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Home/PGCGI/Page 7

Abstract Classes Latest Questions

Himanshu Kulshreshtha
Himanshu KulshreshthaElite Author
Asked: March 9, 2024In: PGCGI

Define QuickBird and IKONOS.

Define QuickBird and IKONOS.

MGY-002
  1. Himanshu Kulshreshtha Elite Author
    Added an answer on March 9, 2024 at 1:00 pm

    QuickBird: QuickBird is a high-resolution Earth observation satellite that was part of the DigitalGlobe constellation. Launched on October 18, 2001, QuickBird was known for its advanced imaging capabilities, providing very high spatial resolution imagery for a variety of applications. Some key featuRead more

    QuickBird:

    QuickBird is a high-resolution Earth observation satellite that was part of the DigitalGlobe constellation. Launched on October 18, 2001, QuickBird was known for its advanced imaging capabilities, providing very high spatial resolution imagery for a variety of applications. Some key features of QuickBird include:

    1. Spatial Resolution: QuickBird was equipped with a panchromatic sensor capable of capturing imagery with a spatial resolution of 61 centimeters (cm). This high spatial resolution allowed for detailed mapping and analysis of urban areas, infrastructure, and natural landscapes.

    2. Multispectral Imaging: In addition to the panchromatic sensor, QuickBird had a multispectral sensor with a spatial resolution of 2.44 meters. The multispectral bands included blue, green, red, and near-infrared, enabling the satellite to capture imagery in different parts of the electromagnetic spectrum.

    3. Applications: QuickBird's high-resolution imagery found applications in urban planning, environmental monitoring, disaster response, agriculture, and defense. The detailed and accurate imagery supported various industries and government agencies in making informed decisions.

    4. Orbit: QuickBird operated in a sun-synchronous orbit, ensuring consistent lighting conditions across its imaging swaths during its passes over the Earth's surface.

    IKONOS:

    IKONOS was one of the pioneering commercial Earth observation satellites and the first to provide high-resolution satellite imagery to the public. Launched on September 24, 1999, by Space Imaging, IKONOS played a crucial role in advancing the field of commercial satellite imagery. Key characteristics of IKONOS include:

    1. Spatial Resolution: IKONOS was renowned for its high spatial resolution, capturing panchromatic imagery with a resolution of 0.82 meters. This level of detail allowed for the identification of small objects and features on the Earth's surface.

    2. Multispectral Imaging: The satellite featured a multispectral sensor with a spatial resolution of 3.2 meters. The multispectral bands included blue, green, red, and near-infrared, providing valuable information for land cover classification and environmental monitoring.

    3. Applications: IKONOS imagery found applications in urban planning, agriculture, forestry, disaster management, and defense. The high-resolution and multispectral capabilities made it a valuable asset for a wide range of industries and government agencies.

    4. Orbit: Similar to QuickBird, IKONOS operated in a sun-synchronous orbit, ensuring consistent lighting conditions and facilitating accurate and repeatable observations.

    Both QuickBird and IKONOS significantly contributed to the commercial Earth observation market by providing high-quality satellite imagery for various applications. While they have been succeeded by newer satellite systems with even higher resolutions, their role in advancing remote sensing technologies and applications remains noteworthy.

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Himanshu Kulshreshtha
Himanshu KulshreshthaElite Author
Asked: March 9, 2024In: PGCGI

Define Spectral resolution.

Define Spectral resolution.

MGY-002
  1. Himanshu Kulshreshtha Elite Author
    Added an answer on March 9, 2024 at 12:59 pm

    Spectral resolution is a key characteristic of remote sensing systems that refers to the ability of a sensor to distinguish and capture details within different wavelength bands of the electromagnetic spectrum. It quantifies the precision with which a sensor can discern variations in radiation intenRead more

    Spectral resolution is a key characteristic of remote sensing systems that refers to the ability of a sensor to distinguish and capture details within different wavelength bands of the electromagnetic spectrum. It quantifies the precision with which a sensor can discern variations in radiation intensity at different wavelengths, allowing for the identification of unique spectral signatures associated with various materials and features on the Earth's surface.

