Skip to main content

Data Collection and Classification in GIS


In GIS, data collection is the process of gathering geographic information from various sources to build a geospatial database, while data classification organizes this data into meaningful categories for analysis, interpretation, and visualization on a map. These two processes form the foundation for creating accurate, informative, and visually appealing maps.


Data Collection in GIS

Definition: The process of acquiring geographic and attribute data through various techniques, tools, and sources. This step ensures that the raw data required for GIS analysis is available in the desired format and quality.

Methods of Data Collection

  1. Field Data Collection:

    • Data is gathered directly at the location of interest using tools such as:
      • GPS Units: Capturing precise coordinates of geographic features.
      • Mobile Devices and Apps: Recording spatial and attribute data using tools like ArcGIS Field Maps or QField.
    • Example: Measuring the exact locations of trees in a forest using a GPS device.
  2. Remote Sensing:

    • Acquiring data through aerial photography, drones, or satellite imagery.
    • Useful for large-scale data collection, such as land cover mapping.
    • Example: Using Sentinel-2 satellite imagery to map urban growth.
  3. Digitizing:

    • Converting analog maps into digital formats by manually tracing features using GIS software.
    • Example: Digitizing a road network from a paper map.
  4. Secondary Data Sources:

    • Utilizing pre-existing datasets from government agencies, private organizations, or open-data portals.
    • Example: Downloading census data for population analysis.

Data Classification in GIS

Definition: The process of categorizing raw data into meaningful groups or classes to simplify its representation and make patterns easier to interpret.

Common Classification Methods

  1. Equal Interval:

    • Divides the range of data into classes of equal size.
    • Use Case: Ideal for data with uniform distribution.
    • Example: Classifying elevation data into intervals of 100 meters each.
  2. Quantile:

    • Distributes data values evenly among the classes, with each class containing the same number of data points.
    • Use Case: Suitable for datasets with a wide range of values.
    • Example: Grouping household incomes into five income brackets with equal counts in each.
  3. Natural Breaks (Jenks):

    • Identifies "breaks" or groupings in the data to minimize variance within classes.
    • Use Case: Effective for data with distinct clusters.
    • Example: Classifying population densities into natural groupings like urban, suburban, and rural.
  4. Standard Deviation:

    • Shows how much each data point deviates from the mean.
    • Use Case: Highlights outliers or extreme values.
    • Example: Mapping temperature anomalies from the average.

How GIS Software Facilitates Data Collection and Classification

  1. Field Data Collection Apps:

    • Tools like ArcGIS Field Maps, QField, or Survey123 allow users to collect data with GPS coordinates and attach attribute information.
    • Example: Collecting tree species data in a forest and recording their exact locations.
  2. Image Analysis Tools:

    • GIS platforms enable image classification for remote sensing data.
    • Example: Using supervised classification in QGIS to identify land cover types such as water, vegetation, and built-up areas.
  3. Data Visualization Tools:

    • GIS software applies classification schemes (e.g., equal interval, natural breaks) to display spatial patterns using colors, symbols, or shading.
    • Example: Visualizing pollution levels on a map using a gradient color scale.

Example Applications

  1. Land Use Mapping:

    • Data Collection: Field surveys and satellite imagery.
    • Classification: Categorizing land into classes like forest, urban, agriculture, and water.
    • Output: A thematic map showing land use types.
  2. Environmental Analysis:

    • Data Collection: Air quality monitoring stations.
    • Classification: Grouping air pollution levels into low, medium, and high categories using standard deviation.
    • Output: Identifying and mapping high-risk pollution zones.
  3. Demographic Analysis:

    • Data Collection: Census data from government databases.
    • Classification: Grouping populations by income, age, or education level using quantile classification.
    • Output: Maps showing income disparities across regions.

Key Points

  1. Integration: Data collection and classification work together to ensure accurate representation of spatial phenomena.
  2. Tool Utilization: GIS software like ArcGIS, QGIS, and Google Earth Engine streamline these processes.
  3. Application: These techniques are used across fields such as urban planning, environmental management, and public health for better decision-making.



