Remote sensing for

Student à South Eastern University of Srilanka
11 Sep 2014
Remote sensing for
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Remote sensing for

Notes de l'éditeur

  1. COMS · COMS Communication, Ocean and Meteorological Satellite - KOMPSAT (Korea)
  2. Energy Source or Illumination (A) - the first requirement for remote sensing is to have an energy source which illuminates or provides electromagnetic energy to the target of interest. Radiation and the Atmosphere (B) - as the energy travels from its source to the target, it will come in contact with and interact with the atmosphere it passes through. This interaction may take place a second time as the energy travels from the target to the sensor. Interaction with the Target (C) - once the energy makes its way to the target through the atmosphere, it interacts with the target depending on the properties of both the target and the radiation. Recording of Energy by the Sensor (D) - after the energy has been scattered by, or emitted from the target, we require a sensor (remote - not in contact with the target) to collect and record the electromagnetic radiation. Transmission, Reception, and Processing (E) - the energy recorded by the sensor has to be transmitted, often in electronic form, to a receiving and processing station where the data are processed into an image (hardcopy and/or digital). Interpretation and Analysis (F) - the processed image is interpreted, visually and/or digitally or electronically, to extract information about the target which was illuminated. Application (G) - the final element of the remote sensing process is achieved when we apply the information that we have been able to extract from the imagery about the target, in order to better understand it, reveal some new information, or assist in solving a particular problem.
  3. Hemisphere-உலகின் அரை உருண்டை
  4. Types of Satellite Images Both of these types of satellites take measurements of different wavelengths of radiation. There are three widely used atmospheric windows (channels) That allow radiation from the lower atmosphere to space: Visible (~0.6 μm) Visible images record visible light from the sun reflected back to the satellite by cloud tops, land, and sea surfaces. Equivalently a black and white photograph from space. Visible images can only be made during daylight.Dark areas: Regions where small amounts of visible light are reflected back to space. i.e. forests, oceans Bright areas: Regions where large amounts of visible light are reflected back to space. i.e. snow, thick clouds Current Visible Image Infrared or IR (10 to 12 μm) Infrared images record infrared radiation emitted directly by cloud tops, land, or ocean surfaces. Cooler temperatures shown as light gray tones. Warmer temperatures shown as dark gray tones. Current IR Image Water vapor (6.5 to 6.7 μm) Water vapor images record infrared radiation emitted by water vapor in the atmosphere. Bright, white shades represent radiation from a moist layer or cloud in the upper troposphere (cold brightness temperature). Dark, gray/black shades represent radiation from the Earth or a dry layer in the middle troposphere (warm brightness temperature). Current WV Image