Figure 1-2 – Summary Of Primary EO-1 Instrument Characteristics. This paper highlights data collects and analysis methodology of a set of standard and unique data collects that were defined to address specific issues. Since L. in general makes up <20% of L, such methods require extremely high accuracy (within ±1% for ocean applications) in the measurement of L, and high accuracy in the aerosol models. Hyperion collects 220 unique spectral channels ranging from 0.357 to 2.576 micrometers with a 10-nm bandwidth. channels with high radiometric accuracy. In a pilot study in the Riverland of South Australia, we report on spatio-temporal variations observed in near surface determined from multi-temporal monitoring of a floodplain with AEM data. Some samples from these subregions of relatively cool Late Palaeozoic temperatures also retain evidence for even earlier cooling from temperatures >120 °C, beginning prior to 350 Ma. Also include in Table 1 is the Hyperion VNIR, and SWIR pixel corresponding to the field measurem, indicated in Table 1, all four sites correspond to approxim, the moisture between the time of the field measurements (December 17-20, content. It is found that the retrieved depths (in a range of ∼1-20 m) match LIDAR depths very well (∼15% average error), indicating significant potential of using hyperspectral satellite sensor for efficient and repetitive observation of shallow coastal regions. Until recently, Landsat technology has suffered from low signal-to-noise ratio (SNR) and comparatively poor radiometric resolution, which resulted in limited application for inland water and land use/cover mapping. The Hyperion Imaging Spectrometer is the first high spatial resolution imaging spectrometer to orbit the Earth. MULTISPECTRAL Parameters HYPERION LAC Spectral Range 0.4 - 2.5 µm 0.9 - 1.6 µm Spatial Resolution 30 m 250 m Swath Width 7.5 Km 185 Km Spectral Resolution 10 nm 2-6 nm The Linear Etalon Imaging Spectral Array (LEISA) Atmospheric Corrector (LAC) is a high spectral resolution wedge imaging spectrometer designed to measure atmospheric water vapor content. The Earth Observing One (EO-1) satellite, a part of National Aeronautics and Space Administration's New Millennium Program, was developed to demonstrate new technologies and strategies for improved Earth observations. These variations are attributed in part, to floodplain management strategies, including an operational salt interception scheme (SIS) and to changes in the regulated height of the river. Techniques for spectral calibration of space-based sensors have been tested and validated with Hyperion. The GIS analysis has proven to be a useful tool for saving time and efforts by searching through vast and remote regions. over, share and access data. The Advanced Land Imager (ALI) is a prototype for a new generation of Landsat-7 Thematic Mapper. The telescope is a three-mirror astigmatic design, the high resolution hyperspectral imager is capable of resolving 220 spectral bands (from 0.4 to 2.5 µm) with a 30 meter resolution. The Late Palaeozoic event (300–270 Ma) is interpreted as cooling associated with the termination of the Alice Springs Orogeny, while cooling prior to 350 Ma probably represents the final stages of Early Middle Palaeozoic unroofing of the southern Adelaide Fold Belt. For the Key West site, derived bathymetry and water properties were validated with NAVOCEANO CHARTS (active bathymetric LIDAR system) and field measurements, respectively. The Hyperion sensor has two spectrometers operating over different spectral ranges. 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Hyperion overpass measurements and analysis into the performance verification nsidc scientist Siri Jodha Singh Khalsa leads the project principal.