LESSON 12.2 — Remote Sensing and GIS
A. Standard Map
| Topic | Governing Source / Method | Exam Focus |
|---|---|---|
| Active vs passive remote sensing | CCRS “Fundamentals of Remote Sensing”; ISRO NRSC training module | Energy source; cloud penetration; sensor type; day/night operation |
| EM spectrum bands and planning use | Standard RS theory; ISRO NRSC | Band → surface property → planning application linkage |
| Four resolution types | ISRO NRSC; Jensen “Remote Sensing of the Environment” | Resolution trade-off; sensor selection by task |
| Satellite platforms (ISRO, international) | ISRO satellite catalogue; ESA; DigitalGlobe/Maxar | Spatial resolution match to planning task; orbit type |
| GIS data models (raster vs vector) | Longley, Goodchild et al.; ESRI GIS Dictionary; ISRO NRSC | Raster for continuous phenomena; vector for discrete features; pixel = smallest raster unit (GATE 2021) |
| GIS operations | Standard GIS analysis framework | Buffer, overlay, network, suitability — operation-to-task match |
| LiDAR and terrain models | ISRO NRSC; standard RS literature | Active sensor; point cloud → DEM/DSM workflow; nDSM = building height |
| Planning applications of RS/GIS | URDPFI 2015 (5-phase framework) | Phase → RS/GIS tool linkage; change detection; sprawl; suitability |
B. Mechanism in Words
- Define the spatial question — identify whether the planning task requires (a) synoptic area coverage of a continuously varying phenomenon (RS is primary), (b) spatially precise discrete feature mapping (vector GIS with field survey), or (c) 3D urban form data (LiDAR); most plans require all three in combination.
- Select sensor and platform — match spatial resolution to minimum mapping unit (building = <1m; ward land use = 5–10m; regional = 30m+); match temporal resolution to rate of change; verify orbit type provides required revisit and illumination consistency.
- Acquire and preprocess imagery — apply radiometric correction (convert digital numbers to reflectance values), geometric correction (orthorectification using DEM), and atmospheric correction (remove scattering/absorption effects) before analysis.
- Classify and extract information — apply supervised or unsupervised classification to assign every pixel to a land cover category; validate accuracy against field samples (minimum 80% overall accuracy for planning-grade LULC maps); compute spectral indices (NDVI for vegetation, NDBI for built-up).
- Build the GIS database — import classified RS outputs as raster layers; digitise or import vector features (roads, boundaries, parcels); georeference all layers to a common coordinate system; link attribute tables.
- Run spatial analysis — execute task-specific GIS operations: buffer zones for proximity analysis, overlay for constraint mapping, network analysis for accessibility, weighted overlay for suitability scoring.
- Validate and integrate into plan — cross-check GIS outputs against field surveys and secondary data; present results as thematic maps aligned with URDPFI 2015 planning phases; document metadata for reproducibility.
C. Core Concept Explanations
C1. Remote Sensing Basics — Passive vs Active; EM Spectrum; Resolution Types
Active vs Passive Sensing
| Basis | Active Remote Sensing | Passive Remote Sensing |
|---|---|---|
| Energy source | Sensor emits its own radiation; measures the return signal | Depends on solar energy reflected from the surface |
| Operating conditions | Day and night; independent of illumination | Requires daylight for optical bands; thermal IR can operate at night |
| Weather penetration | Microwave wavelengths (SAR) penetrate cloud, rain, and haze; operates during monsoon | Optical bands blocked by cloud cover; thermal partially weather-sensitive |
| Typical sensors | SAR (Synthetic Aperture Radar), LiDAR, RADAR altimeter | Multispectral scanners (Landsat OLI, IRS LISS), hyperspectral, thermal IR |
| Planning applications | Flood inundation mapping during monsoon (SAR); building height extraction (LiDAR); ground subsidence | Land use / land cover classification; vegetation mapping; urban sprawl tracking; thermal hotspot identification |
| Cost and complexity | High power demand; complex signal processing | Simpler hardware; lower cost; open data widely available |
Exam anchor: For flood mapping in Indian cities during monsoon, SAR (active) is the only viable option — cloud cover blocks optical sensors precisely when flood data is most needed. This is why ISRO developed the RISAT (Radar Imaging Satellite) programme.
