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Areas of Weakly Anomalous to Anomalous Surface Temperature in Archuleta County, Colorado, as Identified from ASTER Thermal Data

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Note: This "Weakly Anomalous to Anomalous Surface Temperature" dataset differs from the "Anomalous Surface Temperature" dataset for this county (another remotely sensed CIRES product) by showing areas of modeled temperatures between 1o and 2o above the mean, as opposed to the greater than 2o temperatures contained in the "Anomalous Surface Temperature" dataset.

This layer contains areas of anomalous surface temperature in Archuleta County identified from ASTER thermal data and spatial based insolation model. The temperature is 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 that had temperature between 1o and 2o were considered ASTER modeled warm surface exposures (thermal anomalies).

Note: 'o' is used in this description to represent lowercase sigma.

Citation Formats

TY - DATA AB - Note: This "Weakly Anomalous to Anomalous Surface Temperature" dataset differs from the "Anomalous Surface Temperature" dataset for this county (another remotely sensed CIRES product) by showing areas of modeled temperatures between 1o and 2o above the mean, as opposed to the greater than 2o temperatures contained in the "Anomalous Surface Temperature" dataset. This layer contains areas of anomalous surface temperature in Archuleta County identified from ASTER thermal data and spatial based insolation model. The temperature is 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 that had temperature between 1o and 2o were considered ASTER modeled warm surface exposures (thermal anomalies). Note: 'o' is used in this description to represent lowercase sigma. AU - Hussein, Khalid DB - Open Energy Data Initiative (OEDI) DP - Open EI | National Renewable Energy Laboratory DO - 10.15121/1148743 KW - geothermal KW - Colorado KW - Archeluta County KW - Remote sensing KW - ASTER KW - Thermal infrared KW - ArcGIS KW - GIS KW - shapefile KW - shape file KW - geospatial KW - data KW - thermal KW - temperature KW - anomaly detection KW - thermal anomalies KW - geospatial data LA - English DA - 2012/02/01 PY - 2012 PB - Flint Geothermal, LLC T1 - Areas of Weakly Anomalous to Anomalous Surface Temperature in Archuleta County, Colorado, as Identified from ASTER Thermal Data UR - https://doi.org/10.15121/1148743 ER -
Export Citation to RIS
Hussein, Khalid. Areas of Weakly Anomalous to Anomalous Surface Temperature in Archuleta County, Colorado, as Identified from ASTER Thermal Data. Flint Geothermal, LLC, 1 February, 2012, GDR. https://doi.org/10.15121/1148743.
Hussein, K. (2012). Areas of Weakly Anomalous to Anomalous Surface Temperature in Archuleta County, Colorado, as Identified from ASTER Thermal Data. [Data set]. GDR. Flint Geothermal, LLC. https://doi.org/10.15121/1148743
Hussein, Khalid. Areas of Weakly Anomalous to Anomalous Surface Temperature in Archuleta County, Colorado, as Identified from ASTER Thermal Data. Flint Geothermal, LLC, February, 1, 2012. Distributed by GDR. https://doi.org/10.15121/1148743
@misc{OEDI_Dataset_6649, title = {Areas of Weakly Anomalous to Anomalous Surface Temperature in Archuleta County, Colorado, as Identified from ASTER Thermal Data}, author = {Hussein, Khalid}, abstractNote = {Note: This "Weakly Anomalous to Anomalous Surface Temperature" dataset differs from the "Anomalous Surface Temperature" dataset for this county (another remotely sensed CIRES product) by showing areas of modeled temperatures between 1o and 2o above the mean, as opposed to the greater than 2o temperatures contained in the "Anomalous Surface Temperature" dataset.

This layer contains areas of anomalous surface temperature in Archuleta County identified from ASTER thermal data and spatial based insolation model. The temperature is 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 that had temperature between 1o and 2o were considered ASTER modeled warm surface exposures (thermal anomalies).

Note: 'o' is used in this description to represent lowercase sigma.
}, url = {https://gdr.openei.org/submissions/311}, year = {2012}, howpublished = {GDR, Flint Geothermal, LLC, https://doi.org/10.15121/1148743}, note = {Accessed: 2025-05-01}, doi = {10.15121/1148743} }
https://dx.doi.org/10.15121/1148743

Details

Data from Feb 1, 2012

Last updated Aug 23, 2021

Submitted Feb 27, 2014

Organization

Flint Geothermal, LLC

Contact

Khalid Hussein

Khalid.Hussein@colorado.edu

303.492.6782

Authors

Khalid Hussein

Flint Geothermal LLC

Research Areas

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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