No. 51, May/June 2002
Using
geospatial technologies to understand dryland dynamics
Spatial, spectral and temporal resolutions for various imaging systems considered in this investigation, with a qualitative rating (poor, fair, good, excellent) of their applicability to detect and monitor active dust storms.
*Note, at this stage only the visible band of GOES has been used because of the size of most dust storms in the Mojave Desert makes them difficult to detect with the 1-km resolution of the visible band. Therefore, it is unlikely that they would be detected by the 4-km resolution of the thermal bands. |
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