Skip to main content

Raster Data Analysis. GIS

Raster data analysis is a fundamental aspect of GIS that involves working with data represented in a grid-based format known as raster data. Raster data consists of a series of cells or pixels, where each cell represents a value or attribute associated with a specific location on the Earth's surface.

In GIS, raster data analysis refers to the process of manipulating, extracting information, and deriving new insights from raster datasets. This type of analysis enables us to understand spatial patterns, perform calculations, and make informed decisions based on the values within the raster cells.

There are several tools and techniques available for raster data analysis in GIS software. Here are some commonly used ones:

1. Raster Calculator: This tool allows you to perform mathematical operations on raster datasets, such as addition, subtraction, multiplication, and division. It is useful for creating new raster layers by combining or transforming existing ones.

2. Zonal Statistics: Zonal statistics calculates statistics, such as mean, maximum, minimum, or standard deviation, for a specific zone or region defined in a raster dataset. It helps in analyzing and summarizing values within predefined areas of interest.

3. Slope and Aspect Analysis: These tools calculate the slope and aspect of the terrain from elevation raster data. Slope analysis measures the steepness of the land, while aspect analysis determines the orientation or direction of the slope.

4. Reclassification: Reclassification allows you to assign new values or categories to raster cells based on specified criteria. It is helpful in reclassifying continuous data into discrete classes or grouping data for thematic mapping.

5. Density Analysis: Density analysis helps to analyze the concentration or distribution of certain phenomena in a raster dataset. It calculates the density of occurrences within a given area, such as population density or density of crime incidents.

6. Cost Distance Analysis: This tool calculates the least-cost path or distance between locations, considering the cost or resistance values assigned to raster cells. It is commonly used for modeling movement or finding the optimal route based on factors like terrain, land cover, or infrastructure.

7. Suitability Analysis: Suitability analysis assesses the suitability of areas for specific activities or criteria. It involves overlaying multiple raster datasets, assigning weights to each layer, and generating a suitability map to identify areas that meet certain criteria.

These are just a few examples of the numerous raster analysis tools available in GIS software. Each tool serves specific purposes and can be combined to perform complex analyses and generate valuable insights from raster data.

Comments

Popular posts from this blog

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...

Disaster Management

1. Disaster Risk Analysis → Disaster Risk Reduction → Disaster Management Cycle Disaster Risk Analysis is the first step in managing disasters. It involves assessing potential hazards, identifying vulnerable populations, and estimating possible impacts. Once risks are identified, Disaster Risk Reduction (DRR) strategies come into play. DRR aims to reduce risk and enhance resilience through planning, infrastructure development, and policy enforcement. The Disaster Management Cycle then ensures a structured approach by dividing actions into pre-disaster, during-disaster, and post-disaster phases . Example Connection: Imagine a coastal city prone to cyclones: Risk Analysis identifies low-lying areas and weak infrastructure. Risk Reduction includes building seawalls, enforcing strict building codes, and training residents for emergency situations. The Disaster Management Cycle ensures ongoing preparedness, immediate response during a cyclone, and long-term recovery afterw...

Disaster Risk

Disaster Risk 

Evaluation and Characteristics of Himalayas

Time Period Event / Process Geological Evidence Key Terms & Concepts Late Precambrian – Palaeozoic (>541 Ma – ~250 Ma) India part of Gondwana , north bordered by Cimmerian Superterranes, separated from Eurasia by Paleo-Tethys Ocean . Pan-African granitic intrusions (~500 Ma), unconformity between Ordovician conglomerates & Cambrian sediments. Gondwana, Paleo-Tethys Ocean, Pan-African orogeny, unconformity, granitic intrusions, Cimmerian Superterranes. Early Carboniferous – Early Permian (~359 – 272 Ma) Rifting between India & Cimmerian Superterranes → Neotethys Ocean formation. Rift-related sediments, passive margin sequences. Rifting, Neotethys Ocean, passive continental margin. Norian (210 Ma) – Callovian (160–155 Ma) Gondwana split into East & West; India part of East Gondwana with Australia & Antarctica. Rift basins, oceanic crust formation. Continental breakup, East Gondwana, West Gondwana, oceanic crust. Early Cretaceous (130–125 Ma) India broke fr...

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...