Skip to main content

Supervised Classification

In the context of Remote Sensing (RS) and Digital Image Processing (DIP), supervised classification is the process where an analyst defines "training sites" (Areas of Interest or ROIs) representing known land cover classes (e.g., Water, Forest, Urban). The computer then uses these training samples to teach an algorithm how to classify the rest of the image pixels.

The algorithms used to classify these pixels are generally divided into two broad categories: Parametric and Nonparametric decision rules.


Parametric Decision Rules

These algorithms assume that the pixel values in the training data follow a specific statistical distribution—almost always the Gaussian (Normal) distribution (the "Bell Curve").

  • Key Concept: They model the data using statistical parameters: the Mean vector ($\mu$) and the Covariance matrix ($\Sigma$).

  • Analogy: Imagine trying to fit a smooth hill over your data points. If a new point lands high up on the hill, it belongs to that class.

Nonparametric Decision Rules

These algorithms make no assumptions about the statistical distribution of the data. They do not care if the data fits a bell curve.

  • Key Concept: They classify based on discrete geometric shapes (polygons, boxes) or the relative position of the data points themselves.

  • Analogy: Imagine drawing a literal box or fence around your data points. If a new point falls inside the fence, it belongs to that class.


A. Minimum-Distance-to-Means (MDM)

  • Classification: Generally considered a simple Parametric classifier (as it relies on the mean parameter), though it operates geometrically.

  • How it works:

    1. The algorithm calculates the spectral mean vector (the center point or centroid) for each training class.

    2. For every unclassified pixel in the image, it calculates the Euclidean distance to the mean of every class.

    3. The pixel is assigned to the class with the shortest distance.


  • Pros: Very fast computationally; mathematically simple.

  • Cons: It is insensitive to the variance (spread) of the data.

    • Example: If "Urban" data is very scattered (high variance) and "Water" is very tight (low variance), a pixel far from the Urban center might actually belong to Urban, but MDM might classify it as Water just because the Water mean is slightly closer geometrically.

B. Parallelepiped Classification

  • Classification: Nonparametric.

  • How it works:

    1. The algorithm looks at the training data and finds the minimum and maximum brightness values for each band.

    2. It creates a rectangular box (a parallelepiped in multi-dimensional space) defined by these limits.

    3. If a pixel's value falls within the box, it is assigned to that class.

  • Pros: Extremely fast; easy to understand conceptually.

  • Cons:

    • The Correlation Problem: Real remote sensing data (like vegetation in Red vs. NIR bands) is often correlated (diagonal distribution). A rectangular box cannot fit a diagonal data cloud efficiently, leading to large "empty corners" in the box that capture noise/wrong pixels.

    • Overlapping: Pixels often fall into the overlapping area of two boxes, leaving the computer unable to decide.

C. Gaussian Maximum Likelihood (GML/MLC)

  • Classification: Parametric (The standard industry workhorse).

  • How it works:

    1. It assumes the data for each class is normally distributed.

    2. It uses both the Mean vector AND the Covariance matrix to calculate the probability density function.

    3. It calculates the statistical probability of a pixel belonging to each class.

    4. It constructs ellipsoidal equiprobability contours (rather than circles or boxes).

  • Pros: Highly accurate because it accounts for the variance (spread) and covariance (correlation/direction) of the data. It handles "diagonal" data clouds perfectly.

  • Cons: Computationally expensive (slow on massive images); requires a large number of training pixels per class to compute a stable covariance matrix (usually $10N$ to $100N$ pixels, where $N$ is the number of bands).


