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Title: 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}
}