Comments

Popular posts from this blog

Radar Sensors in Remote Sensing

Radar sensors are active remote sensing instruments that use microwave radiation to detect and measure Earth's surface features. They transmit their own energy (radio waves) toward the Earth and record the backscattered signal that returns to the sensor. Since they do not depend on sunlight, radar systems can collect data: day or night through clouds, fog, smoke, and rain in all weather conditions This makes radar extremely useful for Earth observation. 1. Active Sensor A radar sensor produces and transmits its own microwaves. This is different from optical and thermal sensors, which depend on sunlight or emitted heat. 2. Microwave Region Radar operates in the microwave region of the electromagnetic spectrum , typically from 1 mm to 1 m wavelength. Common radar frequency bands: P-band (70 cm) L-band (23 cm) S-band (9 cm) C-band (5.6 cm) X-band (3 cm) Each band penetrates and interacts with surfaces differently: Lo...

Optical Sensors in Remote Sensing

1. What Are Optical Sensors? Optical sensors are remote sensing instruments that detect solar radiation reflected or emitted from the Earth's surface in specific portions of the electromagnetic spectrum (EMS) . They mainly work in: Visible region (0.4–0.7 µm) Near-Infrared – NIR (0.7–1.3 µm) Shortwave Infrared – SWIR (1.3–3.0 µm) Thermal Infrared – TIR (8–14 µm) — emitted energy, not reflected Optical sensors capture spectral signatures of surface features. Each object reflects/absorbs energy differently, creating a unique spectral response pattern . a) Electromagnetic Spectrum (EMS) The continuous range of wavelengths. Optical sensing uses solar reflective bands and sometimes thermal bands . b) Spectral Signature The unique pattern of reflectance or absorbance of an object across wavelengths. Example: Vegetation reflects strongly in NIR Water absorbs strongly in NIR and SWIR (appears dark) c) Radiance and Reflectance Radi...

Geometric Correction

When satellite or aerial images are captured, they often contain distortions (errors in shape, scale, or position) caused by many factors — like Earth's curvature, satellite motion, terrain height (relief), or the Earth's rotation . These distortions make the image not properly aligned with real-world coordinates (latitude and longitude). 👉 Geometric correction is the process of removing these distortions so that every pixel in the image correctly represents its location on the Earth's surface. After geometric correction, the image becomes geographically referenced and can be used with maps and GIS data. Types  1. Systematic Correction Systematic errors are predictable and can be modeled mathematically. They occur due to the geometry and movement of the satellite sensor or the Earth. Common systematic distortions: Scan skew – due to the motion of the sensor as it scans the Earth. Mirror velocity variation – scanning mirror moves at a va...

Thermal Sensors in Remote Sensing

Thermal sensors are remote sensing instruments that detect naturally emitted thermal infrared (TIR) radiation from the Earth's surface. Unlike optical sensors (which detect reflected sunlight), thermal sensors measure heat energy emitted by objects because of their temperature. They work mainly in the Thermal Infrared region (8–14 µm) of the electromagnetic spectrum. 1. Thermal Infrared Radiation All objects above 0 Kelvin (absolute zero) emit electromagnetic radiation. This is explained by Planck's Radiation Law . For Earth's surface temperature range (about 250–330 K), the peak emitted radiation occurs in the 8–14 µm thermal window . Thus, thermal sensors detect emitted energy , not reflected sunlight. 2. Emissivity Emissivity is the efficiency with which a material emits thermal radiation. Values range from 0 to 1 : Water, vegetation → high emissivity (0.95–0.99) Bare soil → medium (0.85–0.95) Metals → low (0.1–0.3) E...

LiDAR in Remote Sensing

LiDAR (Light Detection and Ranging) is an active remote sensing technology that uses laser pulses to measure distances to the Earth's surface and create high-resolution 3D maps . LiDAR sensors emit short pulses of laser light (usually in the near-infrared range) and measure the time it takes for the pulse to return after hitting an object. Because LiDAR measures distance very precisely, it is excellent for mapping: terrain vegetation height buildings forests coastlines flood plains ✅ 1. Active Sensor LiDAR sends its own laser energy, unlike passive sensors that rely on sunlight. ✅ 2. Laser Pulse LiDAR emits thousands of pulses per second (even millions). Wavelengths commonly used: Near-Infrared (NIR) → land and vegetation mapping Green (532 nm) → water/ bathymetry (penetrates shallow water) ✅ 3. Time of Flight (TOF) The sensor measures the time taken for the laser to travel: from the sensor → to the sur...