Term
electromagnetic radiatiation |
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Definition
E=Electrical field, M=magnetic field, travels at the speed of light, perpendicular to each other. |
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Term
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wavelengths range from 400 billionths of a meter to about 10 billionths of a meter, uv waves can burn sking however most are blocked by ozone in the earth’s upper atmophere, uv wavelengths are used extensively in astronomical observatories, some remote sensing observations of the earth are also concerned with the measurement of ozone. |
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Definition
Violet 0.4-0.446 mm, blue 0.446-0.500mm, green 0.500-0.578mm, yellow 0.578-0.592, orange 0.592-0.620, red 0.620-0.7 |
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wavelengths range from less than a centimeter to tens or even hundreds of meters, used to transmit radio and television signals, radio waves can also be used to create images, the reflected waves can be used to form an image of the ground in complete darkness or though clouds |
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Term
spectral profiles of various types of vegetation (grass, coniferous, deciduous, etc), |
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Definition
-can identify and isolate sources of heat -materials absorb and reflect ER at various wavelengths with varying intensity - can detect and identify sources and types of pollution -can identify surface types and materials -can classify urban structures and land use types -can detect natural land covers and surface types -Spongy mesoph11- oxygen and carbon dioxide exchange takes place here -IR radiation is strongly reflected off cell walls -Changing reflection of dying leaf -Reflection of different types of vegetation -surface absorption and reflection of different materials in spectral profiles -bands -bandwidths -gaps -landsat case study spectral resolution of different sensors -landsat TM -7 different bands -7 wavelength intervals -ground resolution 30 by 30 and 120 by 120m for band 6 Band 1 450-515 um blue, lower limit= just above atmospheric scattering, lower limit=peak transmittance of clear water, upper limit= blue chorophyll absorption ends |
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makes water visible, makes water and water quality visible |
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520-600um green Lower limit=blue chlorophyll absorption ends, upper limit=red chlorophyll absorption bengins Maps intensity of chlorophyll reflectance in the green part of the electromagnetic spectrum Vegetation visible as it appears to the human eye |
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630-690 um red Important for vegetation discrimination, differences in reflectance intensity between different types of vegetation also show up in the visible part of the electromagnetic spectrum, cutoff at .690 um due to crossovers of spectral profiles |
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760-900um near infrared Lower limit at .760 um due to crossovers of spectral profiles, biomass depth, intensity and density, intensity of respones in this band can help determine type of vegetation Vegetation density visible |
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1.55-1.75 um mid-infrared Sensitive to plant turgidity water storage, can detect drought-induced stress in early stages, differentiates between clouds, water, ice and snow, hydrologic research Water content of vegetation visible |
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10.40-12.50 um thermal infrared Long wave heat radiation, temperature differences in surfaces, urban heat islands, soil moisture, geothermal activity, volcanic activity -makes heat visible in this panchromatic image makes heat visible in this false- |
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2.08-2.35um mid-infrared Rock formations, surface roughness/smoothness can be distinguished well Makes rock formation visible, |
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Definition
-sensor detects reflect ER from surface objects and atmosphere -land-based systems -sea-based systems -atmospheric systems -landpbased systems landsat SPOT IKONOS IRS -sea-based systems SeaWiFS -atmospheric systems GOES |
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-sensor sends out active signal and receivers altered signal -land-based systems -sea-based system -land-based systems -SRTM -RADARSAT Sea-Based systems -TOPEX -JASON-1 -SEASAT |
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movement of light through a material, transmission is wavelength dependent, the proportional amount of incident radiation passing through a surface. Reflection: the process of radiation bouncing off an object, the angle at which radiation hits an object will be the same angle at which it is reflected, smooth surfaces act as specular reflectors, rough surfaces act as diffuse reflectors |
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the absorption and conversion of electromagnetic radiation to other forms of energy, occurs in the atmosphere and on the ground, tends to occur in absortion bands |
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the unpredictable reflection of radiation by atmospheric particles, most scattering occurs high in the atmosphere and makes the sky seem blue, during sunset, or in the evening the sun is low on the horizon- the sun’s rays have to travel through a longer slice of the atmosphere, this almost totally scatters blue light, letting the longer wave red light through, hence red skies |
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