FeatureParallelepipedMinimum DistanceMaximum Likelihood
TypeNonparametricParametric (Simple)Parametric (Advanced)
GeometryRectangular BoxesCircles/SpheresEllipsoids
AssumptionsNone (Min/Max thresholds)Mean Center PointGaussian Distribution
SpeedVery FastFastSlow / Intensive
AccuracyLow to ModerateModerateHigh
Best Used ForQuick looks; Uncorrelated dataWell-separated classesComplex, correlated data


Comments

Popular posts from this blog

Platforms in Remote Sensing

In remote sensing, a platform is the physical structure or vehicle that carries a sensor (camera, scanner, radar, etc.) to observe and collect information about the Earth's surface. Platforms are classified mainly by their altitude and mobility : Ground-Based Platforms Definition : Sensors mounted on the Earth's surface or very close to it. Examples : Tripods, towers, ground vehicles, handheld instruments. Applications : Calibration and validation of satellite data Detailed local studies (e.g., soil properties, vegetation health, air quality) Strength : High spatial detail but limited coverage. Airborne Platforms Definition : Sensors carried by aircraft, balloons, or drones (UAVs). Altitude : A few hundred meters to ~20 km. Examples : Airplanes with multispectral scanners UAVs with high-resolution cameras or LiDAR High-altitude balloons (stratospheric platforms) Applications : Local-to-regional mapping ...

Types of Remote Sensing

Remote Sensing means collecting information about the Earth's surface without touching it , usually using satellites, aircraft, or drones . There are different types of remote sensing based on the energy source and the wavelength region used. ๐Ÿ›ฐ️ 1. Active Remote Sensing ๐Ÿ“˜ Concept: In active remote sensing , the sensor sends out its own energy (like a signal or pulse) to the Earth's surface. The sensor then records the reflected or backscattered energy that comes back from the surface. ⚙️ Key Terminology: Transmitter: sends energy (like a radar pulse or laser beam). Receiver: detects the energy that bounces back. Backscatter: energy that is reflected back to the sensor. ๐Ÿ“Š Examples of Active Sensors: RADAR (Radio Detection and Ranging): Uses microwave signals to detect surface roughness, soil moisture, or ocean waves. LiDAR (Light Detection and Ranging): Uses laser light (near-infrared) to measure elevation, vegetation...

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 ยตm) Near-Infrared – NIR (0.7–1.3 ยตm) Shortwave Infrared – SWIR (1.3–3.0 ยตm) Thermal Infrared – TIR (8–14 ยตm) — 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...

Resolution of Sensors in Remote Sensing

Spatial Resolution ๐Ÿ—บ️ Definition : The smallest size of an object on the ground that a sensor can detect. Measured as : The size of a pixel on the ground (in meters). Example : Landsat → 30 m (each pixel = 30 × 30 m on Earth). WorldView-3 → 0.31 m (very detailed, you can see cars). Fact : Higher spatial resolution = finer details, but smaller coverage. Spectral Resolution ๐ŸŒˆ Definition : The ability of a sensor to capture information in different parts (bands) of the electromagnetic spectrum . Measured as : The number and width of spectral bands. Types : Panchromatic (1 broad band, e.g., black & white image). Multispectral (several broad bands, e.g., Landsat with 7–13 bands). Hyperspectral (hundreds of very narrow bands, e.g., AVIRIS). Fact : Higher spectral resolution = better identification of materials (e.g., minerals, vegetation types). Radiometric Resolution ๐Ÿ“Š Definition : The ability of a sensor to ...

geostationary and sun-synchronous

Orbital characteristics of Remote sensing satellite geostationary and sun-synchronous  Orbits in Remote Sensing Orbit = the path a satellite follows around the Earth. The orbit determines what part of Earth the satellite can see , how often it revisits , and what applications it is good for . Remote sensing satellites mainly use two standard orbits : Geostationary Orbit (GEO) Sun-Synchronous Orbit (SSO)  Geostationary Satellites (GEO) Characteristics Altitude : ~35,786 km above the equator. Period : 24 hours → same as Earth's rotation. Orbit type : Circular, directly above the equator . Appears "stationary" over one fixed point on Earth. Concepts & Terminologies Geosynchronous = orbit period matches Earth's rotation (24h). Geostationary = special type of geosynchronous orbit directly above equator → looks fixed. Continuous coverage : Can monitor the same area all the time. Applications Weather...