Skip to main content

Graduated Symbol with Quantile Classification

Graduated Symbol with Quantile Classification

Geographical data visualization plays a crucial role in GIS-based research, helping to reveal spatial patterns and distributions. One such method is the Graduated Symbol Map with Quantile Classification, which combines statistical categorization with symbolic representation for effective data interpretation.


1. The Concept of Graduated Symbols

Graduated symbols in GIS are proportional representations of numerical data assigned to geographical features. The size of each symbol changes according to the magnitude of the associated data attribute. This technique is commonly used for:

  • Visualizing variation in spatial datasets (e.g., crime rates, GDP, population density).
  • Highlighting relative differences rather than absolute values.
  • Avoiding misinterpretation often caused by color-based representations in choropleth maps.

For instance, in a crime rate map, cities with higher crime rates would be represented with larger circles, while those with lower crime rates would have smaller circles.


2. Quantile Data Classification: Statistical Basis

Quantile classification is a statistical approach that divides data into equal-sized groups. If the data is divided into four groups (quartiles), each class contains 25% of the total observations.

Mathematical Explanation

Given a dataset D with n observations, a quantile classification finds the k-th percentile (Qk) by:

Qk=X(k×n)Q_k = X_{(k \times n)}

where:

  • kk is the quantile (e.g., 0.25 for the first quartile, 0.50 for the median, etc.).
  • X(k×n)X_{(k \times n)} is the value at the respective position when data is sorted.

Example Dataset

CityCrime Rate (per 100,000 people)
A125
B200
C350
D450
E500
F750
G800
H950

Sorting the data:

125,200,350,450,500,750,800,950125, 200, 350, 450, 500, 750, 800, 950

For quartile-based classification (4 groups):

  • Q1 (25%) → 287.5 (between 200 and 350)
  • Q2 (50%) → 475 (between 450 and 500)
  • Q3 (75%) → 775 (between 750 and 800)

Thus, the class intervals would be:

  1. 125 - 287.5 (Smallest symbols)
  2. 287.6 - 475
  3. 476 - 775
  4. 776 - 950 (Largest symbols)

3. Analytical Benefits and Drawbacks

Benefits

  1. Uniform Distribution of Data in Classes

    • Ensures each class contains an equal number of data points.
    • Helps in avoiding class imbalance that can occur in natural breaks or standard deviation-based classification.
  2. Better Visualization for Skewed Data

    • If the data distribution is highly skewed (i.e., clustered towards one end), quantile classification ensures all data ranges are equally represented.
    • Helps in highlighting contrasts even in small differences.
  3. Easier Interpretation

    • Since each class contains an equal number of data points, comparison across different regions is straightforward.

Drawbacks

  1. Artificial Grouping of Data

    • In cases where the data is not evenly distributed, boundaries might not represent real-world differences.
    • For example, two cities with crime rates of 799 and 801 might be placed in separate categories, creating an artificial break.
  2. Size Misrepresentation in Graduated Symbols

    • If values in a category vary significantly, symbol sizes might exaggerate or understate real differences.
    • For instance, a city with a crime rate of 500 would receive the same symbol size as another with 750, despite a notable difference.

4. Applied Example in GIS

If applying this technique in ArcGIS, QGIS, or Google Earth Engine, the workflow would be:

  1. Data Collection: Import the geospatial dataset (e.g., crime rates, population density).
  2. Sorting and Classification: Use quantile classification to divide the dataset into equal-size groups.
  3. Symbol Scaling: Assign graduated symbols (e.g., circle size increases with crime rate).
  4. Map Interpretation: Analyze spatial distribution and identify hotspots or patterns.


Implementing Graduated Symbols with Quantile Classification in ArcGIS

ArcGIS allows you to apply graduated symbols and classify data using quantiles for effective spatial analysis. Below is a step-by-step guide to implementing this technique.


