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Scientific and Technical Aerospace Reports Volume 38 July 28, 2000

Scientific and Technical Aerospace Reports Volume 38 July 28, 2000

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7.6, while the 1926 events appear to be comparable in size to the subsequent (M approximately 7) 1943 events, <strong>and</strong> an order of<br />

magnitude higher than previously reported.<br />

Author<br />

Deformation; Global Positioning System; Tectonics; Triangulation; Geodetic Surveys; Indonesia<br />

<strong>2000</strong>0064087 Jet Propulsion Lab., California Inst. of Tech., Pasadena, CA USA<br />

Capabilities <strong>and</strong> Limitations of Radio Occultation Measurements for Ionosphere Monitoring<br />

Hajj, G. A., Jet Propulsion Lab., California Inst. of Tech., USA; Romans, L. J., Jet Propulsion Lab., California Inst. of Tech., USA;<br />

Pi, X., Jet Propulsion Lab., California Inst. of Tech., USA; Wang, Chunming, University of Southern California, USA; [1999];<br />

20p; In English; LEO Missions, 9-11 Mar. 1999, Potsdam, Germany; No Copyright; Avail: CASI; A03, Hardcopy; A01, Microfiche<br />

The paper: (1) describes the range of capabilities of GPS radio occultation missions in ionospheric research: (a) ionospheric<br />

profiling; (b) ionospheric imaging; (c) ionospheric data assimilation; <strong>and</strong> (d) measurement of scintillation. (2) Identify strengths<br />

<strong>and</strong> weaknesses of measurements: (a) coverage; (b) resolution; <strong>and</strong> (c) uniqueness of solution.<br />

Derived from text<br />

Global Positioning System; Imaging Techniques; Ionospheric Propagation<br />

<strong>2000</strong>0064521 Arizona Univ., Soil, Water, <strong>and</strong> Environmental Science Dept., Tucson, AZ USA<br />

Using Mixture Analysis for Soil Information Extraction from an AVIRIS Scene at the Walnut Gulch Experimental<br />

Watershed-Arizona<br />

Accioly, L., Arizona Univ., USA; Huete, A. R., Arizona Univ., USA; Batchily, K., Arizona Univ., USA; Summaries of the Seventh<br />

JPL Airborne Earth Science Workshop January 12-16, 1998; Dec. 19, 1998; <strong>Volume</strong> 1, pp. 1-7; In English; See also <strong>2000</strong>0064520;<br />

No Copyright; Avail: CASI; A02, Hardcopy; A04, Microfiche<br />

Due to its ubiquitous presence, soil is present in almost all applications of image-based spectral mixture analysis (SMA). In<br />

many studies, however, most of the interest is given to the fraction of the vegetation endmember <strong>and</strong> its relationship to plant biophysical<br />

parameters. One of the few examples of the application of mixture analysis directly to soil is given by Huete <strong>and</strong> Escadafal<br />

(1991). These authors used SMA for soil biophysical information extraction in the region from 400 to 900 nm. They found that<br />

the variability of 46 soils from different types of environments could be explained by four independent basis curves, which in linear<br />

combination were able to reconstitute the experimental data set. These authors, however, did not use spectral mixture analysis<br />

to produce soil spectral maps. Mixture analysis can be applied on the basis of spectra extracted from the image (image endmembers)<br />

<strong>and</strong>/or on the basis of pure spectra from lab of field (reference endmembers). When the spatial variability within a pixel is<br />

high, as in a semiarid scrubl<strong>and</strong>, mixture analysis on the basis of image endmembers has been shown more accurate than maximum<br />

likelihood supervised classification. The general objective of this study was to derive soil spectral maps of an AVIRIS scene at<br />

the Walnut Gulch Experimental Watershed using mixture analysis. The specific objectives are to: (a) evaluate the dimensionality<br />

of AVIRIS data (i.e., how many endmembers); (b) find the physical meaning of the dimensions (i.e., what feature in the ground<br />

each endmember represents); <strong>and</strong> (c) determine the spatial abundances of the endmembers throughout the AVIRIS scene of the<br />

Walnut Gulch Experimental Watershed.<br />

Derived from text<br />

Image Analysis; Soil Mapping; Spectrum Analysis; Remote Sensing; Infrared Spectrometers<br />

<strong>2000</strong>0064522 Spectral Sciences, Inc., Burlington, MA USA<br />

FLAASH, A MODTRAN4 Atmospheric Correction Package for Hyperspectral Data Retrievals <strong>and</strong> Simulations<br />

Adler-Golden, S., Spectral Sciences, Inc., USA; Berk, A., Spectral Sciences, Inc., USA; Bernstein, L. S., Spectral Sciences, Inc.,<br />

USA; Richtsmeier, S., Spectral Sciences, Inc., USA; Acharya, P. K., Spectral Sciences, Inc., USA; Matthew, M. W., Spectral<br />

Sciences, Inc., USA; Anderson, G. P., Phillips Lab., USA; Allred, C. L., Phillips Lab., USA; Jeong, L. S., Phillips Lab., USA;<br />

Chetwynd, J. H., Phillips Lab., USA; Summaries of the Seventh JPL Airborne Earth Science Workshop January 12-16, 1998; Dec.<br />

19, 1998; <strong>Volume</strong> 1, pp. 9-14; In English; See also <strong>2000</strong>0064520<br />

Contract(s)/Grant(s): F196<strong>28</strong>-91-C-0145; No Copyright; Avail: CASI; A02, Hardcopy; A04, Microfiche<br />

FLAASH (Fast Line-of-sight Atmospheric Analysis of Spectral Hypercubes) is a MODTRAN-based ”atmospheric correction”<br />

software package which is being developed by the Air Force Phillips Laboratory, Hanscom AFB <strong>and</strong> Spectral Sciences, Inc.<br />

to support current <strong>and</strong> planned IR-visible-UV hyperspectral <strong>and</strong> multispectral sensors. The main objectives are to provide (1)<br />

accurate, physics-based derivation of surface <strong>and</strong> atmospheric properties (such as surface albedo, surface altitude, water vapor<br />

column, aerosol <strong>and</strong> cloud optical depths, surface <strong>and</strong> atmospheric temperatures), (2) minimal computation time requirements,<br />

<strong>and</strong> (3) an interactive, user-friendly interface for running arbitrary MODTRAN calculations. FLAASH is written in the Interactive<br />

131

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