Areas with Surface Thermal Anomalies as Detected by ASTER and LANDSAT Data in Northwest Delta, Colorado

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This map shows areas of anomalous surface temperature in northern Saguache Counties identified from ASTER and LANDSAT thermal data and spatial based insolation model. The temperature for the ASTER data was calculated using the Emissivity Normalization Algorithm that separate temperature from emissivity. The incoming solar radiation was calculated using spatial based insolation model developed by Fu and Rich (1999). Then the temperature due to solar radiation was calculated using emissivity derived from ASTER data. The residual temperature, i.e. temperature due to solar radiation subtracted from ASTER temperature was used to identify thermally anomalous areas.

Areas having anomalous temperature in the ASTER data are shown in blue diagonal hatch, while areas having anomalous temperature in the LANDSAT data are shown in magenta on the map. Thermal springs and areas with favorable geochemistry are also shown. Springs or wells having non-favorable geochemistry are shown as blue dots.

Citation Formats

TY - DATA AB - This map shows areas of anomalous surface temperature in northern Saguache Counties identified from ASTER and LANDSAT thermal data and spatial based insolation model. The temperature for the ASTER data was calculated using the Emissivity Normalization Algorithm that separate temperature from emissivity. The incoming solar radiation was calculated using spatial based insolation model developed by Fu and Rich (1999). Then the temperature due to solar radiation was calculated using emissivity derived from ASTER data. The residual temperature, i.e. temperature due to solar radiation subtracted from ASTER temperature was used to identify thermally anomalous areas. Areas having anomalous temperature in the ASTER data are shown in blue diagonal hatch, while areas having anomalous temperature in the LANDSAT data are shown in magenta on the map. Thermal springs and areas with favorable geochemistry are also shown. Springs or wells having non-favorable geochemistry are shown as blue dots. AU - Hussein, Khalid DB - Geothermal Data Repository DP - Open EI | National Renewable Energy Laboratory DO - 10.15121/1361184 KW - geothermal KW - Colorado KW - Delta County KW - Remote sensing KW - ASTER KW - LANDSAT KW - Thermal infrared KW - thermal anomalies KW - surface temperature anomalies KW - map LA - English DA - 2012/02/01 PY - 2012 PB - Flint Geothermal, LLC T1 - Areas with Surface Thermal Anomalies as Detected by ASTER and LANDSAT Data in Northwest Delta, Colorado UR - https://doi.org/10.15121/1361184 ER -
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Hussein, Khalid. Areas with Surface Thermal Anomalies as Detected by ASTER and LANDSAT Data in Northwest Delta, Colorado. Flint Geothermal, LLC, 1 February, 2012, Geothermal Data Repository. https://doi.org/10.15121/1361184.
Hussein, K. (2012). Areas with Surface Thermal Anomalies as Detected by ASTER and LANDSAT Data in Northwest Delta, Colorado. [Data set]. Geothermal Data Repository. Flint Geothermal, LLC. https://doi.org/10.15121/1361184
Hussein, Khalid. Areas with Surface Thermal Anomalies as Detected by ASTER and LANDSAT Data in Northwest Delta, Colorado. Flint Geothermal, LLC, February, 1, 2012. Distributed by Geothermal Data Repository. https://doi.org/10.15121/1361184
@misc{GDR_Dataset_327, title = {Areas with Surface Thermal Anomalies as Detected by ASTER and LANDSAT Data in Northwest Delta, Colorado}, author = {Hussein, Khalid}, abstractNote = {This map shows areas of anomalous surface temperature in northern Saguache Counties identified from ASTER and LANDSAT thermal data and spatial based insolation model. The temperature for the ASTER data was calculated using the Emissivity Normalization Algorithm that separate temperature from emissivity. The incoming solar radiation was calculated using spatial based insolation model developed by Fu and Rich (1999). Then the temperature due to solar radiation was calculated using emissivity derived from ASTER data. The residual temperature, i.e. temperature due to solar radiation subtracted from ASTER temperature was used to identify thermally anomalous areas.

Areas having anomalous temperature in the ASTER data are shown in blue diagonal hatch, while areas having anomalous temperature in the LANDSAT data are shown in magenta on the map. Thermal springs and areas with favorable geochemistry are also shown. Springs or wells having non-favorable geochemistry are shown as blue dots.
}, url = {https://gdr.openei.org/submissions/327}, year = {2012}, howpublished = {Geothermal Data Repository, Flint Geothermal, LLC, https://doi.org/10.15121/1361184}, note = {Accessed: 2025-04-27}, doi = {10.15121/1361184} }
https://dx.doi.org/10.15121/1361184

Details

Data from Feb 1, 2012

Last updated Nov 28, 2017

Submitted Feb 27, 2014

Organization

Flint Geothermal, LLC

Contact

Khalid Hussein

303.492.6782

Authors

Khalid Hussein

Flint Geothermal, LLC

DOE Project Details

Project Name Recovery Act: Use Remote Sensing Data (selected visible and infrared spectrums) to locate high temp ground anomalies in Colorado.Confirm heat flow potential w/ on-site temp surveys to drill deep resource wells

Project Lead Mark Ziegenbein

Project Number EE0002828

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