Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER)

The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) launched on NASA's Terra satellite in December 1999 provides anew tool for Earth observations. ASTER provides high-resolution, 15m(VNIR), 30m (SWIR) and 90m (TIR) coverage for limited areas with unique multispectal SWIR and TIR coverage and 15 m stereo coverage for DEM generation. These data have been used extensively for volcano and glacier monitoring. ASTER observations of over 1000 volcanoes around the world represent a significant increase in our ability to monitor volcanic activity and to map the products of eruptions. The SWIR channels have been used for mapping hot areas with temperatures up to 350 C and the multispectral TIR data have been used to map ash and SO2 plumes. ASTER data are being used in the Global Land Ice Measurements from Space (GLIMS) project to map and catalog the approximately 80,000 glaciers. The objective is to acquire multiple observations to detect changes in ice margins and surface feature velocities. ASTER data acquired over the Jornada Experimental range in New Mexico have been used to extract spectral emissivities in the 8 to 12 micrometer range. These TIR data were also used in models to estimate the surface energy fluxes. Similar analysis of data acquired over the El Reno Oklahoma test site has shown that our satellite estimates of the surface fluxes agree reasonably well with ground measurements.

[1]  K. Watson,et al.  Spectral ratio method for measuring emissivity , 1992 .

[2]  J. Norman,et al.  Evaluation of soil and vegetation heat flux predictions using a simple two-source model with radiometric temperatures for partial canopy cover , 1999 .

[3]  David C. Pieri,et al.  ASTER watches the world's volcanoes: a new paradigm for volcanological observations from orbit , 2004 .

[4]  Yasushi Yamaguchi,et al.  Overview of Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) , 1998, IEEE Trans. Geosci. Remote. Sens..

[5]  R. E. Walker,et al.  Color enhancement of highly correlated images. I - Decorrelation and HSI contrast stretches. [hue saturation intensity , 1986 .

[6]  Tsuneo Matsunaga,et al.  A Temperature-Emissivity Separation Method Using an Empirical Relationship between the Mean, the Maximum, and the Minimum of the Thermal Infrared Emissivity Spectrum , 1994 .

[7]  William P. Kustas,et al.  Estimating evapotranspiration over El Reno, Oklahoma with ASTER imagery , 2002 .

[8]  Roger G. Barry,et al.  Global Land Ice Measurements from Space , 2004 .

[9]  Aaas News,et al.  Book Reviews , 1893, Buffalo Medical and Surgical Journal.

[10]  Hiroyuki Fujisada,et al.  ASTER Level-1 data processing algorithm , 1998, IEEE Trans. Geosci. Remote. Sens..

[11]  M. Abrams The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER): Data products for the high spatial resolution imager on NASA's Terra platform , 2000 .

[12]  M. Abrams The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on NASA's Terra spacecraft , 2003 .

[13]  William P. Kustas,et al.  Estimating surface fluxes over the SGP site with remotely sensed data , 2000 .

[14]  Hiroshi Murakami,et al.  ASTER as a source for topographic data in the late 1990s , 1998, IEEE Trans. Geosci. Remote. Sens..

[15]  J. Norman,et al.  Source approach for estimating soil and vegetation energy fluxes in observations of directional radiometric surface temperature , 1995 .

[16]  William P. Kustas,et al.  Evapotranspiration estimates using ASTER thermal infrared imagery , 2002, SPIE Remote Sensing.