Remote sensing is the art and science of recording, measuring, and analyzing information about a phenomenon from a distance. This radiation is just beyond the violet portion of the visible wavelengths, hence its name. Humans accomplish this task with aid of eyes or by the sense of smell or hearing; so, remote sensing is day-today business for people. Although, the remote sensing includes a wide array of technologies and types, but they all are based on certain common concepts with the same basic components. This radiation is just beyond the violet … There are several regions of the electromagnetic spectrum which are useful for remote sensing. from different regions of electromagnetic spectrum viz., visible, infrared, thermal and microwave regions. This remote sensing method is known as Passive Remote sensing. Optical remote sensing satellites use reflected light to detect electromagnetic energy on the Earth’s surface. For most purposes, the ultraviolet or UV portion of the spectrum has the shortest wavelengths which are practical for remote sensing. Electromagnetic radiation and Electromagnetic spectrum. http://lasp.colorado.edu/cassini/education/Electromagnetic%20Spectrum.htm. Different objects return different amount of energy in different bands … Published Sep 17, 1999. Remote Sensing. Electromagnetic spectrum (EMS) represents the continuum of electromagnetic radiation (EMR) arranged on the basis of wavelengths or frequency. The visible region of the electromagnetic spectrum is from about 400 nm to about 700 nm. Electromagnetic Spectrum. Remote sensing data is useful in obtaining up-to-date land use pattern of large areas at any given time and also monitor changes that occur from time to time. In most of the cases, the Source of energy is the Sun. The interpretation of image can be done visually or electronically with the help of computers and image processing softwares. 2. This radiation is just beyond the violet portion of the visible wavelengths, hence its name. Violet: 0.4 - 0.446 µmBlue: 0.446 - 0.500 µmGreen: 0.500 - 0.578 µmYellow: 0.578 - 0.592 µmOrange: 0.592 - 0.620 µmRed: 0.620 - 0.7 µm. It suggests that EMR is composed of many discrete units called photons/quanta. The sun, being a major source of energy, radiation and illumination, allows capturing reflected light with conventional cameras and films. When solar energy strikes an object or molecules of the atmosphere/hydrosphere, many types of interaction are possible. The image is then interpreted to extract the informations about target. Sensors detect and measure electromagnetic energy in different portions of the spectrum. It is also used to warn people about impending cyclones. Wavelength Regions of Electromagnetic Spectrum used in Remote Sensing. electromagnetic spectrum –. The energy source illuminates or provides electromagnetic energy to the target. The light which our eyes can detect forms the visible spectrum. The sun radiates electro-magnetic energy with a peak wavelength of 0.5 μm. Remote sensing data obtained in the visible and reflective infrared regions mainly depends on the reflectance of objects on the ground … Because of the special nature of this region and its importance to remote sensing in Canada, an entire chapter (Chapter 3) of the tutorial is dedicated to microwave sensing. • EMR is a dynamic form of energy. The basic components of remote sensing system are given below: The target is the object or material being studied. The energy of photon is. All these technologies are integrated to act as one complete system in itself, known as Remote Sensing System. Sensors are also used to measure the given-off energy or emitted energy by the target; reflected-off energy of the target; or transmitted energy from the target. For enquiries, contact us. Although many characteristics of EM energy are easily described by wave theory, another theory known as particle theory offers insight into how electromagnetic energy interacts with matter. This is important since most natural EMR sources have very broad power spectra. Also mention the important functions performed by the committee. The most important and primary requirement for any remote sensing process is to have an energy source. The electromagnetic spectrum ranges from the shorter wavelengths (including gamma and x-rays) to the longer wavelengths (including microwaves and broadcast radio waves). Remote sensing can be used to study damages caused by earthquakes, volcanoes, landslides, floods and melting of ice in polar regions. Different objects return different amount of energy in different bands of the electromagnetic spectrum, incident upon it. But no photographic films exist to directly record emissive infrared (heat). The Source of energy which illuminates or provides electromagnetic energy to the target of interest. This information is used by regional planners and administrators to frame policy matters for all-round development of the region. They are defined as such because no single primary colour can be created from the other two, but all other colours can be formed by combining blue, green, and red in various proportions. The thermal IR region is quite different than the visible and reflected IR portions, as this energy is essentially the radiation that is emitted from the Earth's surface in the form of heat. It is important to recognize how small the visible portion is relative to the rest of the spectrum. One μm is about .00003937 inch and 1 μm equals 1,000 nm. [ Figure 1 - Text Version] For most purposes, the ultraviolet or UV portion of the spectrum has the shortest wavelengths which are practical for remote sensing. However there are a number of electronic devices which detect and record thermal infrared images. Electro-optical remote sensing involves the acqui-sition of information about an object or scene with-out coming into physical contact with that object or scene. The energy is: • The whole range of EMR is called spectrum. These important terms are further explained in the course textbook. The energy interaction with the target depends on the target properties