Electromagnetic Spectrum — Key Bands for Planning
| Band | Wavelength Range | Sensor Type | Planning Application |
|---|---|---|---|
| Visible Blue (B) | 0.45–0.52 µm | Passive optical | Water body delineation; atmospheric scattering correction |
| Visible Green (G) | 0.52–0.60 µm | Passive optical | Vegetation vigour; water turbidity |
| Visible Red (R) | 0.63–0.69 µm | Passive optical | Vegetation stress; soil exposure; land cover classification |
| Near-Infrared (NIR) | 0.76–0.90 µm | Passive optical | Vegetation mapping (strong plant reflectance); NDVI calculation |
| Short-Wave Infrared (SWIR) | 1.55–2.35 µm | Passive optical | Soil moisture; geological mapping; burn scar detection |
| Thermal Infrared (TIR) | 8–14 µm | Passive thermal | Urban heat island mapping; land surface temperature; industrial effluent |
| Microwave (SAR) | 1 cm–1 m | Active (SAR) | Flood mapping; subsidence; crop monitoring through cloud |
| LiDAR (laser) | 0.9–1.55 µm (NIR laser) | Active (ranging) | 3D point cloud; building heights; canopy structure; DEM/DSM |
NDVI (Normalised Difference Vegetation Index):
NDVI = (NIR − Red) / (NIR + Red)
Range: −1 to +1. NDVI > 0.3 = healthy vegetation; NDVI < 0.1 = bare soil or built-up. Used to detect loss of green cover and urban expansion into agricultural land.
Four Resolution Parameters
| Resolution Type | What It Measures | Trade-off | Planning Implication |
|---|---|---|---|
| Spatial | Ground area per pixel (GSD) | High spatial → narrow swath, fewer bands | Building extraction: <1m; ward LULC: 5–10m; regional: 30m+ |
| Spectral | Number and width of wavelength bands | More bands → more data volume, lower temporal frequency | LULC classification: 4–7 bands sufficient; mineral mapping: hyperspectral (100+ bands) |
| Radiometric | Bit depth (grey levels per pixel) | Higher bit depth → larger file size | Dense urban shadow detail: 12-bit+ (4,096 levels); 8-bit (256 levels) adequate for general LULC |
| Temporal | Revisit interval | High temporal → low spatial (geostationary) OR limited coverage (LEO) | Disaster monitoring: hours–days; crop calendar: monthly; urban sprawl: annual multi-temporal |
Resolution trade-off principle: No single sensor excels on all four parameters simultaneously. High spatial resolution narrows swath width and reduces spectral bands. High spectral resolution demands longer dwell time, reducing temporal frequency. Multi-sensor integration is the operational standard.
Source: ISRO NRSC, “Remote Sensing Applications for Urban Planning”; CCRS “Fundamentals of Remote Sensing.”
C2. Satellite Platforms — ISRO, Landsat, SPOT, IKONOS, WorldView
Indian Platforms (ISRO)
| Satellite / Sensor | Spatial Resolution | Spectral Bands | Orbit | Primary Planning Use |
|---|---|---|---|---|
| Cartosat-3 (2019–) | 0.25m Pan; 1.12m MS | Pan + 4 MS | SSO | Building footprint extraction; cadastral mapping; urban FAR audit |
| Cartosat-2 series | 0.6m Pan; 2m MS | Pan + 4 MS | SSO | City-level base map; road network delineation; construction monitoring |
| ResourceSat-2 LISS-IV | 5.8m | 3 bands (G, R, NIR) | SSO | Ward-level land use; agricultural plot mapping; peri-urban monitoring |
| ResourceSat-2 LISS-III | 23.5m | 4 bands (G, R, NIR, SWIR) | SSO | District/regional LULC; vegetation assessment; watershed mapping |
| ResourceSat-2 AWiFS | 56m | 4 bands | SSO | State/national agricultural monitoring; seasonal crop area estimation |
