Skip to main content

Discrete Detectors and Scanning mirrors




  Discrete Detectors:  


Discrete detectors are devices used to capture electromagnetic radiation, such as visible light, infrared, or microwave energy, from the Earth's surface or atmosphere. They convert this radiation into electrical signals that can be processed and turned into images or data. These detectors work on the principle of the photoelectric effect, where incoming photons of light or other electromagnetic waves generate electrical charges within the detector material.


There are several types of discrete detectors used in remote sensing, including:


-   Photodiodes:   These are semiconductor devices that generate a current when exposed to light. They are commonly used in many imaging systems.

-   Charge-Coupled Devices (CCDs):   These are arrays of tiny light-sensitive capacitors that store and transfer electrical charge. CCDs are widely used in digital cameras and remote sensing satellites.

-   CMOS Sensors:   Complementary Metal-Oxide-Semiconductor sensors are another type of image sensor used in digital cameras and some remote sensing instruments.


  Scanning Mirrors:  


Scanning mirrors are mechanical or electronic components used in remote sensing systems to direct the incoming electromagnetic radiation onto the detectors. They enable the sensor to observe different parts of the Earth's surface by changing the sensor's viewing direction. Scanning mirrors come in various forms and can be categorized into two main types:


1.   Mechanical Scanning Mirrors:   These are physical mirrors that are mechanically moved to redirect the sensor's field of view. There are different scanning patterns, including:

   -   Whiskbroom Scanning:   A single detector observes a narrow strip on the ground as the mirror sweeps back and forth.

   -   Pushbroom Scanning:   An array of detectors collects data as the mirror moves, creating a continuous strip of data over time.


2.   Electronic Scanning (Staring Array):   Instead of moving a physical mirror, this method uses an array of detectors, each observing a specific direction. By activating specific detectors, the system can effectively change its viewing direction electronically.


Scanning mirrors determine the spatial resolution, coverage area, and efficiency of data acquisition in a remote sensing system. Different scanning patterns and technologies are chosen based on the specific application and requirements of the mission.



Comments

Popular posts from this blog

Geography of Landslides. Mitigation and Resilience.

A landslide is a geological event in which a mass of rock, earth, or debris moves down a slope under the force of gravity. Landslides can range in size from small to large and can be triggered by natural events such as heavy rainfall, earthquakes, or volcanic activity, or by human activities such as construction or mining. The geography of landslides is affected by a variety of factors that can increase the likelihood of landslides occurring in a particular area. These factors include slope angle and steepness, the type of soil and rock present, the climate and weather patterns of the region, the presence or absence of vegetation, and human activities such as construction, mining, and deforestation. Areas with steep slopes are more prone to landslides because gravity has a stronger effect on loose soil and rock, making it more likely to move downhill. Similarly, areas with loose, sandy soil or weak, fractured rock are more prone to landslides because they are less stable and more easil...

Geography of Flood. Types. Charector.

The geography of floods refers to the characteristics and patterns of floods in different geographic regions. Floods can occur in various landscapes, such as mountains, plains, coastal areas, and urban environments. The geography of a region plays a significant role in determining the frequency, magnitude, and impacts of floods. Some of the factors that influence the geography of floods include: Topography: The shape and elevation of the land can affect the flow and accumulation of water during a flood. For example, flat terrain can lead to slow-moving and widespread flooding, while steep slopes can result in flash floods and landslides. Climate: Regions with high rainfall or snowmelt can experience more frequent and intense floods, while dry regions may experience flash floods due to sudden, heavy rainfall. Hydrology: The characteristics of a river basin, such as its size, shape, and water flow, can influence the severity of a flood. For example, large river basins with extensive floo...

Landslides. USGS

Landslides. TYPES OF LANDSLIDES The term "landslide" describes a wide variety of processes that result in the downward and outward movement of slope-forming materials including rock, soil, artificial fill, or a combination of these. The materials may move by falling, toppling, sliding, spreading, or flowing. The animated GIF shows a graphic illustration of different types of landslides, with the commonly accepted terminology describing their features. The various types of landslides can be differentiated by the kinds of material involved and the mode of movement.

Flood prone regions India

Floods are natural disasters characterized by the overflow of water onto normally dry land. Various factors contribute to floods, including intense rainfall, rapid snowmelt, storm surges from coastal storms, and the failure of dams or levees. The geographical explanation involves understanding the key components of flood-prone regions: 1. Proximity to Water Bodies:    Flood-prone regions are often situated near rivers, lakes, or coastal areas. These locations are more susceptible to flooding as they are in close proximity to large water sources that can overflow during heavy precipitation or storms. 2. Topography:    Low-lying areas with gentle slopes are prone to flooding. Water naturally flows to lower elevations, and flat terrains allow water to accumulate easily. Valleys and floodplains are common flood-prone areas due to their topographical characteristics. 3. Rainfall Patterns:    Regions with high and concentrated rainfall are more likely to experience flooding. Intense and prol...

Volcano

Large magma chamber Bedrock Conduit (pipe) Base Sill Dike Layers of ash emitted by the volcano Flank Layers of lava emitted by the volcano Throat Parasitic cone Lava flow Vent Crater Ash cloud