    Several aspects define spectral resolution:

    1. Number of Bands:

      • Spectral resolution is often described by the number and width of spectral bands in which a sensor can collect data. A sensor with high spectral resolution captures data across numerous narrow bands, providing detailed information about the specific wavelengths at which radiation is measured.
    2. Bandwidth:

      • Bandwidth refers to the range of wavelengths covered by each spectral band. Sensors with narrow bandwidths can discriminate between subtle spectral differences, while those with broader bandwidths capture a more extensive range of wavelengths but with lower spectral specificity.
    3. Spectral Channels:

      • Each spectral band or channel corresponds to a specific range of wavelengths. Sensors with higher spectral resolution have more channels, allowing for a finer subdivision of the electromagnetic spectrum. This enables detailed characterization of surface features, vegetation health, and other environmental parameters.
    4. Spectral Sensitivity:

      • Spectral resolution also considers the sensitivity of a sensor to different wavelengths. A high-resolution sensor is more sensitive to small variations in spectral characteristics, providing the ability to differentiate between subtle differences in the reflectance or emission properties of various materials.
    5. Applications:

      • The spectral resolution of remote sensing instruments is crucial for applications such as land cover classification, vegetation analysis, mineral identification, and environmental monitoring. Different materials exhibit unique spectral signatures, and higher spectral resolution enhances the capability to discriminate between them.
    6. Spatial and Temporal Resolution Trade-offs:

      • There is often a trade-off between spectral, spatial, and temporal resolutions in remote sensing systems. Increasing spectral resolution may lead to a reduction in spatial or temporal resolution and vice versa, depending on the design and specifications of the sensor.
    7. Hyperspectral Imaging:

      • Hyperspectral sensors provide extremely high spectral resolution, capturing data in numerous narrow bands across the electromagnetic spectrum. This technology is particularly valuable for detailed material identification and analysis, offering a wealth of spectral information for each pixel in an image.

    In summary, spectral resolution is a critical factor in remote sensing that influences the level of detail and discrimination capabilities of a sensor. It plays a pivotal role in extracting meaningful information about Earth's surface characteristics, supporting a wide range of applications in fields such as agriculture, forestry, geology, and environmental science.

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Himanshu Kulshreshtha
Himanshu KulshreshthaElite Author
Asked: March 9, 2024In: PGCGI

Define INSAT series.

Define INSAT series.

MGY-002
  1. Himanshu Kulshreshtha Elite Author
    Added an answer on March 9, 2024 at 12:58 pm

    The Indian National Satellite System (INSAT) is a series of multipurpose geostationary satellites operated by the Indian Space Research Organisation (ISRO). The INSAT series plays a pivotal role in providing various communication, broadcasting, meteorological, and search and rescue services to meetRead more

    The Indian National Satellite System (INSAT) is a series of multipurpose geostationary satellites operated by the Indian Space Research Organisation (ISRO). The INSAT series plays a pivotal role in providing various communication, broadcasting, meteorological, and search and rescue services to meet the diverse needs of India and the surrounding region.

    Key features and aspects of the INSAT series include:

    1. Geostationary Orbit:

      • The INSAT satellites are positioned in geostationary orbit, approximately 35,786 kilometers above the equator. This orbit allows the satellites to remain fixed relative to a specific geographic location on Earth, ensuring continuous coverage of the designated service area.
    2. Multipurpose Functionality:

      • INSAT satellites are designed to serve multiple functions, including telecommunications, broadcasting, meteorology, and disaster warning. This multipurpose approach maximizes the utility of the satellite constellation for various sectors.
    3. Telecommunications:

      • INSAT satellites provide a vital communication infrastructure, supporting telecommunication services, broadcasting, and broadband connectivity across India. These satellites play a crucial role in connecting remote and rural areas, contributing to the country's digital communication network.
    4. Broadcasting:

      • The INSAT series facilitates direct-to-home (DTH) broadcasting, enabling the transmission of television signals to households across the country. It has significantly expanded the reach of broadcasting services, offering a wide range of channels to viewers.
    5. Meteorological Services:

      • INSAT satellites contribute to meteorological observations and weather forecasting. They are equipped with advanced sensors and instruments to monitor weather patterns, gather atmospheric data, and support early warning systems for extreme weather events.
    6. Search and Rescue:

      • Some satellites in the INSAT series are equipped with search and rescue transponders to assist in locating and rescuing people in distress, particularly in maritime emergencies. These capabilities enhance India's search and rescue operations.
    7. Satellite-Based Mobile Communication:

      • INSAT satellites have been instrumental in supporting satellite-based mobile communication services. This helps in extending mobile network coverage to remote and inaccessible areas, providing connectivity in challenging terrains.
    8. Technological Advancements:

      • The INSAT series has evolved over time with technological advancements. The later generations of INSAT satellites incorporate improved features, enhanced payloads, and upgraded communication capabilities to meet the growing demands of modern communication and information services.
    9. INSAT System Expansion:

      • Over the years, the INSAT series has been augmented by additional satellite constellations, such as the GSAT (Geostationary Satellite) series, which further expands India's capabilities in communication and broadcasting.