| RISAT-2 / RISAT-1 | 3–50m (SAR) | C-band / X-band SAR | SSO | Monsoon flood mapping; crop damage assessment; coast monitoring |
| INSAT-3D / INSAT-3DR | ~4 km | 6 channels (VIS, IR, WV) | GEO (~36,000 km) | Cyclone tracking; weather monitoring; disaster early warning |
International Platforms
| Satellite / Sensor | Country/Agency | Spatial Resolution | Spectral Bands | Revisit | Primary Planning Use |
|---|---|---|---|---|---|
| Landsat 8/9 OLI | USA (USGS/NASA) | 30m MS; 15m Pan | 9 bands (Blue–SWIR + TIRS) | 16 days | Long-term LULC change detection (archive from 1972); free data; global benchmark |
| Sentinel-2A/B | ESA (EU) | 10m / 20m / 60m | 13 bands (VNIR + SWIR) | 5 days (combined A+B) | Urban growth monitoring; agricultural mapping; open access; replacing Landsat in many planning workflows |
| SPOT 6/7 | Airbus (France) | 1.5m Pan; 6m MS | 4 bands (B, G, R, NIR) | 1–3 days | City-level base maps; corridor planning; post-disaster assessment |
| IKONOS | DigitalGlobe (USA) | 1m Pan; 4m MS | 4 bands | 1–3 days | First commercial 1m satellite (1999); decommissioned 2015; replaced by WorldView series |
| WorldView-3 | Maxar (USA) | 0.31m Pan; 1.24m MS | 8 bands (coastal–SWIR) | <1 day | Highest commercial spatial resolution; building-level planning; infrastructure inventory |
Orbit distinction recap:
– SSO (Sun-Synchronous, 700–800 km): Same local solar time on every pass — consistent illumination for multi-temporal change detection. Cartosat, Landsat, Sentinel-2. (GATE 2017)
– GEO (~36,000 km): Stationary above equator — continuous monitoring of same region. INSAT, GSAT. (GATE 2023, 1993)
Source: ISRO NRSC training materials; USGS Landsat Science; ESA Copernicus documentation.
C3. GIS Data Models — Raster vs Vector
A GIS represents geographic space using one of two data models. The choice is not aesthetic — it determines what analysis is possible and what accuracy is achievable.
| Basis | Raster Data Model | Vector Data Model |
|---|---|---|
| Representational logic | Regular grid of cells; each cell holds one value | Points (x,y), lines (connected points), polygons (closed lines) |
| Best represents | Continuously varying phenomena: elevation, temperature, satellite imagery | Discrete objects with defined boundaries: roads, parcels, buildings |
| Smallest unit | Cell (pixel) — GATE 2021: “pixel” is the correct answer | Coordinate pair (vertex / node) |
| Overlay operation | Cell-by-cell arithmetic — computationally efficient | Geometric intersection — more complex; produces precise boundaries |
| Topology | Implicit in grid position — difficult to encode explicitly | Explicitly defined: connectivity, adjacency, containment stored in data |
| Storage | Fixed by grid dimensions (rows × columns), regardless of content; can be very large | Stores only feature coordinates + attributes; generally compact |
| Scale sensitivity | Resolution fixed at capture; pixelates beyond native GSD | Coordinates-defined; displayable at any scale |
| Typical GIS layers | DEM, satellite imagery, suitability score grids, interpolated surfaces | Road networks, parcel boundaries, building footprints, administrative boundaries |
GATE 2021 anchor: The smallest unit of a raster image is a pixel (cell). This is a foundational GIS vocabulary question — never answer “node” (vector) or “polygon” (vector feature).
