A. FUNDAMENTALS OF REMOTE SENSING (RS)
Spectral Properties & Reflectance
- Spectral Reflectance ($\rho$) is the ratio of reflected radiance to incident radiance at a specific wavelength:
$$\rho(\lambda) = \frac{L_{\text{reflected}}(\lambda)}{L_{\text{incident}}(\lambda)}$$
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Spectral Reflectance Curves: Plot of $\rho$ vs. wavelength (400–2500 nm) for different surface features.
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Vegetation: Low in visible (blue/red absorption by chlorophyll), high peak in NIR (cell structure), moderate in SWIR (water content).
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Water: Low overall; strong absorption in NIR and SWIR; appears dark.
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Soil: Generally increases with wavelength; varies with moisture, texture, and mineral composition.
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[!TIP] Vegetation’s high NIR reflectance is key for NDVI calculation. Water absorbs strongly beyond 700 nm, enabling water body discrimination.
Remote Sensing System & Components
An ideal remote sensing system comprises:
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Energy Source (Sun or active sensor)
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Atmosphere Interaction (scattering, absorption)
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Target Interaction (reflection, emission)
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Sensor Detection (captures reflected/emitted energy)
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Data Recording & Processing (creates usable imagery)
Sensor Resolution
Resolution defines the ability to distinguish details. Four critical types:
| Type | Definition | Example |
|---|---|---|
| Spatial | Ground area represented by a pixel | 30 m (Landsat), 0.5 m (high-res) |
| Spectral | Number and width of wavelength bands | Multispectral (4–10 bands), Hyperspectral (>200 bands) |
| Radiometric | Number of brightness levels (bit depth) | 8-bit (256 levels), 11-bit (2048 levels) |
| Temporal | Revisit frequency over same area | Daily (MODIS), 16-day (Landsat) |
[!TIP] Higher spatial resolution ≠ better classification; trade-offs exist with spectral and radiometric resolution.
Satellite Platforms & Orbits
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Geostationary Satellite: Orbits at ~36,000 km, matches Earth’s rotation → fixed position over equator. High repetivity (continuous monitoring), low spatial resolution. Used for weather (e.g., INSAT, GOES).
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Sun-synchronous Satellite: Polar orbit, passes same latitude at same local solar time. High synoptivity (consistent lighting), moderate repetivity (days to weeks). Used for Earth observation (e.g., IRS, Landsat).
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Synoptivity: Ability to capture wide-area, simultaneous snapshots.
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Repetivity: Frequency of revisiting the same area.
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Indian Satellite Program:
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IRS Series: Earth observation (Resourcesat, LISS, AWiFS).
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INSAT Series: Meteorological and communication.
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Chandrayaan-3: Lunar mission (2023) – objectives: soft landing, rover operations, lunar surface studies; features: indigenous lander (Vikram), rover (Pragyan), scientific payloads for elemental analysis.
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[!TIP] Sun-synchronous orbits ensure consistent illumination for change detection; geostationary ideal for real-time weather tracking.
B. IMAGE ACQUISITION & PROCESSING
Image Interpretation & Analysis
Elements of Visual Interpretation:
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Tone (brightness/color)
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Texture (roughness/smoothness)
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Shape (geometric form)
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Size (relative dimension)
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Pattern (spatial arrangement)
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Association (relationship with other features)
Differentiation:
| Aspect | Visual Image Analysis | Digital Image Analysis |
|---|---|---|
| Input | Hardcopy/on-screen display | Digital pixel values |
| Process | Human interpretation (eyes/brain) | Algorithmic processing (software) |
| Output | Thematic maps, annotations | Classified images, quantitative data |
| Speed | Slow, subjective | Fast, repeatable |
Image Classification
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Supervised Classification:
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Define training sites (regions of known land cover).
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Extract spectral signatures from training data.
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Classify entire image using signatures (e.g., Maximum Likelihood, SVM).
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Unsupervised Classification:
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Algorithm clusters pixels into spectrally similar groups (e.g., ISODATA, K-means).
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Analyst assigns land cover labels to clusters.
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Key Difference: Supervised uses prior knowledge; unsupervised discovers natural groupings.
[!TIP] Supervised requires accurate training data; unsupervised may produce statistically optimal but thematically ambiguous clusters.
Pre-processing & Enhancement
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Image Filtering:
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Low-pass (Smoothing): Reduces noise, blurs edges (e.g., mean filter).
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High-pass (Sharpening): Enhances edges, details (e.g., Laplacian, Sobel).
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Band-pass: Isolates specific frequency features.
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Errors in RS Data:
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Systematic: Predictable, correctable (sensor calibration, orbital drift).
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Non-systematic: Random, unpredictable (atmospheric haze, cloud cover).
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Corrections:
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Radiometric: Corrects for sensor noise, atmospheric effects, illumination.