    In conclusion, the INSAT series stands as a cornerstone of India's space program, providing a comprehensive satellite infrastructure for communication, broadcasting, meteorology, and search and rescue services. The continuous development and deployment of these satellites underscore India's commitment to leveraging space technology for national development and societal welfare.

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Himanshu Kulshreshtha
Himanshu KulshreshthaElite Author
Asked: March 9, 2024In: PGCGI

Define Image histogram.

Define Image histogram.

MGY-002
  1. Himanshu Kulshreshtha Elite Author
    Added an answer on March 9, 2024 at 12:57 pm

    An image histogram is a graphical representation of the distribution of pixel intensity values within a digital image. It provides a visual summary of the image's tonal or color characteristics, allowing for a quick assessment of the image's overall brightness, contrast, and distribution oRead more

    An image histogram is a graphical representation of the distribution of pixel intensity values within a digital image. It provides a visual summary of the image's tonal or color characteristics, allowing for a quick assessment of the image's overall brightness, contrast, and distribution of colors. The histogram displays the frequency of occurrence of different intensity levels in the image, ranging from dark to bright (for grayscale images) or from low to high for each color channel (for color images).

    Here are key elements and concepts associated with image histograms:

    1. X-axis and Y-axis:

      • The x-axis of the histogram represents the possible intensity values, ranging from 0 (black) to 255 (white) for an 8-bit grayscale image. For color images, separate histograms are generated for each color channel (e.g., red, green, blue), and the x-axis represents the intensity values for that specific channel. The y-axis represents the frequency or the number of pixels with a particular intensity value.
    2. Intensity Levels:

      • Each pixel in a digital image has an associated intensity level based on its brightness or color. In grayscale images, the intensity level varies from 0 (black) to 255 (white), while color images have intensity levels for each color channel.
    3. Peak and Valley Analysis:

      • Peaks and valleys in the histogram indicate the prevalence of specific intensity values in the image. Peaks correspond to dominant tones or colors, while valleys represent areas with lower frequency. A well-distributed histogram with balanced peaks and valleys suggests a good range of tonal or color variation in the image.
    4. Contrast and Brightness:

      • Histograms are useful for assessing the overall contrast and brightness of an image. A histogram skewed toward the left may indicate underexposure and dark tones, while a histogram skewed toward the right may suggest overexposure and bright tones.
    5. Color Channels:

      • In color images, separate histograms are generated for each color channel (red, green, blue). Analyzing the histograms of individual channels helps understand the color composition and balance in the image.
    6. Applications:

      • Image histograms are widely used in image processing, computer vision, and photography. They help in adjusting image exposure, enhancing contrast, identifying color balance issues, and assessing the overall quality of an image.

    Understanding and analyzing the histogram of an image is a valuable tool for photographers, image analysts, and graphic designers. It provides insights into the distribution of pixel intensities, allowing for informed adjustments to enhance the visual quality and characteristics of the image.

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Himanshu Kulshreshtha
Himanshu KulshreshthaElite Author
Asked: March 9, 2024In: PGCGI

Explain Visual image interpretation.

Explain Visual image interpretation.

MGY-002
  1. Himanshu Kulshreshtha Elite Author
    Added an answer on March 9, 2024 at 12:55 pm

    Visual image interpretation is a process of extracting meaningful information from images through the visual examination and analysis of their features. It is a fundamental method in remote sensing and geospatial analysis, allowing analysts to interpret and derive insights from satellite or aerial iRead more

    Visual image interpretation is a process of extracting meaningful information from images through the visual examination and analysis of their features. It is a fundamental method in remote sensing and geospatial analysis, allowing analysts to interpret and derive insights from satellite or aerial imagery without relying on automated algorithms. This technique involves the human interpretation of visual cues and patterns present in the imagery. Here are key aspects of visual image interpretation:

    1. Image Features:
      Visual image interpretation relies on the identification and analysis of various features within an image. These features include land cover types (such as vegetation, water bodies, and urban areas), natural and man-made structures, patterns, and anomalies.

    2. Human Perception:
      The process leverages human perception and cognitive abilities to recognize and interpret visual patterns. Analysts use their knowledge of geography, land cover characteristics, and contextual information to identify and classify objects and features in the imagery.