C4. GIS Operations — Buffer, Overlay, Network Analysis, Suitability Analysis
| Operation | Data Model | What It Does | Planning Application |
|---|---|---|---|
| Buffer | Vector (primarily) | Creates a zone of specified distance around a feature (point, line, or polygon) | 500m buffer around industrial zones → identify residential areas at risk; 300m buffer around water bodies → delineate no-development setback zone |
| Clip | Both | Extracts features within a defined boundary polygon | Extract road network within a study area boundary |
| Dissolve | Vector | Merges adjacent polygons sharing the same attribute value | Merge all residential land use parcels into a single residential zone polygon |
| Intersect / Union Overlay | Vector | Intersect: keeps only the area common to both layers; Union: keeps all areas from both layers | Intersect flood zone with residential land use → identify flood-exposed housing; Union two zoning layers → merge permissions |
| Raster Overlay (Map Algebra) | Raster | Cell-by-cell arithmetic combining multiple raster layers using a formula | Weighted suitability: (0.4 × slope score) + (0.3 × proximity to road) + (0.3 × soil stability) |
| Network Analysis | Vector | Computes routes, service areas, and travel times along a connected line network | Shortest route from each ward to nearest hospital; 10-minute service area from a fire station; optimal school bus routing |
| Viewshed Analysis | Raster (DEM) | Determines which ground areas are visible from a specified observer point or line | Heritage conservation buffer — areas with view of fort; wind farm visual impact assessment |
| Proximity / Distance | Raster | Computes distance from each cell to the nearest feature | Distance from each pixel to nearest road → accessibility map for infrastructure planning |
| Weighted Overlay (Suitability) | Raster | Combines multiple criterion layers with assigned weights into a composite suitability score | Identify land parcels suitable for affordable housing: slope + flood risk + infrastructure access + land cost |
Critical distinction — Network analysis requires vector topology:
Network analysis (shortest path, service area, O-D matrix) requires a topologically correct vector line network — nodes must connect at junctions, edges must have direction and impedance attributes. Performing network analysis on a raster elevation grid is a category error. Raster cost-distance analysis can approximate network routing for broad regional planning but cannot replace topological network analysis for street-level routing.
Source: Longley, Goodchild, Maguire & Rhind, “Geographic Information Systems and Science” (Wiley); ESRI GIS Dictionary.
C5. LiDAR — Point Cloud, DEM/DSM, Urban Feature Extraction
LiDAR (Light Detection and Ranging) is an active remote sensing technology that emits rapid laser pulses (typically NIR, 1064nm) and measures the time for each pulse to return from the target. Distance = (speed of light × time) / 2. Multiple return pulses from a single emitted beam allow simultaneous capture of the top of a tree canopy (first return) and the ground beneath (last return).
LiDAR Workflow in Urban Planning:
Aerial LiDAR flight (airborne platform or UAV)
↓
Raw point cloud (x, y, z + intensity + return number)
↓
Point cloud classification
- Ground points → DEM (bare earth)
- Vegetation points → canopy height model
- Building roof points → DSM
↓
nDSM = DSM − DEM (normalised Digital Surface Model)
= height of objects above ground
↓
Building height extraction: nDSM values over building footprints
↓
Urban planning outputs:
- Building height map (FAR verification)
- Tree canopy cover (green space assessment)
- Flood depth modelling (DEM + water level)
- Solar potential mapping (rooftop slope/orientation from DSM)
| LiDAR Output | Data Structure | Definition | Planning Application |
|---|---|---|---|
| Point Cloud | 3D points (x, y, z) | Raw collection of laser return positions with intensity value | Input for all derived products; building condition assessment; heritage documentation |
| DEM | Raster grid | Bare-ground elevation — buildings and vegetation removed | Flood modelling; drainage design; slope analysis; road alignment |
| DSM | Raster grid | Top-of-surface elevation — includes building roofs and tree canopy | Building height calculation (DSM − DEM = nDSM); solar panel suitability; wind exposure |
| nDSM | Raster grid | DSM minus DEM = height of objects above ground | Building height inventory; violation of height restrictions; FAR enforcement |
| TIN | Vector triangles | Variable-density terrain mesh from classified ground points | Precision earthwork volume; road design; complex terrain where DEM resolution is limiting |
LiDAR is always active. It emits its own laser pulses. It is not a passive sensor. It is not a satellite-only technology — airborne LiDAR (fixed-wing aircraft) and UAV-mounted LiDAR are both operational. Satellite LiDAR exists (ICESat-2) but is used for global elevation profiling, not building-scale urban mapping.
Source: ISRO NRSC active sensing materials; standard RS literature (Jensen; Lillesand & Kiefer).
