapes drawn on a transparent sheet. Geoprocessing is just cutting, joining, or comparing those shapes to get new shapes or information. 1. Clipping ✂️ Imagine you have a big map and you only want to keep a part of it (like cutting a photo into a smaller rectangle). You use another shape (like the boundary of a district) to "clip" and keep only what is inside. Result: Only the data inside the clipping shape remains. 2. Erase 🚫 Opposite of clipping. You remove (erase) the area of one shape from another shape. Example: You have a city map and want to remove all the park areas from it. 3. Identify 🔍 This checks which features from one layer fall inside (or touch) another layer. Example: Identify all the schools inside a flood zone. 4. Union 🤝 Combines two shapes together and keeps everything from both. Works like stacking two transparent sheets and redrawing t...