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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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fire hazard through models that simulate fire spread. In this paper, we describe the AVIRIS derived products we are developing<br />

to map wildl<strong>and</strong> fuels.<br />

Derived from text<br />

Thematic Mapping; Remote Sensing; Mountains; California; Forest Fires; Fire Prevention; Chaparral<br />

<strong>2000</strong>0064569 California Univ., Dept. of L<strong>and</strong>, Air, <strong>and</strong> Water Resources, Davis, CA USA<br />

Evaluation of L<strong>and</strong>scape Structure Using AVIRIS Quicklooks <strong>and</strong> Ancillary Data<br />

S<strong>and</strong>erson, Eric W., California Univ., USA; Ustin, Susan L., California Univ., USA; Summaries of the Seventh JPL Airborne Earth<br />

Science Workshop January 12-16, 1998; Dec. 19, 1998; <strong>Volume</strong> 1, pp. 355-364; In English; See also <strong>2000</strong>0064520<br />

Contract(s)/Grant(s): 1995-GlobalCh00404; No Copyright; Avail: CASI; A02, Hardcopy; A04, Microfiche<br />

Currently the best tool for examining l<strong>and</strong>scape structure is remote sensing, because remotely sensed data provide complete<br />

<strong>and</strong> repeatable coverage over l<strong>and</strong>scapes in many climatic regimes. Many sensors, with a variety of spatial scales <strong>and</strong> temporal<br />

repeat cycles, are available. The Airborne Visible/Infrared Imaging Spectrometer (AVIRIS) has imaged over 4000 scenes from<br />

over 100 different sites throughout North America. For each of these scenes, one-b<strong>and</strong> ”quicklook” images have been produced<br />

for review by AVIRIS investigators. These quicklooks are free, publicly available over the Internet, <strong>and</strong> provide the most complete<br />

set of l<strong>and</strong>scape structure data yet produced. This paper describes the methodologies used to evaluate the l<strong>and</strong>scape structure of<br />

quicklooks <strong>and</strong> generate corresponding datasets for climate, topography <strong>and</strong> l<strong>and</strong> use. A brief discussion of preliminary results<br />

is included at the end. Since quicklooks correspond exactly to their parent AVIRIS scenes, the methods used to derive climate,<br />

topography <strong>and</strong> l<strong>and</strong> use data should be applicable to any AVIRIS analysis.<br />

Derived from text<br />

Infrared Imagery; L<strong>and</strong> Use; Remote Sensing; Topography; Climatology<br />

<strong>2000</strong>0064570 Jet Propulsion Lab., California Inst. of Tech., Pasadena, CA USA<br />

The AVIRIS Low Altitude Option-An Approach to Increase Geometric Resolution <strong>and</strong> Improve Operational Flexibility<br />

Simultaneously<br />

Sarture, Charles M., Jet Propulsion Lab., California Inst. of Tech., USA; Chovit, Christopher J., Jet Propulsion Lab., California<br />

Inst. of Tech., USA; Chrien, Thomas G., Jet Propulsion Lab., California Inst. of Tech., USA; Eastwood, Michael L., Jet Propulsion<br />

Lab., California Inst. of Tech., USA; Green, Robert O., Jet Propulsion Lab., California Inst. of Tech., USA; Kurzwell, Charles<br />

G., Jet Propulsion Lab., California Inst. of Tech., USA; Summaries of the Seventh JPL Airborne Earth Science Workshop January<br />

12-16, 1998; Dec. 19, 1998; <strong>Volume</strong> 1, pp. 365; In English; See also <strong>2000</strong>0064520; No Copyright; Abstract Only; Available from<br />

CASI only as part of the entire parent document<br />

From 1987 through 1997 the Airborne Visible-InfraRed Imaging Spectrometer has matured into a remote sensing instrument<br />

capable of producing prodigious amounts of high quality data. Using the NASA/Ames ER-2 high altitude aircraft platform, flight<br />

operations have become very reliable as well. Being exclusively dependent on the ER-2, however, has limitations: the ER-2 has<br />

a narrow cruise envelope which fixes the AVIRIS ground pixel at 20 meters; it requires a significant support infrastructure; <strong>and</strong><br />

it has a very limited number of bases it can operate from. In the coming years, the ER-2 will also become less available for AVIRIS<br />

flights as NASA Earth Observing System satellite underflights increase. Adapting AVIRIS to lower altitude, less specialized aircraft<br />

will create a much broader envelope for data acquisition, i.e., higher ground geometric resolution while maintaining nearly<br />

the ideal spatial sampling. This approach will also greatly enhance flexibility while decreasing the overall cost of flight operations<br />

<strong>and</strong> field support. Successful adaptation is expected to culminate with a one-month period of demonstration flights.<br />

Author<br />

Airborne Equipment; Flight Altitude; Flight Operations; Low Altitude; Remote Sensing; U-2 Aircraft<br />

<strong>2000</strong>0064571 Zurich Univ., Remote Sensing Labs., Switzerl<strong>and</strong><br />

Parametric Geocoding of AVIRIS Data Using a Ground Control Point Derived Flightpath<br />

Schlaepfer, Daniel, Zurich Univ., Switzerl<strong>and</strong>; Meyer, Peter, Zurich Univ., Switzerl<strong>and</strong>; Itten, Klaus, Zurich Univ., Switzerl<strong>and</strong>;<br />

Summaries of the Seventh JPL Airborne Earth Science Workshop January 12-16, 1998; Dec. 19, 1998; <strong>Volume</strong> 1, pp. 367-372;<br />

In English; See also <strong>2000</strong>0064520; No Copyright; Avail: CASI; A02, Hardcopy; A04, Microfiche<br />

The position of scanning airborne systems (e.g. of the AVIRIS instrument) never is as stable as the behaviour of sensors on<br />

spaceborne platforms. Thus, geometric distortions occur due to variations of the flight-path as well as of the attitude (given by<br />

roll, pitch <strong>and</strong> heading angles) of the plane. These distortions can not be corrected by ground control point based traditional georeferencing<br />

procedures easily, since the movements can not be approximated satisfyingly by polynomial transformations of the<br />

image. A linewise calculation has to be performed instead, to consider the behaviour of the plane. Various projects have been carried<br />

out at the RSL, which require an exact localization of ground truth measurement or need the information from a digital eleva-<br />

116

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