C6. Planning Applications — Land-Use Change, Sprawl Mapping, Suitability
Land-Use Change Detection
Multi-temporal satellite imagery (same sensor, same season, different years) is classified independently and then compared pixel-by-pixel. Change matrix shows which land use categories converted to which others.
| Technique | Method | Planning Use |
|---|---|---|
| Post-classification comparison | Classify Year 1 and Year 2 independently; compare class labels | Most reliable for long time-gaps; quantifies net change between categories |
| Image differencing | Subtract reflectance values or index values (NDVI, NDBI) between two dates | Rapid identification of changed areas; requires same atmospheric conditions |
| Change detection using NDBI | NDBI = (SWIR − NIR) / (SWIR + NIR); positive = built-up | Detect conversion of agricultural or open land to built-up — urban sprawl quantification |
Urban Sprawl Mapping
Sprawl is identified by comparing urban built-up extent across census years using classified satellite imagery. The Shannon Entropy index (derived from land use distribution across zones) quantifies sprawl: higher entropy = more dispersed, fragmented growth.
Key satellite data for India: Landsat archive (1972–present, free) provides longest available time series. Sentinel-2 (2015–present) provides higher temporal frequency (5-day revisit) at moderate resolution (10m).
Suitability Analysis Workflow
A weighted overlay suitability analysis for a new settlement zone typically follows:
- Identify criteria (slope, flood risk, distance from existing infrastructure, land cost, agricultural quality)
- Convert each criterion to a raster layer with a standardised score (e.g., 1–5, where 5 = most suitable)
- Assign weights to each criterion based on planning priorities (AHP or expert judgement)
- Compute weighted sum: Suitability = Σ(weight_i × score_i)
- Classify the output into suitability zones (High, Medium, Low, Excluded)
- Validate against field reconnaissance and stakeholder input
GIS Applications Aligned to URDPFI 2015 Phases
| URDPFI Phase | RS / GIS Role |
|---|---|
| I — Existing Situation | Base map from Cartosat; LULC classification; topographic mapping from DEM; infrastructure inventory |
| II — Projection | Population demand mapped to spatial units; scenario overlays (projected population × service gaps) |
| III — Plan Formulation | Weighted overlay suitability analysis; zoning map generation; alternative plan visualisation |
| IV — Implementation | Construction monitoring via temporal imagery; building permit database linked to cadastral parcels |
| V — Monitoring | Multi-temporal change detection; FAR/setback compliance monitoring; periodic plan review |
Source: URDPFI 2015, Volume I, Chapter 4; ISRO NRSC, “GIS for Urban Planning.”
D. Worked Numericals and Parameter Tables
No NAT questions are prescribed for Lesson 12.2. Two reference tables fulfil Section D.
Table D1 — Raster vs Vector Decision Table
| Planning Task | Correct Data Model | Justification |
|---|---|---|
| LULC classification from satellite imagery | Raster | Imagery is inherently raster; classification assigns a class to each pixel |
| Shortest route from hospital to accident site | Vector | Requires topologically connected road network; impedance (travel time) on edges |
| Slope analysis for site suitability | Raster (from DEM) | Slope is a continuously varying surface derived from elevation grid |
| Delineating property parcel boundaries | Vector (polygon) | Parcels are discrete, bounded legal units with precise coordinate definitions |
| Flood inundation extent mapping from SAR | Raster | SAR backscatter is an image grid; water/non-water classification is pixel-based |
| Service area analysis (10 min from fire station) | Vector (network) | Requires road topology, travel speed, turn restrictions — raster cannot encode these |
| Temperature surface across a city (urban heat island) | Raster | Temperature is continuously varying; interpolated from point samples or from thermal band |
| Buffer zone around water body (no-build setback) | Vector | Buffer is a geometric operation on a discrete polygon feature |
| Building height extraction | Raster (nDSM from LiDAR) | nDSM = DSM − DEM is a raster arithmetic operation on elevation grids |
| Administrative boundary delineation | Vector (polygon) | Boundaries are precise legal lines, not continuous surfaces |
Table D2 — Satellite Resolution Comparison by Planning Task
| Planning Task | Minimum Spatial Resolution Needed | Suitable Satellites | Notes |
|---|---|---|---|
| Individual building footprint mapping | < 1m | Cartosat-3 (0.25m), WorldView-3 (0.31m Pan), SPOT 6/7 (1.5m Pan) | For FAR audit, setback verification |
| Ward-level land use / land cover | 5–10m | ResourceSat-2 LISS-IV (5.8m), Sentinel-2 (10m) | Standard for city master plans |
| District / regional LULC | 20–30m | ResourceSat-2 LISS-III (23.5m), Landsat 8/9 (30m) | Regional plans; long-term change detection archive |
| Agricultural crop monitoring | 30–60m | ResourceSat-2 AWiFS (56m), Landsat 8/9 (30m) | Seasonal crop area estimation; peri-urban farmland loss |
| Urban sprawl over 30-year period | 30m | Landsat archive (1972–present) | Only freely available long time-series at this resolution |
| Flood inundation during monsoon | 10–25m (SAR) | RISAT-2 (3–25m), Sentinel-1 SAR (10m) | Cloud penetration mandatory; optical unusable during active flood |
| Weather/disaster early warning | ~4 km | INSAT-3D/3DR (GEO) | Rapid revisit required; spatial resolution is secondary |
| Solar rooftop potential mapping | < 1m + LiDAR DSM | Cartosat-3 + aerial LiDAR | Needs roof geometry and slope/orientation from nDSM |
E. Common Confusions
- LiDAR is always active — not passive, not satellite-only. LiDAR emits laser pulses; it does not depend on sunlight. Airborne and UAV-mounted LiDAR are more common for urban mapping than satellite LiDAR (ICESat-2 is a profiling instrument, not an area-mapping tool).
