Ads
related to: remote sensing handbook second edition
Search results
Results From The WOW.Com Content Network
Remote sensing is the acquisition of information about an object or phenomenon without making physical contact with the object, in contrast to in situ or on-site observation. The term is applied especially to acquiring information about Earth and other planets .
The Cambridge Edition of the Works of Schopenhauer; Cambridge Handbooks in Philosophy; Cambridge Hegel Translations; The Cambridge History of Modern European Thought; Cambridge Introductions to Key Philosophical Texts; Cambridge Introductions to Philosophy; Cambridge Introductions to Philosophy and Biology; The Cambridge Kant German-English Edition
Remote sensing is the acquisition of information about an object or phenomenon without making physical contact with the object and thus in contrast to on site observation. Subcategories This category has the following 14 subcategories, out of 14 total.
Spectroradiometry is a technique in Earth and planetary remote sensing, which makes use of light behaviour, specifically how light energy is reflected, emitted, and scattered by substances, to explore their properties in the electromagnetic (light) spectrum and identify or differentiate between them. [1]
Second, the two-way travel time of radiation from and back to the sensor can calculate the distance in active remote sensing systems, for example, Interferometric synthetic-aperture radar. This helps geomorphological studies of ground motion , and thus can illuminate deformations associated with landslides , earthquakes , etc. [ 3 ] [ 4 ]
Prof. Maître's research advanced in the fields ranging from digital camera to computational photography. He has done extensive research in remote sensing applications. His work included studies related to troposphere effects and its multi-temporal correction in differential SAR interferometry, [2] watermarking, [3] feature detection of SAR images [4] and Hough Transform applications.
Remote sensing is an approach to modeling evapotranspiration using an energy balance and the latent heat flux to find evapotranspiration rates. Evapotranspiration (ET) is a part of the water cycle , and accurate ET readings are important to local and global models to manage water resources.
One of the most important applications of thermal remote sensing in earth sciences is to calculate the Land Surface Temperature (LST). LST is a measurement of how hot the land is to the touch. It differs from air temperature (the temperature given in weather reports) because land heats and cools more quickly than air. [ 15 ]