    3. Training and Expertise:
      Effective visual interpretation requires training and expertise in understanding different land cover types, recognizing distinctive spectral signatures, and interpreting the significance of specific spatial patterns. Analysts often undergo specialized training to enhance their interpretative skills.

    4. Use of Stereoscopic Vision:
      Stereoscopic image interpretation involves viewing pairs of overlapping images to create a three-dimensional effect. This technique helps analysts discern terrain elevation, identify land features more accurately, and improve their ability to interpret complex landscapes.

    5. Applications:
      Visual image interpretation finds applications in various fields such as agriculture, forestry, urban planning, environmental monitoring, and disaster management. Analysts can assess land cover changes, monitor deforestation, identify crop health, and detect urban expansion, among other applications.

    6. Advancements and Technology:
      While automated image analysis techniques are gaining prominence, visual interpretation remains valuable, especially in situations where human expertise is crucial. Modern tools, including geographic information systems (GIS) and specialized software, assist analysts in visualizing and annotating imagery, enhancing the interpretation process.

    7. Challenges:
      Visual image interpretation is subject to challenges such as atmospheric conditions, image resolution limitations, and the complexity of certain landscapes. Overcoming these challenges requires experience and a comprehensive understanding of the factors influencing image interpretation.

    In summary, visual image interpretation involves the manual examination and analysis of satellite or aerial imagery to derive meaningful information about the Earth's surface. This method leverages human cognitive abilities and expertise to recognize patterns, features, and changes, making it a valuable tool in various fields that rely on accurate and context-rich spatial information.

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Himanshu Kulshreshtha
Himanshu KulshreshthaElite Author
Asked: March 9, 2024In: PGCGI

Define Scattering.

Define Scattering.

MGY-002
  1. Himanshu Kulshreshtha Elite Author
    Added an answer on March 9, 2024 at 12:54 pm

    Scattering, in the context of physics and optics, refers to the process by which particles or waves deviate from their original trajectory when they encounter an obstacle or interact with other particles. This phenomenon is fundamental to various fields, including electromagnetic waves, acoustics, aRead more

    Scattering, in the context of physics and optics, refers to the process by which particles or waves deviate from their original trajectory when they encounter an obstacle or interact with other particles. This phenomenon is fundamental to various fields, including electromagnetic waves, acoustics, and quantum mechanics.

    In the context of electromagnetic waves, such as light or radio waves, scattering occurs when these waves encounter objects that have dimensions comparable to their wavelength. The interaction leads to a redistribution of the wave energy in different directions. There are three primary types of scattering:

    1. Rayleigh Scattering:

      • Rayleigh scattering occurs when the size of the scattering particles is much smaller than the wavelength of the incident waves. It is responsible for the blue color of the sky during the day. The shorter wavelengths of sunlight are scattered more efficiently by the smaller atmospheric particles, causing the sky to appear blue.
    2. Mie Scattering:

      • Mie scattering occurs when the size of the scattering particles is comparable to the wavelength of the incident waves. This type of scattering is more prevalent with larger particles, such as water droplets in clouds or dust particles in the atmosphere. Unlike Rayleigh scattering, Mie scattering does not strongly favor shorter wavelengths, resulting in a more diffuse scattering pattern.
    3. Non-Selective Scattering:

      • Non-selective or geometric scattering occurs when the size of the scattering particles is much larger than the wavelength of the incident waves. In this case, the scattering is independent of wavelength, and the intensity of the scattered light is relatively uniform across the spectrum.

    Scattering phenomena are not limited to electromagnetic waves; they also occur with other types of waves, such as acoustic waves or particles in quantum mechanics. In acoustics, scattering can be observed when sound waves encounter obstacles or irregularities in a medium, leading to the redirection of sound energy.

    Understanding scattering is crucial in various scientific disciplines and has practical applications. For example, in remote sensing, the analysis of scattered light can provide information about the composition and characteristics of the scattering medium. Additionally, the study of scattering plays a vital role in fields like atmospheric science, astronomy, and material science, contributing to our comprehension of wave interactions in different environments.

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Himanshu Kulshreshtha
Himanshu KulshreshthaElite Author
Asked: March 9, 2024In: PGCGI

What is radiometric error? Describe various techniques used to remove radiometric errors from a remote sensing image.

What does radiometric error mean? Give an explanation of the many methods used to eliminate radiometric inaccuracies from a remote sensing image.

