UNIT 1: CORE CONCEPTS OF REMOTE SENSING & GIS
I. FUNDAMENTALS OF REMOTE SENSING
A. Electromagnetic Spectrum & Spectral Reflectance
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Electromagnetic (EM) Spectrum: Range of EM radiation from gamma rays to radio waves. Remote sensing primarily uses visible, infrared (IR), and microwave regions.
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Spectral Reflectance (ρ): Ratio of reflected radiation to incident radiation on a surface. Varies with wavelength, creating a unique spectral signature for each material.
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Typical Spectral Reflectance Curves:
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Soil: Generally low, increasing with wavelength. Influenced by moisture, texture, organic matter, and iron oxide content.
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Vegetation: Low in blue/red (chlorophyll absorption), high in green (peak), very high in near-infrared (NIR) due to cell structure. Red-edge transition is critical.
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Water: Very low in NIR and SWIR (strong absorption). Increases slightly in blue/green but decreases with turbidity/depth.
[!TIP] Exam Focus: Be ready to sketch generalized curves for all three on the same graph, labeling key absorption/reflection features (e.g., red edge for vegetation).
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| Factor | Influence on Spectral Response |
|---|---|
| Material Composition | Chemical makeup determines absorption features (e.g., water absorption bands). |
| Surface Roughness | Affects bidirectional reflectance; rough surfaces scatter more. |
| Atmospheric Conditions | Scattering (Rayleigh, Mie) and absorption (water vapor, CO₂) alter signal. |
| Sun-Sensor Geometry | Illumination and viewing angles change reflectance (anisotropy). |
| Temporal Factors | Phenology (vegetation stage), moisture content, tidal state (water). |
B. Ideal Remote Sensing System
A conceptual system for efficient data acquisition and information extraction. Functional Components:
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Energy Source: Sun (passive) or onboard transmitter (active).
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Atmosphere-Earth Surface Interaction: Radiation modifies via absorption, scattering.
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Sensor: Detects and records reflected/emitted EM energy.
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Data Processing & Correction: Radiometric & geometric correction to generate usable imagery.
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Information Extraction & Analysis: Visual/digital interpretation to derive information.
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Application: Utilized for specific user needs (e.g., mapping, monitoring).
[!TIP] Common Pitfall: Students often forget the atmosphere as an active component modifying the signal before it reaches the sensor.
C. Sensor Resolutions
Four fundamental resolutions define a sensor's capability. Trade-offs exist; improving one often degrades another.
| Resolution Type | Definition | Significance | Example Trade-off |
|---|---|---|---|
| Spatial | Minimum separable distance on ground (pixel size). | Determines detail level, smallest identifiable object. | Higher spatial resolution → smaller swath width, lower temporal resolution. |
| Spectral | Number and width of EM wavelength bands. | Enables material discrimination (e.g., vegetation vs. soil). | More spectral bands (hyperspectral) → lower spatial resolution or data volume. |
| Temporal | Revisit time (time between successive observations of same area). | Critical for monitoring dynamic phenomena (floods, crops). | Higher temporal resolution (frequent revisit) → often lower spatial resolution (wide swath). |
| Radiometric | Number of brightness levels (bit depth) sensor can distinguish. | Affects ability to detect subtle differences in reflectance. | Higher radiometric resolution (e.g., 12-bit) → larger data volume, requires more storage. |
[!TIP] Exam Tip: Remember "SpaTial" for Spatial, Temporal. "SpecTral" for Spectral. "RadiomeTric" for Radiometric.
II. REMOTE SENSING PLATFORMS & SENSORS
A. Satellite Orbits & Characteristics
| Feature | Geostationary Orbit (GEO) | Sun-Synchronous Orbit (SSO) |
|---|---|---|
| Altitude | ~36,000 km | ~700-800 km (LEO) |
| Orbit Period | 24 hours (matches Earth's rotation) | ~90-100 minutes |
| Inclination | 0° (equatorial) | ~98° (polar) |
| Swath | Very wide (~⅓ Earth) | Narrow (10-300 km) |
| Key Advantage | Continuous viewing of same area (weather monitoring). | Constant solar illumination (same sun angle) for consistent image comparison. |
| Key Disadvantage | Very low spatial resolution. | Revisit time depends on latitude & swath; may need multiple satellites for high frequency. |
| Synoptivity | High (large area at once). | Low (narrow swath). |
| Repetivity | Continuous (high temporal). | Moderate (depends on constellation). |
Synoptivity: Ability to image a large area in a single acquisition.
Repetivity: Frequency of revisiting the same area.
B. Indian Satellite Programs (IRS & Chandrayaan-3)
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IRS (Indian Remote Sensing) Series:
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Objectives: Resource management (agriculture, forestry, water), environment monitoring, urban planning, disaster management.
