ASTER Thermal Anomalies in Western Colorado

E., Richard

doi:10.15121/1148769

Title: ASTER Thermal Anomalies in Western Colorado

Dataset
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Abstract

This layer contains the areas identified as areas of anomalous surface temperature from ASTER satellite imagery. The temperature is calculated using the Emissivity Normalization Algorithm that separate temperature from emissivity. Areas that had temperature greater than 2o, and areas with temperature equal to 1o to 2o, were considered ASTER modeled very warm and warm surface exposures (thermal anomalies), respectively Note: 'o' is used in place of lowercase sigma in this description.

Authors:

E., Richard

Flint Geothermal, LLC

Publication Date:: Tue Jan 01 04:00:00 UTC 2013

Other Number(s):: 296

DOE Contract Number:: EE0002828

Research Org.:: DOE Geothermal Data Repository; Flint Geothermal, LLC

Sponsoring Org.:: USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Program (EE-4G)

Collaborations:: Flint Geothermal, LLC

Subject:: 15 GEOTHERMAL ENERGY; ASTER; ArcGIS; Colorado; GIS; Remote Sensing; algorithm; anomaly detection; geospatial; geospatial data; geothermal; shape file; shapefile; surface anomaly; surface exposures; surface temperature; thermal anomalies

OSTI Identifier:: 1148769

DOI:: https://doi.org/10.15121/1148769

Citation Formats


                    E., Richard. ASTER Thermal Anomalies in Western Colorado.  United States: N. p., 2013. 
        Web.  doi:10.15121/1148769.

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                    E., Richard. ASTER Thermal Anomalies in Western Colorado.  United States.  doi:https://doi.org/10.15121/1148769

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                    E., Richard. 2013.  
"ASTER Thermal Anomalies in Western Colorado".  United States.  doi:https://doi.org/10.15121/1148769.  https://www.osti.gov/servlets/purl/1148769. Pub date:Tue Jan 01 04:00:00 UTC 2013

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@article{osti_1148769,

  title        = {ASTER Thermal Anomalies in Western Colorado},

  author       = {E., Richard},

  abstractNote = {This layer contains the areas identified as areas of anomalous surface temperature from ASTER satellite imagery. The temperature is calculated using the Emissivity Normalization Algorithm that separate temperature from emissivity. Areas that had temperature greater than 2o, and areas with temperature equal to 1o to 2o, were considered ASTER modeled very warm and warm surface exposures (thermal anomalies), respectively Note: 'o' is used in place of lowercase sigma in this description.},

  doi          = {10.15121/1148769},

  journal      = {},

  number       = ,

  volume       = ,

  place        = {United States},

  year         = {Tue Jan 01 04:00:00 UTC 2013},

  month        = {Tue Jan 01 04:00:00 UTC 2013}

}

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DOI: https://doi.org/10.15121/1148769

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