MGY-002
  1. Himanshu Kulshreshtha Elite Author
    Added an answer on March 9, 2024 at 12:53 pm

    Radiometric Error in Remote Sensing: Radiometric errors in remote sensing refer to inaccuracies or variations in the recorded intensity values of electromagnetic radiation across the different spectral bands of an image. These errors can result from sensor characteristics, atmospheric conditions, orRead more

    Radiometric Error in Remote Sensing:

    Radiometric errors in remote sensing refer to inaccuracies or variations in the recorded intensity values of electromagnetic radiation across the different spectral bands of an image. These errors can result from sensor characteristics, atmospheric conditions, or processing issues, leading to inconsistencies in the radiometric information captured by the sensor. Correcting radiometric errors is essential for ensuring the accuracy and reliability of quantitative analysis and interpretation of remote sensing data.

    Techniques to Remove Radiometric Errors:

    1. Radiometric Calibration:

      • Radiometric calibration is a fundamental step to correct sensor-specific radiometric errors. It involves establishing a relationship between the recorded digital numbers (DN) in an image and the corresponding physical radiance values. Calibration coefficients are applied to convert DN values to radiance, ensuring consistency across different scenes and sensors.
    2. Histogram Matching:

      • Histogram matching is a technique used to adjust the distribution of pixel values in an image. By aligning the histograms of different spectral bands or images, this method helps in normalizing radiometric variations. It ensures that images captured under different conditions or sensors have similar statistical properties, facilitating meaningful comparisons.
    3. Flat-Field Correction:

      • Flat-field correction is employed to compensate for spatial variations in sensor sensitivity. It involves dividing each pixel value in an image by a corresponding pixel value in a flat-field image, which represents a uniform scene. This correction helps in mitigating radiometric variations caused by sensor sensitivity differences across the image.
    4. Atmospheric Correction:

      • Atmospheric correction addresses radiometric errors caused by the absorption and scattering of electromagnetic radiation by the Earth's atmosphere. Various models, such as the Dark Object Subtraction (DOS) or the Fast Line-of-Sight Atmospheric Analysis of Hypercubes (FLAASH), estimate and remove atmospheric effects, enhancing the accuracy of radiometric information.
    5. Relative Radiometric Normalization:

      • Relative radiometric normalization involves adjusting the radiometric values of an image to make them comparable with another image captured under different conditions. This technique is particularly useful for time-series analysis, where consistent radiometric values across different scenes are essential. Common methods include histogram matching and statistical normalization.
    6. Cross-Calibration:

      • Cross-calibration involves comparing radiometric measurements from one sensor with those of a well-calibrated reference sensor. By establishing a relationship between the sensors, cross-calibration helps in reducing radiometric discrepancies and ensuring consistency in the radiometric information derived from different sensors.
    7. Sensor Gain and Offset Adjustment:

      • Some radiometric errors may arise from variations in sensor gain and offset settings. Adjusting these parameters during image processing helps in normalizing pixel values and ensuring consistency in radiometric information.
    8. Top-of-Atmosphere (TOA) Reflectance Conversion:

      • Converting digital numbers to top-of-atmosphere reflectance values standardizes the radiometric information in remote sensing data. This conversion corrects for variations in illumination conditions, sun angle, and sensor geometry, facilitating accurate radiometric analysis.
    9. Noise Reduction Techniques:

      • Radiometric errors can be exacerbated by noise in remote sensing images. Various noise reduction techniques, such as filtering or mathematical operations like averaging, help in smoothing out random variations and improving the overall radiometric quality of the image.
    10. Use of Calibration Targets:

      • Deploying on-ground calibration targets with known reflectance values assists in calibrating and validating remote sensing data. These targets can be used to assess and correct radiometric errors, ensuring the accuracy of the derived information.

    In conclusion, addressing radiometric errors is critical for maintaining the reliability and quantitative integrity of remote sensing data. These techniques collectively contribute to the normalization, correction, and calibration of radiometric information, enabling accurate and consistent analysis for applications such as land cover mapping, change detection, and environmental monitoring. The selection of specific techniques depends on the nature of the radiometric errors present and the objectives of the remote sensing analysis.

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Himanshu Kulshreshtha
Himanshu KulshreshthaElite Author
Asked: March 9, 2024In: PGCGI

What is ground truth data? Give an account of ground truth data collection.

What is ground truth data? Give an account of ground truth data collection.  