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Features: Variety of sensors (LISS, AWiFS, WiFS, HySIS). Sun-synchronous orbits. Progressive improvement in spatial (from 72m to <5m), spectral, and temporal resolutions.
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Chandrayaan-3 (Lunar Mission):
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Objectives: Safe and soft landing on Moon's south polar region, rover operations, in-situ scientific experiments.
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Salient Features: Lander (Vikram), Rover (Pragyan), propulsion module. First mission to land near lunar south pole. Studied lunar surface composition, exosphere.
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C. Earth Observation Satellites
| Category | Examples | Primary Use | Key Characteristics |
|---|---|---|---|
| Earth Resource | Landsat (US), Sentinel-2 (EU) | Land cover, agriculture, forestry, geology. | Multispectral (4-13 bands), moderate resolution (10-30m), free data, long historical archive (Landsat). |
| Weather/ Meteorological | INSAT (India), NOAA/GOES (US) | Weather forecasting, cyclone tracking, sea surface temperature. | Geostationary (INSAT, GOES) or polar-orbiting (NOAA). Broad spectral coverage (visible, IR, water vapor). High temporal resolution (15-30 min). |
III. IMAGE INTERPRETATION & CLASSIFICATION
A. Visual Interpretation
Elements of Interpretation:
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Tone/Color: Relative brightness/color in B&W or color composites.
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Texture: Roughness/smoothness (e.g., forest = coarse, water = smooth).
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Shape: Geometric form (e.g., buildings = rectangular, rivers = sinuous).
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Size: Relative/absolute dimensions.
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Pattern: Spatial arrangement (e.g., orchards = regular, natural forest = irregular).
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Association: Relationship with other features (e.g., airport with runways, terminals, roads). Tools:
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Stereoscope: For 3D viewing from stereo pairs (parallax for height/depth).
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Color Composites: e.g., False Color Composite (FCC) using NIR, Red, Green bands (NIR=Red, Red=Green, Green=Blue). Vegetation appears red, water dark blue/black.
B. Digital Image Analysis
| Aspect | Visual Interpretation | Digital Image Analysis |
|---|---|---|
| Basis | Human eye-brain pattern recognition. | Computer algorithms & statistical analysis. |
| Data | Hardcopy prints or screen display. | Digital pixel values (DN). |
| Speed | Slow, subjective, expert-dependent. | Fast, objective, repeatable. |
| Output | Thematic maps, qualitative. | Quantitative results, classified raster/vector. |
| Image Filtering | Not applicable. | Spatial Domain Filters: <br>• Smoothing (Low-pass): Reduces noise (e.g., mean filter). <br>• Edge Enhancement (High-pass): Sharpens boundaries (e.g., Laplacian, Sobel). |
C. Classification Methods
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Supervised Classification:
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Process: User selects training samples (representative areas of known land cover). Algorithm (e.g., Maximum Likelihood) learns spectral signature and classifies entire image.
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Steps: 1. Define classes, 2. Collect training data, 3. Train classifier, 4. Classify image, 5. Evaluate accuracy (confusion matrix).
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Use: When prior knowledge of classes exists.
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Unsupervised Classification (Clustering):
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Process: Algorithm (e.g., ISODATA, K-means) groups pixels into clusters based on spectral similarity without training data. User then interprets/clusters into information classes.
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Steps: 1. Specify number of clusters, 2. Run clustering, 3. Analyze cluster properties, 4. Merge/assign to meaningful classes.
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Use: Exploratory analysis, unknown area, generating spectral classes.
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[!TIP] Key Difference: Supervised uses training data to define classes; Unsupervised lets the data define clusters.
IV. GIS FUNDAMENTALS
A. Definition, Objectives & Components
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Definition: GIS is a computer-based system for capturing, storing, managing, analyzing, and displaying geographically referenced data.
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Objectives: Support decision-making for spatial problems, integrate diverse data, automate mapping, perform spatial analysis, model scenarios.
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Five Core Components:
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Hardware: Computer, storage, GPS, plotters.
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Software: GIS application (ArcGIS, QGIS), DBMS, tools.
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Data: Spatial data (features with location) + Attribute data (descriptive info). Most critical and expensive component.
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People: skilled users, managers, decision-makers.
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Procedures: Workflow, data standards, quality control.
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B. Data Sources & Collection Objectives
| Data Type | Sources | Collection Objective in GIS |
|---|---|---|
| Primary Data | Field survey, GPS, ground truthing, digitizing from maps. | Create new, accurate spatial datasets for specific project needs. |
| Secondary Data | Existing maps, aerial photos, satellite imagery, census data, government databases. | Leverage existing, often cheaper/free data to build GIS quickly. |
Primary Objective of Data Collection: To obtain accurate, relevant, and current spatial and attribute data that meets the specific requirements of the GIS application.