and the radiation. GPSC Prelims and Mains Notes, GPSC Test Series, Remote sensing: principles, electromagnetic spectrum, components and applications. There are several regions of the electromagnetic spectrum which are useful for remote sensing. Current bathymetric and ice LIDAR generally uses green light (e.g., NASA’s HSRL-1 LIDAR, with a spectrum of 532 nm). A good number of studies carried over nearly three decades testifies the role of remote sensing in soil related studies. The Remote Sensing is basically a multi-disciplinary science which includes a combination of various disciplines such as optics, spectroscopy, photography, computer, electronics and telecommunication, satellite launching etc. The portion of the spectrum of more recent interest to remote sensing is the microwave region from about 1 mm to 1 m. This covers the longest wavelengths used for remote sensing. • EMR is characterized by wavelength and frequency. Different This depends on the property of material (structural, chemical, and physical), surface roughness, angle of incidence, intensity, and wavelength of radiant energy. The wavelengths used in most agricultural remote sensing applications cover only a small region of the electromagnetic spectrum. Hue and saturation are independent characteristics of colour. • The foundation of remote sensing technology is based on the measurement and interpretation of the patterns of EMR. It allows geographers to look at change over a large area over time. Electromagnetic radiation spectrum In remote sensing terminology, electromagnetic energy is generally expressed in terms of wavelength, λ. Remote sensing data is helpful for updating existing geological maps, rapid preparation of lineament and tectonic maps, identifying the sites for quarrying the minerals and helpful in locating fossil fuel deposits. Principles of remote sensing Detection and discrimination of objects or surface features means detecting and recording of radiant energy reflected or emitted by objects or surface material. When a remote sensing instrument has a line-of-sight with an object that is reflecting sunlight or emitting heat, the instrument collects and records the radiant energy.While most remote sensing systems are designed to collect reflected radiation, some sensors, especially those on meteorological satellites, directly measure absorption phenomena, such as those associated with carbon dioxide (CO 2) and … From the following definitions, we can have a better understanding about Remote Sensing: According to White (1977), Remote Sensing includes all methods of obtaining pictures or other There are several regions of the electromagnetic spectrum which are useful for remote sensing. The sensor is a remote device to collect and record the electromagnetic radiation. The next portion of the spectrum of interest is the infrared (IR) region which covers the wavelength range from approximately 0.7 µm to 100 µm - more than 100 times as wide as the visible portion! understanding the information to be extracted from remote sensing data. Wavelengths are measured in micrometers (μm) or nanometers (nm). Emission of electromagnetic radiation, or EMR (sun/self- emission), Transmission of energy from the source to the surface of the earth, as well as absorption and scattering, Interaction of EMR with the earth’s surface: reflection and emission, Transmission of energy from the surface to the remote sensor, Data transmission, processing and analysis. electromagnetic an electric field a magnetic field … is a wave that propagates (radiates) through a vacuum at the speed of light (just under 300 000 m/s) and transfers energy from one place to another … these waves carry energy as … However, modern Remote Sensing means acquiring information about earth’s land and water surfaces by using reflected or emitted electromagnetic energy. DMPQ- “The revolt of 1857 led to far-reaching changes in the system of administration and the policies of the British government.” Elucidate. It can be used for updating road maps, asphalt conditions, and wetland delineation. The electromagnetic spectrum is the term used to describe to entire range of all possible frequencies of electromagnetic radiation. Some Earth surface materials, primarily rocks and minerals, fluoresce or emit visible light when illuminated by UV radiation. The light which our eyes - our "remote sensors" - can detect is part of the visible spectrum. If they did, then they would have to be cooled (and kept very cold during use), which would be very impractical. Detection and discrimination of objects or surface features means detecting and recording of radiant energy reflected or emitted by objects or surface material. Progressive stages in remote sensing are as follows: At temperature above absolute zero, all objects radiate electromagnetic energy by virtue of their atomic and molecular oscillations. Remote sensing, also called earth observation, refers to obtaining information about objects or areas at the Earth’s surface without being in direct contact with the object or area. The infrared region can be divided into two categories based on their radiation properties - the reflected IR, and the emitted or thermal IR. Trace the sequence of events during French revolution. DMPQ- Give historical background of Public account committee. DMPQ- Write an essay about the evolution of Paintings during Mughal period. Although we see sunlight as a uniform or homogeneous colour, it is actually composed of various wavelengths of radiation in primarily the ultraviolet, visible and infrared portions of the spectrum. Remote sensing: principles, electromagnetic spectrum, components and applications Remote sensing, also called earth observation, refers to obtaining information about objects or areas at the Earth’s surface without being in direct contact with the object or area. The longest visible wavelength is red and the shortest is violet. There are a number of stages in a Remote Sensing process, and each of them is important for successful operation. 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