MGY-002
  1. Himanshu Kulshreshtha Elite Author
    Added an answer on March 9, 2024 at 12:52 pm

    Ground Truth Data: Ground truth data refers to real-world, on-site information that serves as a reliable reference for validating or calibrating remotely sensed data. In remote sensing, it is crucial to compare and verify the accuracy of data collected from satellites, aerial platforms, or other senRead more

    Ground Truth Data:

    Ground truth data refers to real-world, on-site information that serves as a reliable reference for validating or calibrating remotely sensed data. In remote sensing, it is crucial to compare and verify the accuracy of data collected from satellites, aerial platforms, or other sensors with actual conditions on the ground. Ground truth data provides a means to assess the reliability and precision of remote sensing observations, aiding in the interpretation and validation of satellite imagery or sensor outputs.

    Ground Truth Data Collection:

    The process of collecting ground truth data involves acquiring accurate, detailed information about the physical properties, features, or conditions of the Earth's surface at specific locations. Here's an account of ground truth data collection:

    1. Field Surveys:

      • Field surveys involve physically visiting the locations of interest to collect direct measurements and observations. Ground truth data collected during field surveys provide accurate and current information about land cover, land use, topography, vegetation types, and other relevant features. Surveyors may use GPS devices, cameras, and other tools to document conditions on-site.
    2. GPS Measurements:

      • Global Positioning System (GPS) technology is commonly employed in ground truth data collection. GPS receivers provide precise location coordinates, allowing surveyors to accurately document the geographic coordinates of specific features. This information aids in georeferencing and validating remote sensing data.
    3. Photographic Documentation:

      • Photographs taken on-site serve as valuable ground truth data. High-resolution images capture visual details of land cover, vegetation, and terrain features. Photographs can be used for visual interpretation, comparison with satellite imagery, and documentation of changes over time.
    4. Field Spectroscopy:

      • Field spectroscopy involves measuring the spectral reflectance of materials on the ground using handheld spectroradiometers. These devices capture the electromagnetic radiation reflected or emitted by surfaces in different wavelengths. Spectroscopic measurements provide detailed information about the spectral characteristics of ground features, aiding in the calibration of remote sensing data.
    5. Soil Sampling:

      • Soil samples collected from the ground provide information about soil composition, moisture content, and other soil properties. This data is essential for calibrating remote sensing observations related to soil conditions, agriculture, and land management.
    6. Vegetation Sampling:

      • Ground truth data collection often includes vegetation sampling to assess species composition, biomass, and health. Techniques such as quadrat sampling, transect surveys, and vegetation density measurements contribute to a comprehensive understanding of vegetation characteristics.
    7. Meteorological Measurements:

      • Meteorological data collected at ground stations contribute to the validation of atmospheric conditions observed in remote sensing data. Measurements of temperature, humidity, wind speed, and other meteorological parameters help calibrate atmospheric correction algorithms applied to satellite imagery.
    8. Permanent Ground Control Points (GCPs):

      • Permanent GCPs are precisely located points on the Earth's surface with known coordinates. These points serve as reference markers for georeferencing satellite or aerial imagery. Ground truth data related to permanent GCPs is collected and maintained to ensure accurate spatial referencing in remote sensing applications.
    9. Temporal Data Collection:

      • Ground truth data collection is often conducted at multiple time points to capture seasonal variations, changes in land cover, and dynamic environmental conditions. Temporal data enhance the understanding of Earth's dynamics and contribute to the validation of time-series satellite observations.
    10. Collaborative Citizen Science:

      • Citizen science initiatives involve engaging the public in ground truth data collection. Volunteers or community members contribute to data collection efforts, providing valuable information about local conditions, biodiversity, and environmental changes.

    In summary, ground truth data collection is a crucial step in the remote sensing workflow. It involves obtaining accurate and reliable information directly from the Earth's surface to validate, calibrate, and interpret remotely sensed data. The integration of ground truth data enhances the accuracy and reliability of remote sensing applications across various fields, including environmental monitoring, agriculture, land use planning, and disaster management.

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Himanshu Kulshreshtha
Himanshu KulshreshthaElite Author
Asked: March 9, 2024In: PGCGI

Explain the platforms used in remote sensing and orbits.

Explain the platforms used in remote sensing and orbits.  