C. Spatial & Attribute Data Integration
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Integration Mechanism: Each spatial feature (point, line, polygon) is assigned a unique identifier (Feature ID or Primary Key).
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Linkage: The attribute table contains a Foreign Key (same as Feature ID) that links each record to its corresponding spatial feature.
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Relational Database Management System (RDBMS): Manages attribute tables. Allows queries like "Show all wells (spatial) where yield > 100 L/min (attribute)" by joining tables on the common key.
[!TIP] Conceptual Link: Spatial Data answers "WHERE?" and "WHAT SHAPE?". Attribute Data answers "WHAT?", "WHEN?", "HOW MUCH?".
V. GIS DATA MODELS & STRUCTURES
A. Vector vs. Raster Data Structures (Detailed Comparison)
| Feature | Vector Data Model | Raster Data Model |
|---|---|---|
| Basic Unit | Points, Lines, Polygons (defined by coordinates). | Grid cells (pixels) with a value. |
| Topology | Explicitly stored (connectivity, adjacency). Essential for network analysis. | Implied by cell arrangement. No inherent topology. |
| Storage | Compact for discrete features; storage depends on vertex count. | Large for high-resolution data; storage = rows × cols × bits/pixel. |
| Scale Dependence | Scale-dependent. Data must be generalized for smaller scales. | Scale-independent in theory (but resolution fixed). |
| Analysis Suitability | Best for: Network analysis (roads), boundary operations (overlay), precise measurements. | Best for: Surface analysis (slope, aspect), cell-based modeling (suitability), image processing. |
| Data Capture | Digitizing (tablet, on-screen), GPS points, coordinates from surveys. | Scanning, direct from sensors, rasterization of vectors. |
| Visual Quality | Smooth, sharp edges at any scale (theoretically). | Blocky/pixelated when zoomed in; resolution-limited. |
B. Data Models in GIS
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Feature-Based (Vector) Model: Represents real-world entities as discrete objects with geometry (coordinates) and attributes.
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Grid-Based (Raster) Model: Represents continuous surfaces or phenomena as a matrix of cells, each with a value representing a property (e.g., elevation, land cover).
C. Data Conversion in GIS
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Vector-to-Raster (Rasterization): Convert vector features to grid cells.
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Method: For each cell, determine which feature it falls within (point-in-polygon). Assign cell value from feature's attribute.
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Use: Preparing vector data for raster-based analysis (e.g., suitability modeling).
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Raster-to-Vector (Vectorization): Convert raster grid to vector features.
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Method: Edge detection to find boundaries, then line following to create arcs, polygonization to close loops.
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Use: Creating editable vector maps from scanned images or classified imagery.
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D. Shapefile Creation Procedure
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Digitization:
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Manual: Using a digitizing tablet to trace features from a hardcopy map.
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On-Screen (Heads-up): Tracing features directly from a georeferenced raster image (e.g., satellite image, scanned map) in GIS software.
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Attribute Assignment: During/after digitization, populate the attribute table. Each feature gets a unique ID. Add descriptive fields (e.g.,
Road_Name,LandUse_Type). -
Topology Building (Optional but Recommended): Define rules (e.g., no dangles, no overlaps) and build topology to ensure data integrity for network or polygon analysis. Creates topological relationships (arcs, nodes, polygons).
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Saving as Shapefile: The final vector layer is saved as a
.shp(geometry),.shx(index),.dbf(attributes), and.prj(projection) file set.
VI. SPATIAL REFERENCE & ANALYSIS
A. Coordinate Systems
| System | Description | Units | Use Case |
|---|---|---|---|
| Geographic | Latitude/Longitude based on a spheroid/ellipsoid (e.g., WGS84). | Degrees (°) | Global datasets, raw GPS data. |
| Projected | Mathematical projection of Earth's curved surface onto a flat plane. | Meters/Feet (linear) | GIS analysis, mapping, measurement. Minimizes distortion for a region. |
| Common Projected Systems | UTM (Universal Transverse Mercator), State Plane Coordinate System (US), national grids. |
B. Map Projections
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Importance: Earth is 3D, maps are 2D. All projections introduce distortion in shape, area, distance, or direction. Choosing a projection depends on the map's purpose (e.g., conformal for navigation, equal-area for thematic maps).
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UTM Projection:
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System: Global system of 60 zones (6° wide, numbered 1-60 from 180°W).
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Characteristics: Transverse Mercator projection. Conformal (preserves shape locally). Scale factor of 0.9996 at central meridian to minimize distortion. Each zone has its own central meridian and false easting/northing (in meters) to avoid negative coordinates.
[!TIP] UTM Zone Calculation: Zone number =
floor((Longitude + 180) / 6) + 1. For India (68°E to 97°E), Zones 43 to 47. -
C. Spatial Analysis Techniques
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Buffer Analysis:
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Concept: Create a zone of specified distance around a feature (point, line, polygon).
