Discuss about different types of remote sensing.
Share
Lost your password? Please enter your email address. You will receive a link and will create a new password via email.
Please briefly explain why you feel this question should be reported.
Please briefly explain why you feel this answer should be reported.
Please briefly explain why you feel this user should be reported.
Remote sensing is a technology used to acquire information about the Earth's surface and atmosphere without physical contact. It involves the detection, measurement, and analysis of electromagnetic radiation emitted, reflected, or scattered from objects and features on the Earth's surface. There are various types of remote sensing techniques, each offering unique advantages and applications:
Passive Remote Sensing:
Passive remote sensing relies on the detection of natural radiation emitted or reflected by the Earth's surface and atmosphere. Sensors passively receive radiation without emitting any energy themselves. The most common source of radiation for passive remote sensing is the Sun. Examples of passive remote sensing techniques include:
Active Remote Sensing:
Active remote sensing involves the emission of energy by a sensor and the measurement of the reflected or scattered radiation. Active sensors provide their own source of electromagnetic radiation and measure the energy returned from the Earth's surface. Examples of active remote sensing techniques include:
Hyperspectral Remote Sensing:
Hyperspectral remote sensing involves capturing information across hundreds or even thousands of narrow spectral bands within the electromagnetic spectrum. This high spectral resolution enables detailed characterization and discrimination of surface materials based on their unique spectral signatures. Hyperspectral sensors are valuable for applications such as mineral exploration, environmental monitoring, and precision agriculture.
Multispectral Remote Sensing:
Multispectral remote sensing captures information across several discrete spectral bands within the electromagnetic spectrum. While not as detailed as hyperspectral data, multispectral imagery is still valuable for distinguishing between different land cover types, monitoring vegetation health, and assessing environmental changes over time. Multispectral sensors are commonly used in satellite-based Earth observation systems.
Photogrammetry:
Photogrammetry involves the use of overlapping aerial or satellite images to create three-dimensional models of the Earth's surface. By analyzing the geometric relationships between overlapping images, photogrammetry can accurately measure distances, elevations, and volumes. Photogrammetry is widely used in cartography, urban planning, and infrastructure development.
Microwave Remote Sensing:
Microwave remote sensing utilizes microwave radiation to penetrate through clouds, vegetation, and soil, allowing for observations regardless of weather conditions or time of day. Microwave sensors are particularly useful for monitoring soil moisture, sea surface temperature, and ocean salinity. They are also employed in weather forecasting, climate research, and polar ice monitoring.
In conclusion, remote sensing encompasses a diverse array of techniques for observing and analyzing the Earth's surface and atmosphere. Passive and active remote sensing methods, hyperspectral and multispectral imaging, photogrammetry, and microwave remote sensing each offer unique capabilities and applications across various fields, including environmental monitoring, natural resource management, urban planning, agriculture, and disaster management. The choice of remote sensing technique depends on factors such as spatial resolution requirements, spectral sensitivity, atmospheric conditions, and specific research or application objectives.