Ideal Remote Sensing System.

Remote sensing is the science (and to some extent, art) of acquiring information about the Earth's surface without actually being in contact with it. This is done by sensing and recording reflected or emitted energy and processing, analyzing, and applying that information."

In much of remote sensing, the process involves an interaction between incident radiation and the targets of interest. This is exemplified by the use of imaging systems where the following seven elements are involved. Note, however that remote sensing also involves the sensing of emitted energy and the use of non-imaging sensors.

1. 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.

2. 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.

3. 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.

4. 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.

5. 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).

6. Interpretation and Analysis (F) - the processed image is interpreted, visually and/or digitally or electronically, to extract information about the target which was illuminated.

7. Application (G) - the final element of the remote sensing process is achieved when we apply the information 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.

Comments

Groundwater – Porosity and Permeability

Groundwater refers to the water that resides beneath the Earth's surface in the pores and crevices of rock, sediment, and soil. Two key properties that influence the movement and storage of groundwater are porosity and permeability: 1. Porosity: - Definition: Porosity refers to the volume percentage of void spaces (pores or openings) in a geological material, such as soil or rock. - Role: Porosity determines how much water a subsurface material can hold. It is a measure of the material's capacity to store water. - Factors: Porosity is influenced by the size and arrangement of particles within the material. Highly porous materials have more void spaces, while less porous materials have fewer. - Units: Porosity is expressed as a percentage, with 0% indicating complete solidity (no pore spaces) and 100% indicating complete void space. 2. Permeability: - Definition: Permeability refers to the ability of a geological material to transmit fluids, such as water. It meas

Ground Water

Groundwater Terminology, Concepts, and Facts Key Terms Aquifer: A geological formation that can store and transmit significant quantities of water. Water Table: The upper surface of the saturated zone in an aquifer. Recharge: The process of replenishing groundwater through precipitation or other sources. Discharge: The process of groundwater flowing out of an aquifer, typically into surface water bodies or through wells. Hydraulic Gradient: The slope of the water table. Darcy's Law: A law that describes the flow of groundwater through porous media. Permeability: The ability of a material to transmit water. Porosity: The amount of void space in a material. Concepts Groundwater Flow: Groundwater moves from areas of higher hydraulic head to areas of lower hydraulic head. Groundwater Contamination: The introduction of pollutants into groundwater. Groundwater Depletion: The excessive extraction of groundwater, leading to a decline in water table levels. Saltwater Intrusion:

Artisan Wells Basins

Artisan Wells and Basins Artesian wells are a type of well that harnesses the natural pressure of water trapped underground to force water to the surface without pumping. This phenomenon occurs in specific geological formations known as artesian basins . Key Terminologies and Concepts Aquifer: A geological formation that can store and transmit water. It is typically made up of porous rocks or sediments like sandstone or gravel. Confined Aquifer: An aquifer that is sandwiched between two impermeable layers (like clay or shale) that prevent water from escaping. Artesian Basin: A geological structure where a confined aquifer is tilted and has a recharge area at a higher elevation than the discharge area. This creates a pressure gradient that forces water to flow upwards. Potentiometric Surface: The theoretical level to which water would rise in a well drilled into an artesian aquifer if there were no restrictions. It is determined by the pressure head in the aquifer. Flowing Artesian

Watershed. Catchment. Basin

A watershed, also known as a river basin or drainage basin, is a fundamental concept in geohydrology and hydrology. It refers to a specific geographic area or region of land where all the surface water, including rainfall, snowmelt, and runoff, drains into a common outlet, such as a river, lake, or ocean. Here's an explanation of each term: 1. Watershed: A watershed is essentially a natural hydrological unit defined by the topography of the land. It represents the entire area from which all precipitation and surface water flow eventually gathers at a single point. This point is typically where the main river or stream within the watershed exits into a larger body of water, such as an ocean. Watersheds come in various sizes, from small ones that encompass a few square miles to enormous ones that cover entire continents. 2. River/Drainage Basin: A river basin or drainage basin is another way to describe a watershed. It's the land area that collects and channels water into a river

Discrete Detectors and Scanning mirrors Across the track scanner Whisk broom scanner.

Multispectral Imaging Using Discrete Detectors and Scanning Mirrors (Across-Track Scanner or Whisk Broom Scanner) Multispectral Imaging: This technique involves capturing images of the Earth's surface using multiple sensors that are sensitive to different wavelengths of electromagnetic radiation. This allows for the identification of various features and materials based on their spectral signatures. Discrete Detectors: These are individual sensors that are arranged in a linear or array configuration. Each detector is responsible for measuring the radiation within a specific wavelength band. Scanning Mirrors: These are optical components that are used to deflect the incoming radiation onto the discrete detectors. By moving the mirrors, the sensor can scan across the scene, capturing data from different points. Across-Track Scanner or Whisk Broom Scanner: This refers to the scanning mechanism where the mirror moves perpendicular to the direction of flight. This allows for t

Vineesh V, Geography

Search This Blog