Skip to main content

Weighted Overlay in GIS: A Spatial Decision-Making Technique


Weighted Overlay is a widely used spatial decision-making technique in Geographic Information Systems (GIS). It functions as an analytical method that balances multiple spatial factors by assigning relative importance to each variable. Essentially, it integrates scientific reasoning with logical evaluation to determine the suitability of locations for specific purposes.

In simple terms, Weighted Overlay is a method that combines several spatial raster layers. Each layer represents a different factor influencing the decision-making process. Before integration, the values of each raster layer are standardized to a common evaluation scale, typically ranging from 1 to 5 or 1 to 9. Subsequently, each layer is assigned a weight based on its relative importance. The final suitability value for each cell is calculated by summing the weighted contributions of all layers.

The conceptual formula can be expressed as:

Final Suitability Value = (Layer 1 × Weight 1) + (Layer 2 × Weight 2) + ... + (Layer n × Weight n)

A practical example can be illustrated through groundwater well site selection. Identifying a suitable location for a water well requires consideration of multiple environmental and geological factors, including soil type, slope, proximity to pollution sources, and groundwater depth. Each factor individually provides partial information; however, comprehensive site suitability assessment requires integrating all factors simultaneously.

For instance, soil type may be considered the most influential factor and assigned a weight of 40 percent. Groundwater depth may be assigned a weight of 30 percent, slope 20 percent, and distance from pollution sources 10 percent. After reclassifying and standardizing these factors, the Weighted Overlay analysis produces a suitability map that categorizes areas into highly suitable, moderately suitable, and unsuitable zones.

Weighted Overlay is commonly applied in groundwater potential mapping, land-use planning, pollution risk assessment, infrastructure site selection (such as roads, factories, and treatment plants), and environmental and hydrological studies.

It is important to note that Weighted Overlay primarily operates on raster datasets rather than vector data. Therefore, several preprocessing steps are required before analysis, including reclassification of input layers, standardization of cell size, and alignment of spatial extent. These steps ensure consistency and accuracy in the final output.

Although Weighted Overlay is a powerful analytical tool, its results depend heavily on the selection of input factors, the classification scheme used, and the weights assigned to each variable. Consequently, careful evaluation and domain expertise are essential to ensure reliable and scientifically meaningful outcomes.


Comments

Popular posts from this blog

Regional Geography, Systematic Geography, Idiographic, Nomothetic, Inductive and Deductive Approaches

T wo major ways of studying Geography : the Regional Approach and the Systematic Approach . It also explains the related ideas of idiographic vs. nomothetic and inductive vs. deductive reasoning , especially in the context of the Hartshorne–Schaefer debate . 1. Regional Geography: “All About One” Regional Geography studies one particular region in detail . A region is an area that has some degree of homogeneity (sameness) within its boundary but is also unique or different from other regions . For example, if we study Palakkad District , we may study: Relief and drainage Climate Soil Vegetation Agriculture Population Occupation Economy Culture Political characteristics The purpose is to understand the complete geographical personality of Palakkad and the relationships among its different features. Key concepts Region: A geographical area with identifiable characteristics and boundaries. Homogeneity: Si...

Multispectral and Hyperspectral Imaging Systems

The main idea is how a remote-sensing sensor collects information about an area . A sensor does not simply take an ordinary photograph. It measures the electromagnetic energy reflected or emitted by objects in different wavelength bands . Depending on how many bands are measured and how the sensor collects them, different imaging systems are used. 1. Multispectral vs. Hyperspectral Multispectral imaging (MSI) records information in a limited number of relatively broad, separate spectral bands , such as blue, green, red, near-infrared and shortwave infrared. Hyperspectral imaging (HSI) records information in many narrow and usually contiguous spectral bands . Therefore, it provides a much more detailed spectral signature of each pixel. The resulting dataset is commonly called a hyperspectral data cube (hypercube) because it contains: X-axis → spatial information Y-axis → spatial information Z-axis → wavelength/spectral information Thus, hype...

Discrete Detectors and Scanning mirrors Across the track scanner Whisk broom scanner.

Multispectral Imaging Using Discrete Detectors and Scanning Mirrors (Across-Track Scanner or Whisk Broom Scanner) Multispectral Imaging:  This technique involves capturing images of the Earth's surface using multiple sensors that are sensitive to different wavelengths of electromagnetic radiation.  This allows for the identification of various features and materials based on their spectral signatures. Discrete Detectors:  These are individual sensors that are arranged in a linear or array configuration.  Each detector is responsible for measuring the radiation within a specific wavelength band. Scanning Mirrors:  These are optical components that are used to deflect the incoming radiation onto the discrete detectors.  By moving the mirrors,  the sensor can scan across the scene,  capturing data from different points. Across-Track Scanner or Whisk Broom Scanner:  This refers to the scanning mechanism where the mirror moves perpendicular to the direction of flight.  This allows for t...

Thermal Infrared Remote Sensing

1. Principles Thermal Infrared Remote Sensing is based on the detection of naturally emitted electromagnetic radiation from objects, rather than reflected solar energy. According to Planck's Radiation Law , all objects with a temperature above absolute zero (0 K) emit electromagnetic radiation. For Earth surface features, the peak emission lies in the Thermal Infrared (TIR) region of 3–14 μm of the electromagnetic spectrum. The amount of radiation emitted is primarily a function of surface temperature and emissivity . Sensors measure the radiant energy flux density (W/m²) , which is later converted to surface temperature using Stefan-Boltzmann's Law . 2. Radiation Properties in TIR Emissivity (ε): Ratio of radiation emitted by a surface to that emitted by a perfect blackbody at the same temperature. Natural surfaces like water (ε ≈ 0.98) have high emissivity, while bare soils and metals have lower values. Blackbody: An idealized object th...

Satalite

Landsat → Land resources SPOT → High-resolution mapping IRS → Indian natural-resource mapping ASTER → Geology + thermal + DEM QuickBird → Very high spatial resolution MODIS → Daily global monitoring GOES → Weather monitoring AVHRR → Weather + vegetation + ocean AVIRIS → Hyperspectral imaging Highest spectral resolution: AVIRIS (224 narrow bands) Highest spatial resolution in this list: QuickBird (~0.61 m PAN) Highest temporal frequency: GOES (minutes) Best broad global monitoring: MODIS Indian sensors: IRS-LISS III and LISS IV Hyperspectral: AVIRIS Thermal + multispectral + DEM: ASTER abbreviations MSS – Multispectral Scanner System TM – Thematic Mapper ETM+ – Enhanced Thematic Mapper Plus GOES – Geostationary Operational Environmental Satellite AVHRR – Advanced Very High Resolution Radiometer HRV – High Resolution Visible HRVIR – High Resolution Visible and Infrared HRG – High Resolution Geometric ...