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Geometric: Corrects for Earth curvature, platform motion, terrain displacement (using GCPs and polynomial transformation).
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C. GEOGRAPHIC INFORMATION SYSTEM (GIS) FUNDAMENTALS
Definition & Components
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GIS Definition: A system for capturing, storing, analyzing, managing, and presenting spatial or geographic data.
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Key Components:
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Hardware (computers, GPS, scanners)
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Software (ArcGIS, QGIS, GRASS)
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Data (spatial and attribute)
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People (users, managers)
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Methods/Procedures (data collection, analysis workflows)
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GIS Data: Sources & Objectives
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Sources:
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Primary: Field surveys, GPS, digitization.
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Secondary: Maps, satellite imagery, census data, existing databases.
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Objectives of Data Collection:
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Support specific analysis (e.g., site suitability, network analysis).
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Ensure accuracy, completeness, and relevance.
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Maintain interoperability and standards.
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Data Models & Structure
| Model | Structure | Elements | Advantages | Disadvantages |
|---|---|---|---|---|
| Vector | Points, lines, polygons | Coordinates + attributes | Precise, compact, topology possible | Complex for continuous data |
| Raster | Grid of pixels | Cell values (digital numbers) | Simple, good for continuous surfaces | Large data volume, less precise |
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Data Conversion:
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Raster to Vector: Vectorization (tracing edges, thinning).
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Vector to Raster: Rasterization (assigning cell values based on feature attributes).
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[!TIP] Vector preferred for discrete features (roads, parcels); raster for continuous surfaces (elevation, temperature).
Spatial & Attribute Data Integration
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Integration: Each spatial feature (point/line/polygon) has a unique key linking to its attribute table (non-spatial data).
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Geodatabase: A database optimized for spatial data, storing:
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Feature classes (spatial data)
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Attribute tables (tabular data)
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Relationships (links between tables)
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Topology (spatial rules)
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D. COORDINATE SYSTEMS & MAP PROJECTIONS
Coordinate Systems
| System | Description | Example |
|---|---|---|
| Geographic | Angular coordinates on sphere/ellipsoid | Latitude/Longitude (WGS84) |
| Projected | Cartesian coordinates on flat surface | UTM, State Plane, Mercator |
Map Projections
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Why Important?: Earth is 3D; maps are 2D → projections introduce distortion in shape, area, distance, direction.
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Types:
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Cylindrical (Mercator): Conformal, distorts area near poles.
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Conic (Albers): Equal-area, good for mid-latitude regions.
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Azimuthal (Stereographic): Preserves shape from a point.
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Universal Transverse Mercator (UTN):
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Key Features:
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60 zones (6° wide), each with central meridian.
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Scale factor at central meridian: \boxed{k_0 = 0.9996} (slightly reduces scale).
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False easting/northing to avoid negative coordinates.
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Conformal (preserves local shape).
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Distortion: No projection is perfect; choice depends on map purpose (e.g., navigation vs. area calculation).
[!TIP] UTM is widely used for large-scale mapping; always check zone and datum (e.g., WGS84 vs. NAD83).
E. GIS DATA INPUT & MANAGEMENT
Data Input Procedures
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Digitization:
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Manual: Heads-up (on-screen) or heads-down (tablet).
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Automated: Scanning + vectorization (edge detection).
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Create Shapefiles:
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Define geometry type (point/line/polygon).
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Set coordinate system.
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Digitize features; attributes entered manually or joined from tables.
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Data Editing: Modify vertices, fix topology errors.
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Topology Building: Define spatial relationships (e.g., no gaps between polygons, connectivity of lines).
Data Quality & Errors
Problems of Using RS Data in GIS:
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Scale Mismatch: RS pixel size vs. map scale.
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Resolution Issues: Mixed pixels, coarse resolution obscuring details.
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Geometric Errors: Residual misregistration after correction.
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Thematic Accuracy: Classification errors (spectral confusion, training site bias).
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Temporal Inconsistency: Multi-temporal images may have different acquisition conditions.
[!TIP] Always assess RS data accuracy before GIS integration; use ground truth data for validation.
F. GIS SPATIAL ANALYSIS OPERATIONS
Query & Measurement
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Attribute Query: Select features based on non-spatial attributes (e.g.,
SELECT * FROM roads WHERE type='Highway'). -
Spatial Query: Select based on location (e.g., features within 1 km of a river).
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Measurement:
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Distance: Euclidean or geodesic (on sphere).
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Area/Perimeter: Calculated from polygon coordinates (planar for projected data).
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Overlay & Neighborhood Analysis
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Overlay Analysis: Combines multiple layers to create new features.
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Union: All features from both layers.
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Intersection: Only overlapping areas.
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Identity: Features of one layer clipped by another, retaining attributes.
