ASTER Thermal Anomalies in Western Colorado
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:
- Publication Date:
- Other Number(s):
- 296
- DOE Contract Number:
- EE0002828
- Research Org.:
- USDOE Geothermal Data Repository (United States); 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
- Keywords:
- geothermal; Colorado; Remote Sensing; ASTER; GIS; shapefile; shape file; geospatial; ArcGIS; geospatial data; anomaly detection; surface anomaly; surface temperature; algorithm; thermal anomalies; surface exposures
- Geolocation:
- 40.875522982203,-104.98394375|36.827097813078,-104.98394375|36.827097813078,-108.84004375|40.875522982203,-108.84004375|40.875522982203,-104.98394375
- OSTI Identifier:
- 1148769
- DOI:
- https://doi.org/10.15121/1148769
- Project Location:
-
Citation Formats
E., Richard. ASTER Thermal Anomalies in Western Colorado. United States: N. p., 2013.
Web. doi:10.15121/1148769.
E., Richard. ASTER Thermal Anomalies in Western Colorado. United States. doi:https://doi.org/10.15121/1148769
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 00:00:00 EST 2013
@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 = {2013},
month = {1}
}
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