Hyperspectral Imagery - What is it? What can it do?
Abstract
Because all materials reflect, absorb, or emit photons in ways characteristic of their molecular makeup, a high resolution trace of the transmitted, reflected, emitted, or luminesced radiation versus wavelength forms a graphical record unique to a given material. The laboratory use of spectral measurements to identify minerals, pigments, and organic and inorganic compounds is an established and reliable technique; and, the reasoning goes, if such could be done from air or space, it would give remote sensing a similar capability. Unfortunately, the useful absorption bands are narrow, 10 nanometers (nm) or less, and cannot be recorded with broad band systems such as Landsat. With the advent of the Airborne Visible Infrared Imaging Spectrometer (AVIRIS) and similar systems, the narrow band capability entered the remote sensing domain. AVIRIS is a true spectrometer, collecting reflecting solar energy (0.4-2.5 micra) in about 220 channels, or images, each in a spectral bandwidth of about 9.6 nm. This type of narrow band information is called hyperspectral.
Document Details
- Document Type
- Technical Report
- Publication Date
- Sep 04, 1990
- Accession Number
- ADA231164
Entities
People
- Jack N. Rinker
Organizations
- Geospatial Research Laboratory