MGY-002
  1. Himanshu Kulshreshtha Elite Author
    Added an answer on March 9, 2024 at 12:50 pm

    Remote sensing involves the acquisition of information about the Earth's surface from a distance, typically using sensors mounted on various platforms. These platforms can be airborne or spaceborne, and they follow specific orbits to capture data systematically. Understanding the characteristicRead more

    Remote sensing involves the acquisition of information about the Earth's surface from a distance, typically using sensors mounted on various platforms. These platforms can be airborne or spaceborne, and they follow specific orbits to capture data systematically. Understanding the characteristics of these platforms and their orbits is crucial for effective remote sensing applications. Let's explore the platforms used in remote sensing and the associated orbits:

    1. Platforms Used in Remote Sensing:

    a. Airborne Platforms:

    • Aircraft: Airborne remote sensing platforms involve the deployment of sensors on aircraft. These can range from small unmanned aerial vehicles (UAVs) to large manned aircraft. Airborne platforms offer flexibility in terms of data acquisition and can be deployed on demand for specific missions. They are commonly used for high-resolution imaging, surveillance, and rapid response to events.

    • Helicopters: Helicopters provide a stable platform for remote sensing applications, allowing for hovering and low-altitude flights. They are suitable for tasks like aerial photography, urban mapping, and environmental monitoring.

    b. Spaceborne Platforms:

    • Satellites: Satellites are the primary spaceborne platforms for remote sensing. They orbit the Earth and carry various sensors to capture data across the electromagnetic spectrum. Satellites are categorized into different types based on their orbits, such as low Earth orbit (LEO), medium Earth orbit (MEO), and geostationary orbit (GEO). They offer global coverage, systematic data collection, and long-term monitoring capabilities.

    • Space Stations: While not dedicated to remote sensing, space stations like the International Space Station (ISS) occasionally capture imagery for scientific purposes. The advantage of space stations is their ability to provide continuous observations of specific areas.

    2. Orbits in Remote Sensing:

    a. Low Earth Orbit (LEO):

    • Altitude: 160 to 2,000 kilometers above the Earth's surface.
    • Characteristics:
      • Short orbital periods (around 90 to 120 minutes).
      • High spatial resolution.
      • Suitable for high-resolution imaging and monitoring dynamic processes.
      • Examples: Landsat series, Sentinel-2, and International Space Station.

    b. Medium Earth Orbit (MEO):

    • Altitude: 2,000 to 35,786 kilometers above the Earth's surface.
    • Characteristics:
      • Moderate orbital periods (several hours).
      • Balanced trade-off between spatial and temporal resolution.
      • Suitable for navigation and communication satellites.
      • Examples: Global Navigation Satellite Systems (GNSS) like GPS and GLONASS.

    c. Geostationary Orbit (GEO):

    • Altitude: Approximately 35,786 kilometers above the Equator.
    • Characteristics:
      • Fixed position relative to the Earth's surface.
      • Continuous observation of specific areas.
      • Suitable for meteorological and communication satellites.
      • Longer orbital periods (24 hours).
      • Examples: Geostationary Operational Environmental Satellites (GOES).

    d. Sun-Synchronous Orbit (SSO):

    • Altitude: Varies but typically around 600 to 800 kilometers above the Earth's surface.
    • Characteristics:
      • Maintains a consistent angle between the orbital plane and the Sun.
      • Revisits the same area at the same local solar time.
      • Suitable for imaging missions requiring consistent lighting conditions.
      • Examples: Landsat series, Sentinel-2.

    e. Polar Orbit:

    • Altitude: Varies but typically in the low Earth orbit range.
    • Characteristics:
      • Passes over the Earth's poles.
      • Provides global coverage over time.
      • Suitable for mapping and monitoring applications.
      • Examples: Aqua and Terra satellites.

    f. Highly Elliptical Orbit (HEO):

    • Altitude: Varies with a highly elliptical shape.
    • Characteristics:
      • Combines advantages of LEO and GEO.
      • Suitable for specific Earth observation and communication missions.
      • Examples: Molniya orbits used by some communication satellites.

    g. Molniya Orbit:

    • Altitude: Highly elliptical with apogee over high latitudes.
    • Characteristics:
      • Designed for high-latitude coverage with extended dwell time.
      • Suited for communication and navigation satellites.
      • Examples: Some Russian communication satellites.

    h. Heliocentric Orbit:

    • Orbits the Sun rather than the Earth.
    • Characteristics:
      • Used for solar observation missions.
      • Allows continuous monitoring of the Sun.
      • Examples: Solar and Heliospheric Observatory (SOHO).

    Understanding these platforms and orbits is essential for mission planning, data acquisition, and optimizing the capabilities of remote sensing systems. The choice of platform and orbit depends on the specific objectives of the remote sensing mission, including spatial resolution requirements, revisit frequency, and the nature of the Earth processes being monitored.

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Himanshu Kulshreshtha
Himanshu KulshreshthaElite Author
Asked: March 9, 2024In: PGCGI

What is spectral signature? Describe the spectral signature of vegetation and the factors influencing it. Support your answer with neat well labelled diagrams, wherever required.

