The percent of energy that is reflected off a surface and back to a sensor.
Surface reflectance of materials can be measured using instruments such as spectrophotometers or colorimeters, which detect the amount of light reflected off a surface at different wavelengths. These instruments provide quantitative data on the reflectance properties of the material, which can be used to analyze its color and appearance characteristics. By comparing the reflected light to a reference standard, accurate measurements of surface reflectance can be obtained.
Reflectance is the measure of how much light is reflected off an object's surface. It affects the appearance of objects under different lighting conditions by determining how much light is absorbed or reflected, which can change the object's color, brightness, and overall visibility. Objects with high reflectance appear brighter and more vivid, while those with low reflectance may appear darker or less distinct.
Fluid that it attracted to a nearby surface and remains attached even when the surface curves away from the initial flow direction.
Reflectance refers to the amount of light that is reflected off a surface, while reflectivity is a measure of how efficiently a surface reflects light. Reflectance is a property of the surface, while reflectivity is a physical property of the material. In the context of light and surface interactions, reflectance and reflectivity are related in that they both describe how much light is reflected off a surface, but reflectivity specifically quantifies the efficiency of that reflection.
The term for the percentage of light reflected by something is called "reflectance." Reflectance measures the proportion of light that is reflected by a surface compared to the total amount of light that shines on it.
Reflectance curves show the reflectivity as a function of wavelengt.
Some major ground features and their typical spectral reflectance curves include vegetation, which shows high reflectance in the visible spectrum and low reflectance in the near-infrared spectrum; water, which has low reflectance across all wavelengths; soil, which typically has higher reflectance in the visible spectrum and lower reflectance in the near-infrared spectrum; and urban areas, which have varying spectral reflectance depending on surface materials like asphalt, concrete, and buildings.
the amount of solar radiation/the surface area of atmosphere/8
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It is so by definition.
Spectral reflectance measure a thin film's characteristics by reflecting light off the film and analyzing the resulting reflectance spectrum over a range of wavelengths. Light reflected from different interfaces of the film can be in- or out-of-phase so these reflections add or subtract, depending upon the wavelength of the light and the film's thickness and index. The result is intensity oscillations in the reflectance spectrum that are characteristic of the film.To determine the film's thickness, the software calculates a theoretical reflectance spectrum that matches as closely as possible to the measured spectrum. It begins with an initial guess for what the reflectance spectrum should look like, based on the nominal film stack. This includes information on the thickness and the refractive index of the different layers and the substrate that make up the sample. The theoretical reflectance spectrum is then adjusted by adjusting the film's properties until a best fit to the measured spectrum is found.This metrology can be used on thin film thickness measurement, even for transparent films.
Radiance is the variable directly measured by remote sensing instruments. Basically, you can think of radiance as how much light the instrument "sees" from the object being observed. When looking through an atmosphere, some light scattered by the atmosphere will be seen by the instrument and included in the observed radiance of the target. An atmosphere will also absorb light, which will decrease the observed radiance. Radiance has units of watt/steradian/square meter. Reflectance is the ratio of the amount of light leaving a target to the amount of light striking the target. It has no units. If all of the light leaving the target is intercepted for the measurement of reflectance, the result is called "hemispherical reflectance." Reflectance (or more specifically hemispherical reflectance) is a property of the material being observed. Radiance, on the other hand, depends on the illumination (both its intensity and direction), the orientation and position of the target and the path of the light through the atmosphere. With effort, many of the atmospheric effects and the solar illumination can be compensated for in digital remote sensing data. This yields something which is called "apparent reflectance," and it differs from true reflectance in that shadows and directional effects on reflectance have not been dealt with. Many people refer to this (rather inaccurately) as "reflectance." For most of the vegetation indices in this FAQ, radiance, reflectance, and apparent reflectance can be used interchangeably. However, since reflectance is a property of the target material itself, you will get the most reliable (and repeatable) vegetation index values using reflectance. Apparent reflectance is adequate in many cases. See the related link.
Bidirectional Reflectance Distribution Function
Surface reflectance of materials can be measured using instruments such as spectrophotometers or colorimeters, which detect the amount of light reflected off a surface at different wavelengths. These instruments provide quantitative data on the reflectance properties of the material, which can be used to analyze its color and appearance characteristics. By comparing the reflected light to a reference standard, accurate measurements of surface reflectance can be obtained.
as such there is no soecific difference..
James Richard Wallis has written: 'The fifty-foot chord definition for forest road curves' -- subject(s): Roads, Tables, Curves in engineering, Forestry engineering
KissingThe act of kissing.A kiss.Mathematics. A contact, as between two curves or surfaces, at three or more common points.