- Network analysis cannot be performed on a raster. Road routing, service area calculation, and O-D matrix analysis require topologically connected vector line networks with traversal costs. Raster cost-distance is an approximation for regional analysis only — it does not respect turn restrictions, one-way streets, or signal delays.
- DSM ≠ DEM. DSM includes building roofs and tree canopy. DEM is bare ground only. The difference (nDSM = DSM − DEM) gives object height above ground. Using DSM for drainage modelling produces incorrect flow paths because buildings appear as terrain obstacles.
- NDVI is not a land use map. NDVI measures relative vegetation vigour (NIR − Red) / (NIR + Red). A high NDVI pixel is vegetated — but it could be a park, farm, forest, or vegetated road median. Converting NDVI directly to a land use map without further classification is a methodological error.
- Spatial resolution ≠ accuracy. A 0.25m image is not automatically more accurate than a 10m image — accuracy depends on geometric correction, atmospheric correction, and classification method. A well-processed 10m Sentinel-2 scene may have higher classification accuracy than a poorly processed 0.5m image.
- SSO ≠ GEO. Sun-Synchronous orbit (700–800 km) provides consistent illumination and is used for change detection. Geostationary orbit (~36,000 km) provides continuous monitoring of a fixed region and is used for weather and disaster warning. They serve different planning functions — never substitute one for the other.
F. Exam Traps
| Trap | Incorrect Belief | Correct Principle |
|---|---|---|
| Network analysis on raster | Road routing can be computed on an elevation grid or satellite image raster | Network analysis requires vector topology (nodes, edges, impedance). Raster has no connectivity logic — it cannot represent one-way streets, turn costs, or junctions |
| LiDAR is passive | LiDAR uses reflected laser light like a camera | LiDAR is an active sensor — it emits its own laser pulses and measures return time. It does not depend on solar radiation |
| LiDAR is satellite-only | LiDAR data comes only from satellites | Airborne LiDAR (fixed-wing or UAV-mounted) is the standard for urban building height mapping. Satellite LiDAR (ICESat-2) profiles elevation along a narrow track — it does not produce area-wide urban maps |
| DSM = DEM | Both are elevation models so they are interchangeable | DSM includes surface objects (buildings, trees); DEM is bare ground only. Using DSM for drainage modelling distorts flow paths. nDSM = DSM − DEM = object heights |
| High spatial resolution = better for all tasks | Always choose the highest-resolution satellite available | Resolution trade-offs mean high spatial → narrow swath + fewer spectral bands + higher cost. Landsat 30m is correct for long-term LULC; Cartosat 0.25m is correct for building-level work |
| SSO provides continuous coverage like GEO | SSO revisits the same area daily | SSO revisit is 1–26 days depending on swath width. Only GEO orbit provides continuous (sub-hourly) monitoring of the same region. Using SSO for real-time cyclone tracking is incorrect |
| Passive sensors work during monsoon flooding | Optical sensors can image through cloud | Optical (passive) sensors are blocked by cloud. SAR (active, microwave) is the only option during monsoon cloud cover — this is the technical basis for ISRO’s RISAT programme |
| NDVI directly equals land use category | NDVI > 0.3 means the area is classified as “green” land use | NDVI is a spectral index, not a classification. Multiple land uses (park, farm, forest) produce similar NDVI values. Supervised or unsupervised classification — not thresholding a single index — produces a land use map |
| Weighted overlay uses raster and vector interchangeably | Suitability layers can be in any format | Weighted overlay (raster map algebra) requires all input layers to be in raster format with identical cell size and spatial extent. Vector layers must be rasterised first |
| Temporal resolution is about how long the sensor has existed | Temporal resolution = archive depth | Temporal resolution is the revisit interval — how often the sensor re-images the same location. It is independent of how long the programme has operated |
G. Answer-Writing Cues
MCQ / MSQ — Active vs passive sensor identification:
“LiDAR and SAR are active sensors — each emits its own energy source (laser pulses and microwave radiation respectively). Landsat OLI, IRS LISS, and SPOT are passive sensors that record solar radiation reflected from the Earth’s surface. Thermal infrared sensors are passive but can operate at night because they record energy emitted by the surface rather than reflected solar energy.”