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Applications: Riparian buffer (100m from river), noise pollution zone (500m from highway), service area of a hospital (5km drive time).
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Overlay Analysis:
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Concept: Combine two or more thematic layers to identify relationships. Operates on overlapping polygons.
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Types:
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Intersection: Output retains only the area where all input layers overlap. Features get attributes from all layers. (Most common).
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Union: Output retains all areas from all input layers. Features get attributes from the layer they came from.
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Identity: Like intersection, but retains all features from the identity layer (first input), with attributes from the second layer where they overlap.
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[!TIP] Mnemonic: Intersection = In common. Union = Unites everything.
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D. Errors in GIS
| Error Type | Cause | Examples | Mitigation |
|---|---|---|---|
| Systematic (Deterministic) | Predictable, consistent bias. | Incorrect projection parameters, sensor calibration drift, digitizing tablet scale error. | Calibration, use accurate control points, apply correction models. |
| Non-Systematic (Random) | Unpredictable, variable. | Operator error during digitizing, atmospheric noise in RS data, inconsistent attribute entry. | Quality control (QC) checks, training, data validation rules, multiple measurements. |
[!TIP] Key Difference: Systematic error has a pattern (can be corrected); non-systematic is random (reduced by better procedures).
VII. APPLICATIONS & INTEGRATION CHALLENGES
A. Land Use/Land Cover (LULC) Change Assessment (Integrated RS-GIS Workflow)
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Data Acquisition: Obtain multi-temporal satellite images (e.g., Landsat 2000, 2020) for the study area.
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Pre-processing: Perform atmospheric correction and geometric correction/orthorectification (using DEM) to align images perfectly.
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Image Classification: Apply supervised or unsupervised classification separately for each date to generate LULC maps (e.g., classes: agriculture, urban, forest, water).
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Post-classification Processing: Clean classified maps (remove speckle, generalize).
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GIS Overlay & Change Detection: In GIS, perform overlay analysis (intersection) of the two classified raster/vector layers. Create a change matrix (cross-tabulation) to quantify gains/losses for each class.
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Analysis & Mapping: Identify change hotspots, calculate rates of change, map conversion types (e.g., forest → agriculture).
B. Water Resources Applications
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Watershed Delineation: Use Digital Elevation Model (DEM) from RS (e.g., SRTM, ASTER) in GIS to derive flow direction, accumulation, and automatically delineate watershed boundaries and stream networks.
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Groundwater Mapping: Identify potential recharge zones (lineaments, fractures from satellite imagery), map aquifer extent (using geophysical data integrated in GIS), and model groundwater flow.
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Flood Assessment & Management:
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Inundation Mapping: Use SAR (Sentinel-1) or optical imagery during flood to map extent.
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Risk Zoning: Combine flood hazard maps (from hydraulic models) with exposure data (population, infrastructure) in GIS.
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Floodplain Delineation: Use DEM and hydraulic models in GIS.
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C. Traffic Management Applications
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Route Optimization: GIS network analysis (shortest path, vehicle routing problem) for emergency services, delivery fleets.
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Congestion Monitoring: Use high-temporal resolution RS (e.g., from traffic cameras, or SAR for large-scale flow) to estimate traffic density/speed. Integrate with GIS to visualize congestion hotspots.
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Infrastructure Planning: Optimal location for new roads, intersections, or public transport hubs using suitability modeling (overlay of slope, land use, existing network).
D. Problems in Using Remote Sensing Data in GIS
| Problem | Description | Consequence | Mitigation |
|---|---|---|---|
| Resolution Mismatch | RS data spatial resolution differs from other GIS layers (e.g., 30m RS vs. 1:1000 scale cadastral map). | Inaccurate overlay, loss of detail, aggregation issues. | Resample data to common resolution (but beware of information loss). Use appropriate scale for analysis. |
| Format Compatibility | RS data often in specific formats (e.g., GeoTIFF, HDF) with complex metadata; GIS may use shapefiles, geodatabases. | Data import errors, loss of band information, projection issues. | Use GIS software's raster support, convert formats carefully, preserve metadata (especially projection/georeferencing). |
| Geometric Errors | Systematic: Sensor optics, Earth curvature. Random: Platform instability. | Misregistration with other layers, positional inaccuracy. | Orthorectification using accurate Ground Control Points (GCPs) and DEM. Always check RMSE (Root Mean Square Error). |
| Radiometric/Atmospheric | Atmospheric scattering/absorption not corrected. | Incorrect pixel values, poor classification accuracy. | Perform atmospheric correction (e.g., Dark Object Subtraction, DOS, or using atmospheric models). |
[!TIP] Golden Rule: "Garbage In, Garbage Out (GIGO)." The quality of GIS analysis is fundamentally limited by the quality and compatibility of the input RS data. Always pre-process and validate RS data before integration.