Spectral signature: what is it? Explain the vegetation’s spectral signature and the things that affect it. When necessary, include clear, labeled diagrams to support your response.

MGY-002
  1. Himanshu Kulshreshtha Elite Author
    Added an answer on March 9, 2024 at 12:49 pm

    Spectral Signature: A spectral signature is a unique pattern of reflectance or emission of electromagnetic radiation across different wavelengths for a specific material or feature on the Earth's surface. It serves as a distinctive fingerprint that aids in the identification and classificationRead more

    Spectral Signature:

    A spectral signature is a unique pattern of reflectance or emission of electromagnetic radiation across different wavelengths for a specific material or feature on the Earth's surface. It serves as a distinctive fingerprint that aids in the identification and classification of various land cover types in remote sensing applications. The spectral signature of an object is derived from its interaction with sunlight or other electromagnetic sources, and it can be represented graphically by plotting reflectance values at different wavelengths.

    Spectral Signature of Vegetation:

    The spectral signature of vegetation exhibits distinct characteristics across different regions of the electromagnetic spectrum. Generally, vegetation has a unique pattern due to its absorption and reflection properties, which are influenced by the presence of chlorophyll and other pigments. The following factors contribute to the spectral signature of vegetation:

    1. Visible Spectrum:

      • In the visible spectrum (400 to 700 nanometers), vegetation strongly absorbs light in the blue and red wavelengths while reflecting strongly in the green. This results in the characteristic green appearance of healthy vegetation in true-color images. The spectral signature in this range typically shows low reflectance in the blue and red bands and high reflectance in the green band.
    2. Near-Infrared (NIR) Spectrum:

      • Vegetation strongly reflects near-infrared radiation (700 to 1300 nanometers) due to the cellular structure and high water content in plant leaves. Healthy vegetation exhibits a peak in reflectance in the near-infrared region. This distinctive feature is crucial for vegetation health monitoring and classification. The spectral signature in the near-infrared range is characterized by a sharp increase in reflectance.
    3. Red-Edge Spectrum:

      • The red-edge portion of the spectrum (around 700 to 750 nanometers) is particularly sensitive to chlorophyll absorption and is valuable for discriminating between different vegetation types and assessing vegetation health. The spectral signature in the red-edge region shows a characteristic plateau or inflection point related to the chlorophyll absorption.

    Factors Influencing the Spectral Signature of Vegetation:

    1. Leaf Pigments:

      • Chlorophyll, the primary pigment responsible for photosynthesis, strongly influences the spectral signature of vegetation. The absorption and reflection properties of chlorophyll in the visible and near-infrared regions contribute to the unique spectral features of healthy vegetation.
    2. Leaf Structure:

      • The internal structure of plant leaves affects how light interacts with vegetation. The presence of air spaces, cell structure, and leaf arrangement influence the reflectance patterns at different wavelengths. Dense and healthy vegetation tends to have a higher NIR reflectance due to the cellular structure.
    3. Water Content:

      • Water content in vegetation strongly influences the spectral signature, especially in the shortwave infrared (SWIR) region. Changes in water content can impact the absorption features in the SWIR spectrum, providing information about vegetation stress or water availability.
    4. Canopy Structure:

      • The overall structure of the vegetation canopy, including factors like canopy density and arrangement of leaves, affects how light penetrates and interacts with the vegetation. These factors influence the spectral signature, particularly in terms of the amount of sunlight reaching the ground and being reflected back.
    5. Physiological Conditions:

      • The physiological condition of vegetation, such as its health, stress levels, and growth stage, can influence the spectral signature. Healthy vegetation typically exhibits a distinctive spectral response, while stressed or diseased vegetation may show variations in the reflectance patterns.

    Diagram:

    Here's a simplified diagram illustrating the typical spectral signature of vegetation:

    Spectral Signature of Vegetation

    In this diagram:

    • The x-axis represents the wavelength of electromagnetic radiation.
    • The y-axis represents the reflectance values.
    • The graph shows characteristic dips in the blue and red bands, corresponding to chlorophyll absorption, and a peak in the near-infrared region due to strong reflection.

    Understanding the spectral signature of vegetation is essential for remote sensing applications, including vegetation mapping, land cover classification, and monitoring environmental changes. The distinct patterns in reflectance across different spectral bands allow for the discrimination of various vegetation types and provide valuable information about the health and condition of ecosystems.

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