Surface Temperature Anomalies Derived from Night Time ASTER Data Corrected for Solar and Topographic Effects, Alamosa and Saguache Counties, Colorado

Hussein, Khalid

doi:10.15121/1361050

Title: Surface Temperature Anomalies Derived from Night Time ASTER Data Corrected for Solar and Topographic Effects, Alamosa and Saguache Counties, Colorado

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Abstract

This map shows areas of anomalous surface temperature in Alamosa and Saguache Counties 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 greater than 2o were considered ASTER modeled "very warm modeled surface temperature" are shown in red on the map. Areas that had temperatures between 1o and 2o were considered ASTER modeled "warm modeled surface temperature" are shown in yellow on the map. This map also includes the locations of shallow temperature survey points, locations of springs or wells with favorable geochemistry, faults, transmission lines, and areas of modeled basement weakness "fairways." Note: 'o' is used in this description to represent lowercase sigma.

Authors:: Hussein, Khalid

Publication Date:: Wed Feb 01 00:00:00 EST 2012

Other Number(s):: 318

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), Geothermal Technologies Program (EE-2C)

Subject:: 15 Geothermal Energy

Keywords:: geothermal; Remote sensing; ASTER; Colorado; Thermal infrared; Alamosa County; Saguache County; map; surface temperature anomalies; thermal anomalies

Geolocation:: 38.611939237693,-104.1489828125|36.862265662716,-104.1489828125|36.862265662716,-106.8625046875|38.611939237693,-106.8625046875|38.611939237693,-104.1489828125

OSTI Identifier:: 1361050

DOI:: https://doi.org/10.15121/1361050

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                    Hussein, Khalid. Surface Temperature Anomalies Derived from Night Time ASTER Data Corrected for Solar and Topographic Effects, Alamosa and Saguache Counties, Colorado.  United States: N. p., 2012. 
        Web.  doi:10.15121/1361050.

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                    Hussein, Khalid. Surface Temperature Anomalies Derived from Night Time ASTER Data Corrected for Solar and Topographic Effects, Alamosa and Saguache Counties, Colorado.  United States.  doi:https://doi.org/10.15121/1361050

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                    Hussein, Khalid. 2012.  
"Surface Temperature Anomalies Derived from Night Time ASTER Data Corrected for Solar and Topographic Effects, Alamosa and Saguache Counties, Colorado".  United States.  doi:https://doi.org/10.15121/1361050.  https://www.osti.gov/servlets/purl/1361050. Pub date:Wed Feb 01 00:00:00 EST 2012

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@article{osti_1361050,

  title        = {Surface Temperature Anomalies Derived from Night Time ASTER Data Corrected for Solar and Topographic Effects, Alamosa and Saguache Counties, Colorado},

  author       = {Hussein, Khalid},

  abstractNote = {This map shows areas of anomalous surface temperature in Alamosa and Saguache Counties 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 greater than 2o were considered ASTER modeled "very warm modeled surface temperature" are shown in red on the map. Areas that had temperatures between 1o and 2o were considered ASTER modeled "warm modeled surface temperature" are shown in yellow on the map. This map also includes the locations of shallow temperature survey points, locations of springs or wells with favorable geochemistry, faults, transmission lines, and areas of modeled basement weakness "fairways." Note: 'o' is used in this description to represent lowercase sigma.},

  doi          = {10.15121/1361050},

  journal      = {},

  number       = ,

  volume       = ,

  place        = {United States},

  year         = {Wed Feb 01 00:00:00 EST 2012},

  month        = {Wed Feb 01 00:00:00 EST 2012}

}

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DOI: https://doi.org/10.15121/1361050

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