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GIS 104
absorption,reflectance and transmission
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Light reflection, absorption and transmission
The 3 ways
electromagnetic radiation
from the sun can interact with the
Earth's surface
Remote Sensing Energy Mechanics
1.
Incident energy
(Ei) strikes the
Earth
2.
Reflected energy
(Er)
3.
Absorbed energy
(Ea)
4.
Transmitted energy
(
Et
)
Some
electromagnetic energy
(EM) freely passes through the
atmosphere window
before hitting the Earth's surface
In remote sensing,
light rays
(incident energy) bounce off (reflected energy) objects back to the sensor in
orbit
Sensors
detect the reflected energy
Incident energy (Ei)
The EM radiation that actually makes it to Earth
Spectral reflectance (p)
The proportion of reflected incident
energy
Incident
energy interacts differently with different
features
on Earth
Earth's features have different proportions of
energy
being reflected,
absorbed
, and transmitted
Each
object has its own
spectral
signature
Spectral bands
Ranges of wavelength ranges, e.g.
infrared
spectrum is from 750 nm to 1 mm,
ultraviolet
range is from 100 to 400 nm
Multispectral
images
Can have 3 to 10 bands
Hyperspectral
images
Have hundreds of finer bands