Step 1: Load the Data

  1. Open ArcGIS Pro or ArcMap.
  2. Click Add Data → Select the shapefile or geodatabase feature class that contains your spatial data (e.g., crime rates, population).
  3. Ensure your dataset includes a numerical field for classification (e.g., "Crime Rate per 100,000 people").

Step 2: Open the Symbology Panel

  1. Right-click on the layer in the Table of Contents.
  2. Select Symbology.
  3. Choose Graduated Symbols.

Step 3: Configure the Classification

  1. In the Symbology tab:
    • Choose the Value Field (e.g., "Crime Rate").
    • Set Normalization (optional, e.g., dividing crime counts by population size).
  2. Under Classification, select Quantile (Equal Count).
  3. Set the number of classes (e.g., 4 for quartiles, 5 for quintiles).
  4. Click Classify to generate class breaks.

Step 4: Customize Symbol Sizes

  1. Adjust the minimum and maximum symbol sizes for clear differentiation.
  2. Use proportional scaling to ensure readability.
  3. Optionally, choose circle, square, or other symbols to best represent the data.

Step 5: Finalize and Export

  1. Click Apply to preview the changes.
  2. Click OK to finalize the symbology.
  3. To export the map:
    • Go to Layout View.
    • Add a Legend, Title, Scale Bar, and North Arrow.
    • Export as PDF, PNG, or GeoTIFF.

Example Use Case: Crime Rate Mapping

  • Dataset: Crime rates in different districts.
  • Classification: Quantile (4 classes)
    • 0–250 crimes: Smallest symbol
    • 251–500 crimes: Medium symbol
    • 501–750 crimes: Large symbol
    • 751+ crimes: Largest symbol
  • Output: A clear spatial pattern showing high-crime areas.






Quantile Classification






The Graduated Symbol with Quantile Classification is a powerful GIS visualization tool that balances spatial representation with statistical fairness. It ensures that all areas receive equal emphasis, which is useful in urban planning, socio-economic studies, and environmental monitoring. However, careful interpretation is required to avoid artificial class separations and misrepresentation due to symbol scaling.

Comments

Popular posts from this blog

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...

Atmospheric Window

The atmospheric window in remote sensing refers to specific wavelength ranges within the electromagnetic spectrum that can pass through the Earth's atmosphere relatively unimpeded. These windows are crucial for remote sensing applications because they allow us to observe the Earth's surface and atmosphere without significant interference from the atmosphere's constituents. Key facts and concepts about atmospheric windows: Visible and Near-Infrared (VNIR) window: This window encompasses wavelengths from approximately 0. 4 to 1. 0 micrometers. It is ideal for observing vegetation, water bodies, and land cover types. Shortwave Infrared (SWIR) window: This window covers wavelengths from approximately 1. 0 to 3. 0 micrometers. It is particularly useful for detecting minerals, water content, and vegetation health. Mid-Infrared (MIR) window: This window spans wavelengths from approximately 3. 0 to 8. 0 micrometers. It is valuable for identifying various materials, incl...

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...

Radar image. Polarization in Remote Sensing

L band radars operate on a wavelength of 15-30 cm and a frequency of 1-2 GHz. L band radars are mostly used for clear air turbulence studies. S band radars operate on a wavelength of 8-15 cm and a frequency of 2-4 GHz. Because of the wavelength and frequency, S band radars are not easily attenuated. . Polarization refers to the direction of travel of an electromagnetic wave vector's tip: vertical (up and down), horizontal (left to right), or  circular (rotating in a constant plane left or right). . a synthetic aperture radar (SAR) for high-resolution imaging. a radar altimeter, to measure the ocean topography. echo amplitude a wind scatterometer to measure wind speed and direction. Other types of radars have been flown for Earth observation missions: precipitation radars such as the  Tropical Rainfall Measuring Mission, or cloud radars like the one used on Cloudsat. . RISAT-1 (SAR, ISRO India, 2012) RORSAT (SAR, Soviet Union, 1967-1988) Seasat (SAR, altimeter, scatterometer, US, 19...

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...