MCQ — GIS operation selection:
“To identify all residential parcels within 500m of a proposed industrial zone, the correct GIS operation is a buffer (500m around the industrial zone boundary) followed by a spatial join or intersect with the residential land use layer. Network analysis would be incorrect here — the task requires proximity in Euclidean space, not travel distance along roads.”
MSQ — Satellite selection for a given task:
“For mapping the extent of urban sprawl in a metropolitan region over the period 1990–2025, the appropriate satellite data source is Landsat 5/7/8/9 (30m resolution, free archive from 1972, consistent multispectral bands across the series). Cartosat-3 at 0.25m resolution would have insufficient archive depth and prohibitive data volume for a 35-year regional study.”
MCQ / MSQ — LiDAR product identification:
“Building height data extracted from LiDAR requires computing the nDSM (normalised Digital Surface Model = DSM − DEM). The DSM records the top of all surface objects including buildings and trees; the DEM records bare ground. The difference gives the height of each object above the terrain. This nDSM is used for FAR verification and building height violation detection.”
H. PYQ Linkage Note
| Topic | Exam Appearance | Pattern |
|---|---|---|
| Pixel as smallest raster unit | GATE 2021 — direct vocabulary MCQ | “The smallest unit of a raster image is called ___” → pixel; never node/polygon |
| GEO orbit for weather monitoring | GATE 2023, 1993 — orbit type identification | GEO = stationary = INSAT = weather/cyclone tracking |
| SSO for change detection | GATE 2017 — orbit-to-application match | SSO = consistent solar time = multi-temporal comparison = change detection |
| DEM application — flood/slope | GATE 2017 — terrain model selection | DEM = bare ground raster = slope/watershed/flood; DSM ≠ DEM |
| Active vs passive sensor | GATE multiple years — sensor classification | LiDAR and SAR = active; Landsat / IRS / SPOT = passive; thermal = passive (night-capable) |
| GIS operations (buffer/overlay) | State PSC years — operation-to-task match | Buffer = proximity; overlay/intersect = two-layer combination; network = routing |
| Cartosat resolution | Current affairs + GATE — Indian RS literacy | Cartosat-3 = 0.25m Pan = highest resolution Indian satellite |
I. Mini-Check — Lesson 12.2
Q1. (MSQ — select ALL correct) Which of the following statements about remote sensing sensors are correct?
(A) SAR (Synthetic Aperture Radar) can image through cloud cover during monsoon season
(B) LiDAR depends on reflected sunlight and cannot be used at night
(C) Landsat 8 OLI is a passive multispectral sensor operating in Sun-Synchronous orbit
(D) INSAT-3D in Geostationary orbit is suitable for multi-temporal urban land use change detection
(E) Thermal infrared sensors are classified as passive sensors
Answer: A, C, E
Explanation: (A) SAR is active, microwave — cloud-penetrating. Correct. (B) LiDAR is active — emits its own laser pulses; operates day and night. Incorrect. (C) Landsat 8 OLI is passive multispectral in SSO. Correct. (D) INSAT-3D in GEO provides continuous coverage of the same region at ~4km spatial resolution — not suitable for city-level land use change detection which requires 5–30m resolution and temporal archive. Incorrect. (E) Thermal IR sensors record surface-emitted radiation without their own energy source — passive. Correct.
