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GIS and remote sensing

Civil Engineering (B.E./B.Tech) · Surveying · free study notes for exams, placements and interviews

In short

A Geographic Information System (GIS) is computer software plus a database that stores, displays, queries and analyses data tied to position on the Earth, while remote sensing is the science of obtaining information about the surface without touching it, using sensors on satellites, aircraft or drones. Together they form the data-capture and data-analysis halves of modern spatial engineering: remote sensing supplies imagery and DEMs, GIS converts them into maps, areas, routes and decisions. In Indian universities this topic appears in Surveying-II / Advanced Surveying and in GATE Civil (Geomatics Engineering section), examined through resolution types, electromagnetic spectrum, data models, projections, NDVI and classification. Employers who test it include NRSC/ISRO, Survey of India, RITES, L&T, AECOM, WAPCOS, state remote sensing application centres, smart-city SPVs, and GIS firms such as Genesys, RMSI and ESRI India.

Explained

What GIS is: components, data models and functions

GIS analysis operations

  1. Buffer: a zone of given width around a feature — e.g. 100 m from a river bank for a flood-plain or riverfront building restriction.
  2. Overlay (vector): *intersect* (common area only), *union* (all areas), *clip* (cookie-cutter), *erase*, *symmetric difference*, *identity*. Intersect, union and identity outputs carry attributes from both inputs; clip and erase keep only the input layer's attributes.
  3. Map algebra (raster overlay): cell-by-cell arithmetic or logical combination; used in weighted-overlay suitability models (e.g. landfill siting, groundwater potential).
  4. Reclassification: grouping values into classes (slope 0-5°, 5-10° …) before weighting.
  5. Network analysis: shortest path, service area, allocation, tracing — needs connected, topologically clean lines with impedance (length, time, cost).
  6. Interpolation: generating a continuous surface from point samples — IDW (inverse distance weighting), kriging, spline, natural neighbour; used for rainfall, groundwater table, contaminant plumes.
  7. Terrain analysis on a DEM: slope, aspect, hillshade, flow direction and accumulation, watershed delineation, viewshed, cut-and-fill volumes, profile and cross-sections.
  8. Geocoding and address matching: converting addresses to coordinates; the reverse is reverse geocoding.
  9. Digitising errors to fix: sliver polygons, dangling nodes, duplicate arcs, unclosed polygons — cleaned by snapping tolerance and topology rules.

Coordinate systems, datums and projections

Remote sensing: physics and platforms

Resolutions, sensors and Indian missions

Image processing and classification

GIS-RS integration and civil engineering workflows

Key points

Formulas and examples

NDVI = (NIR − Red) / (NIR + Red) — dimensionless, range −1 to +1; NIR and Red are reflectance (or DN) values. Water < 0, bare soil ≈ 0.1-0.2, dense vegetation 0.6-0.9.
NDWI = (Green − NIR) / (Green + NIR); NDBI = (SWIR − NIR) / (SWIR + NIR) — water and built-up indices, same range.
Number of pixels in a raster = Area / (cell size)²; File size (bytes) ≈ rows × columns × bands × (bits per pixel / 8)
Area on ground of one pixel = (GSD)², GSD in m → area in m²; 1 hectare = 10,000 m²; 1 km² = 100 ha
Instantaneous field of view: GSD = β × H, where β = IFOV in radians and H = sensor altitude (m)
Ground area imaged per scene = swath width × along-track length (km²)
Radiometric resolution: number of grey levels = 2ⁿ, n = bit depth
Map scale: ground distance = map distance × scale denominator; smallest mappable detail ≈ 0.25 mm × denominator
Overall accuracy = (Σ diagonal of error matrix) / (total samples); Kappa κ = (p₀ − pₑ)/(1 − pₑ), p₀ = observed agreement, pₑ = chance agreement = Σ(row total × column total)/N²
RMSE of georeferencing = √[ Σ((Δx)² + (Δy)²) / n ], n = number of GCPs, Δ in map units (m)
Slope from a DEM: tan θ = Δh / Δd; percent slope = 100 × Δh/Δd

Example 1 — NDVI from LISS-III reflectance. A pixel gives Red = 0.08 and NIR = 0.46 reflectance; a second pixel gives Red = 0.22, NIR = 0.26.

Example 2 — Pixel count, area and file size. A LISS-III scene (23.5 m resolution, 4 bands, 10-bit stored in 16-bit) covers a 141 km × 141 km swath.

Example 3 — Area of a classified land-use class. A supervised classification on a 23.5 m raster labels 48,200 pixels as "built-up".

Example 4 — Georeferencing RMSE. Four GCPs give residuals (Δx, Δy) in metres: (1.2, −0.8), (−1.5, 0.6), (0.9, 1.1), (−0.4, −1.3).

Example 5 — Classification accuracy and kappa. A 3-class error matrix (rows = classification, columns = reference), N = 200:

Classified ↓ / Reference →WaterVegetationBuilt-upRow total
Water452350
Vegetation368980
Built-up2105870
Column total508070200

Comparison tables.

VectorRaster
StorageCoordinates of featuresGrid of cells
Best forBoundaries, networks, cadastreImagery, elevation, continuous data
File sizeSmall; set by vertex count, not areaLarge, grows as 1/(cell size)²
OverlayComputationally heavier, exactFast map algebra, cell-limited precision
TopologyExplicitly storedImplicit in cell neighbourhood
Output lookClean lines at any zoomBlocky when zoomed beyond resolution
SensorResolutionBandsTypical Indian use
AWiFS (Resourcesat)56 m4Crop acreage, drought, national land use
LISS-III23.5 m4Watershed, forest cover, district planning
LISS-IV5.8 m3Urban land use, cadastral-level thematic work
Cartosat-12.5 m stereoPanCartoDEM, alignment studies, contours
Cartosat-2/3~0.65 m to ~0.25-0.3 mPan + MXUtility mapping, property tax surveys
RISAT / Sentinel-13-25 m (SAR)C/X bandFlood mapping in monsoon, subsidence

Where it is used

Interview questions

Common mistakes

Related topics

Photogrammetry and drone surveys · Theodolite, total station and GPS · Surveying: chain, compass and levelling · Transportation engineering (alignment and route surveys) · Hydrology and watershed management · Urban planning and town planning.

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