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Drainage Regionalization

Drainage regionalization refers to the systematic classification of river systems based on common physical, hydrological, and geomorphological characteristics . In India, drainage is mainly categorized according to: Origin and river characteristics Direction of flow / discharge Size of catchment area Physiographic control and geological structure This framework helps understand: Water resource distribution Flood potential Landform development River behavior and environmental management Drainage Basin / Catchment Area The total area drained by a river and its tributaries. Example: The Ganga basin is India's largest, covering nearly 26% of the country. Watershed A smaller hydrological unit within a basin, separated by ridges or highlands. Perennial Rivers Flow throughout the year; fed by rainfall + snowmelt. Example: Ganga, Brahmaputra. Seasonal (Non-perennial) Rivers Flow mainly during the monsoon; dry up in summer. ...

Biogeographical Zones of India

India's natural environment is divided into 10 biogeographical zones based on distinct biological communities , ecological conditions , geological history , and climatic variations . This classification, widely referenced in ecology and conservation, comes from the work of Rodgers and Panwar (1988) under the Wildlife Institute of India. These 10 zones are further subdivided into 27 biogeographic provinces . This system helps scientists understand: Species distribution Habitat diversity Ecosystem functions Conservation priorities 1. Biogeography The scientific study of the distribution of species, ecosystems, and biotic communities across space and time. 2. Biogeographical Zone A large geographical area separated from others by ecological, climatic, or physical boundaries. Each zone has unique plants, animals, and environmental conditions. 3. Biogeographic Province A smaller subdivision within a biogeographical zone that reflects finer ecologi...

shortest path QGIS

TIN QGiS

Carbon Cycle

Carbon Cycle 

Nonlinear Contrast Enhancement

  🔹 What is Contrast Enhancement? Contrast enhancement improves the difference between light and dark areas of an image so that important features become more visible. It changes the Digital Number (DN) values (brightness values) of pixels to make the image clearer and easier to interpret. There are two main types of contrast enhancement: Linear (simple stretching or scaling of pixel values) Nonlinear (based on the statistical distribution of pixel values) Here, we focus on Nonlinear Contrast Enhancement methods. ⚙️ 1. Histogram Equalization 🔸 Concept: In this method, all pixel brightness values (DNs) are redistributed so that there are roughly an equal number of pixels for each possible brightness level. The result is a flatter histogram , meaning the image uses the full range of brightness values more evenly. 🔸 Purpose: To increase contrast in areas where pixel values are heavily concentrated (for example, dark or light regions). 🔸...

cyclone

Contrast Enhancement

Image enhancement is the process of improving the visual quality and interpretability of an image. The goal is not to change the physical meaning of the image data , but to make important features easier to identify for visual interpretation or automatic analysis (e.g., classification, feature extraction). In simple terms, image enhancement helps make an image clearer, sharper, and more informative for human eyes or computer algorithms. Purpose of Image Enhancement To improve visual appearance of images. To highlight specific features such as roads, rivers, vegetation, or built-up areas. To enhance contrast or brightness for better differentiation. To reduce noise or remove distortions. To prepare images for further processing like classification or edge detection. Common Image Enhancement Operations Image Reduction: Decreases the size or resolution of an image. Useful for faster processing or overview visualization. Image Mag...

QGIS Buffers

Atmospheric Correction

It is the process of removing the influence of the atmosphere from remotely sensed images so that the data accurately represent the true reflectance of Earth's surface . When a satellite sensor captures an image, the radiation reaching the sensor is affected by gases, water vapor, aerosols, and dust in the atmosphere. These factors scatter and absorb light, changing the brightness and color of the features seen in the image. Although these atmospheric effects are part of the recorded signal, they can distort surface reflectance values , especially when images are compared across different dates or sensors . Therefore, corrections are necessary to make data consistent and physically meaningful. 🔹 Why Do We Need Atmospheric Correction? To retrieve true surface reflectance – It separates the surface signal from atmospheric influence. To ensure comparability – Enables comparing images from different times, seasons, or sensors. To improve visual quality – Remo...