Q2. (MSQ — select ALL correct) A planner needs to perform a suitability analysis to identify land parcels for a new affordable housing project. The criteria are: slope gradient, distance from proposed metro station, flood risk zone, and existing land use. Which of the following statements about the GIS methodology are correct?
(A) All criterion layers must be in raster format with identical cell size before weighted overlay can be applied
(B) Network analysis is the correct GIS operation to compute distance from the metro station to each parcel
(C) The flood risk zone layer (a vector polygon) must be rasterised before inclusion in the weighted overlay
(D) A buffer operation around the metro station can generate a proximity score layer for the weighted overlay
(E) Weighted overlay requires all input layers to be in vector format
Answer: A, C, D
Explanation: (A) Weighted overlay (raster map algebra) requires all layers in raster format with matching extent and cell size. Correct. (B) Distance from metro station to parcels is a Euclidean proximity (buffer/distance raster) task, not a network analysis task. Network analysis computes travel time/distance along roads — the criterion here is proximity, not routed distance. Incorrect. (C) Vector flood polygon must be rasterised to participate in raster map algebra. Correct. (D) A buffer generates a zone of distance; converting it to a scored proximity raster (e.g., 5 = within 300m, 1 = beyond 1,500m) is a valid approach to generate the criterion layer. Correct. (E) Weighted overlay is a raster operation — not vector. Incorrect.
Q3. (MCQ) A planner wishes to extract building heights for an entire city to verify FAR compliance. After obtaining airborne LiDAR data, the first step is to classify the point cloud into ground and non-ground points, producing a DSM and a DEM. What derived product directly represents building heights above ground?
(A) DTM
(B) TIN
(C) nDSM (DSM − DEM)
(D) NDVI
Answer: (C) nDSM (DSM − DEM)
Explanation: nDSM (normalised Digital Surface Model) = DSM − DEM. DSM records the top of all surface objects (building roofs, tree canopy). DEM records bare ground elevation. Their difference isolates the height of above-ground objects. Over building footprints, nDSM values equal building height above terrain — directly applicable for FAR and height-limit compliance checking. DTM is another name for bare-ground terrain (similar to DEM). TIN is a terrain representation format. NDVI is a vegetation spectral index with no relationship to building heights.
Q4. (MCQ) Which satellite orbit type ensures that a sensor passes over the same latitude at the same local solar time on every revisit, enabling consistent illumination conditions for multi-temporal land use change detection?
(A) Geostationary (GEO)
(B) Polar orbit
(C) Sun-Synchronous orbit (SSO)
(D) Low Earth Orbit (LEO) with random inclination
Answer: (C) Sun-Synchronous orbit (SSO)
Explanation: In SSO (700–800 km altitude), the orbital plane precesses at the same rate as Earth orbits the Sun, ensuring the satellite passes over a given latitude at the same local solar time on every pass. This guarantees consistent illumination angle and shadow geometry across all images in a time series — essential for valid multi-temporal comparison. GEO provides continuous coverage of one region but at ~4km spatial resolution — unsuitable for urban LULC mapping. Polar orbit achieves global coverage but does not maintain consistent solar time. (GATE 2017)
Q5. (MCQ) A GIS analyst attempts to compute the shortest travel route between two hospitals using a raster DEM layer as the input network. This approach is technically flawed because:
(A) DEMs store elevation data in floating point format which network solvers cannot read
(B) Raster data has no topological connectivity — it cannot represent road junctions, one-way constraints, or turn costs required for network analysis
(C) Network analysis requires data in GEO coordinate system, not projected coordinates
(D) The DEM resolution of 30m is too coarse for routing calculations
Answer: (B)
Explanation: Network analysis (shortest path, service area) requires a topologically connected vector line network where edges carry impedance values (travel time, distance) and nodes represent junctions with turn restrictions. A raster DEM has no topology — it stores elevation values in a grid of cells with no connectivity rules, no direction attributes, and no junction logic. The conceptual mismatch is the data model, not the resolution, coordinate system, or data type. Option (D) is a secondary practical concern but is not the fundamental flaw — even a 1m DEM would fail for the same structural reason.