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Erase: Removes areas of one layer from another.
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Buffer Analysis: Creates zone of specified distance around features.
- Applications: Riparian buffers, noise zones, service areas.
[!TIP] Overlay in raster uses Boolean logic; in vector uses polygon overlay operations. Buffer distances must use appropriate coordinate system (projected for accurate meters).
Other Operations
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Reclassification: Assigns new values to existing classes (e.g., simplifying land cover categories).
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Surface Analysis:
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Slope: Gradient from DEM (degrees or %).
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Aspect: Direction of slope (0–360°).
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Derived from DEM using neighborhood statistics (e.g., Horn’s method).
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G. INTEGRATION OF RS & GIS & APPLICATIONS
RS-GIS Integration
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Role of RS: Primary source of spatial data (imagery) for GIS.
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Workflow:
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Acquire multi-temporal RS data.
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Pre-process (atmospheric, geometric correction).
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Classify to create thematic maps (e.g., LULC).
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Import classified raster into GIS; convert to vector if needed.
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Integrate with other GIS layers (roads, boundaries) for analysis.
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Perform spatial analysis (overlay, buffer, change detection).
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Land Use/Land Cover (LULC) Change Assessment
Procedure:
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Multi-temporal image acquisition: Same sensor, season, and minimal cloud cover.
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Pre-processing: Co-registration, atmospheric correction.
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Classification: Supervised/unsupervised for each date.
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Change Detection:
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Post-classification comparison: Compare classified maps; generate transition matrix.
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Other: Image differencing, vegetation index trends.
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GIS Integration: Spatially analyze change patterns, calculate areas, identify drivers (proximity to roads, urban sprawl).
Application Domains
Water Resources:
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Watershed Delineation: Use DEM to define drainage networks and boundaries.
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Surface Water Mapping: Identify water bodies from RS (NDWI, thresholding).
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Groundwater Potential: Integrate geology, lineaments, drainage, slope.
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Flood/Drought Assessment: Monitor inundation extent (SAR/optical), vegetation health (VCI).
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Irrigation Management: Crop water requirement mapping, scheduling.
Other Applications:
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Traffic Management: Real-time monitoring, route optimization.
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Urban Planning: Urban sprawl mapping, infrastructure planning.
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Disaster Management: Hazard zonation (landslides, earthquakes), emergency response.
[!TIP] For LULC change, post-classification comparison reduces errors from atmospheric and sensor differences between dates.
H. SPECIFIC TERMS & CONCEPTS (Short Note Topics)
Stereoscope
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Definition: Optical device for viewing overlapping aerial photographs in 3D (stereoscopic vision).
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Use: Photogrammetry for elevation extraction, feature identification, terrain analysis.
Key Point: Requires parallax from overlapping images (typically 60% forward overlap).
Spectral Reflectance Curves
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Graphical representation of reflectance vs. wavelength for Earth surface features.
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Significance: Enables spectral separation of land cover types; basis for band selection and vegetation indices (e.g., NDVI = $$\displaystyle \frac{(NIR - Red)}{(NIR + Red)} $$).
Image Filtering
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Concept: Mathematical operation on pixel neighborhoods to enhance or suppress features.
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Types:
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Low-pass: Smoothing, noise reduction (mean, median).
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High-pass: Edge enhancement (Laplacian, gradient).
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Band-pass: Isolates specific spatial frequencies.
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Application: Pre-processing for classification, feature extraction.
UTM Projection
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Universal Transverse Mercator: Global system of 60 transverse Mercator zones.
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Key Features:
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Scale factor $$\displaystyle k_0 = 0.9996 $$ at central meridian.
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False easting (500,000 m) and northing (equator 0 m for Northern Hemisphere).
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Conformal, minimal distortion within zone.
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Use: Large-scale topographic mapping, GIS data integration.
Buffer Analysis
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Concept: Creates a zone of specified distance around a spatial feature (point, line, polygon).
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Applications: Environmental impact assessment (e.g., buffer around wetlands), service area delineation (e.g., hospitals), corridor planning.
Note: Requires projected coordinate system for accurate distance.
Overlay Analysis
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Concept: Spatial overlay of two or more layers to combine their attributes and geometries.
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Types:
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Vector: Union, intersection, identity, erase.
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Raster: Boolean operations (AND, OR, XOR) on cell values.
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Use: Suitability analysis, change detection, intersection of zones.
Synoptivity and Repetivity
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Synoptivity: Ability to capture a wide, contiguous area in a single acquisition (e.g., satellite swath). Enables regional studies.
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Repetivity: Frequency of revisiting the same area (temporal resolution). Enables monitoring of dynamic processes (e.g., crop growth, floods).
Trade-off: Sun-synchronous orbits offer good synoptivity and consistent lighting; geostationary offer high repetivity but coarse resolution.