Monitoring heat flux using Landsat TM/ETM+ thermal infrared data - A case study at Karapiti ('Craters of the Moon') thermal area, New Zealand

Md Bodruddoza Mia, Chris J. Bromley, Yasuhiro Fujimitsu

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Abstract

Thermal infrared (TIR) data from available, daytime, Landsat-TM/ETM+ satellite imagery, supported by ground measurements, were used in this study to investigate changes between 1990 and 2011 in the radiative component of the anomalous surface heat flux emitted from the 0.5km2 Karapiti thermal area, at Wairakei Geothermal Field, Taupo, New Zealand. The geothermal radiative heat flux (net RHF), of subsurface origin, was then assessed by subtracting the re-radiated heat flux that is of solar origin, as determined using coincident satellite imagery at two external sites. The total net RHF decreased by about 7MW from 1990 to 2011. Results of a vegetation index study, using ratios of two (visible) spectral bands, implied that the area of healthy vegetation at Karapiti has progressively increased during this period. This supports the evidence for a decrease in geothermal heat flux, because the health of thermally-stressed vegetation is inversely related to shallow ground temperature. Although images of apparent land-surface temperature (LST) show large variations with time, this is attributable to ambient temperature change. Spot ground estimates of heat flux using a calorimeter also showed, on average, a decreasing trend of heat fluxes between 2000 and 2009, although several sites showed stable heat fluxes. Further supporting evidence came from repeated ground-based temperature-depth profiles, which showed that the near-surface boiling point depth lowered in levels at most sites between 2000 and 2011, although several sites located in actively-steaming bare-ground (~98°C at ~0.1m depth) remained relatively stable. In conclusion, satellite imagery and supporting ground-based evidence suggest a pattern of gradual decline (despite some time and spatial variations) in overall heat fluxes over the past decade from the Karapiti thermal area. An analysis of satellite infrared data provides a useful and cost-effective option for monitoring of the total radiative component of surface heat-loss from relatively large areas of steaming ground, such as at Karapiti.

Original languageEnglish
Pages (from-to)1-10
Number of pages10
JournalJournal of Volcanology and Geothermal Research
Volume235-236
DOIs
Publication statusPublished - Aug 1 2012

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New Zealand
Moon
moon
craters
Landsat thematic mapper
crater
heat flux
Heat flux
Infrared radiation
Monitoring
monitoring
satellite imagery
Satellite imagery
vegetation
land surface temperature
Geothermal fields
Temperature
Hot Temperature
temperature
Boiling point

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology

Cite this

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title = "Monitoring heat flux using Landsat TM/ETM+ thermal infrared data - A case study at Karapiti ('Craters of the Moon') thermal area, New Zealand",
abstract = "Thermal infrared (TIR) data from available, daytime, Landsat-TM/ETM+ satellite imagery, supported by ground measurements, were used in this study to investigate changes between 1990 and 2011 in the radiative component of the anomalous surface heat flux emitted from the 0.5km2 Karapiti thermal area, at Wairakei Geothermal Field, Taupo, New Zealand. The geothermal radiative heat flux (net RHF), of subsurface origin, was then assessed by subtracting the re-radiated heat flux that is of solar origin, as determined using coincident satellite imagery at two external sites. The total net RHF decreased by about 7MW from 1990 to 2011. Results of a vegetation index study, using ratios of two (visible) spectral bands, implied that the area of healthy vegetation at Karapiti has progressively increased during this period. This supports the evidence for a decrease in geothermal heat flux, because the health of thermally-stressed vegetation is inversely related to shallow ground temperature. Although images of apparent land-surface temperature (LST) show large variations with time, this is attributable to ambient temperature change. Spot ground estimates of heat flux using a calorimeter also showed, on average, a decreasing trend of heat fluxes between 2000 and 2009, although several sites showed stable heat fluxes. Further supporting evidence came from repeated ground-based temperature-depth profiles, which showed that the near-surface boiling point depth lowered in levels at most sites between 2000 and 2011, although several sites located in actively-steaming bare-ground (~98°C at ~0.1m depth) remained relatively stable. In conclusion, satellite imagery and supporting ground-based evidence suggest a pattern of gradual decline (despite some time and spatial variations) in overall heat fluxes over the past decade from the Karapiti thermal area. An analysis of satellite infrared data provides a useful and cost-effective option for monitoring of the total radiative component of surface heat-loss from relatively large areas of steaming ground, such as at Karapiti.",
author = "Mia, {Md Bodruddoza} and Bromley, {Chris J.} and Yasuhiro Fujimitsu",
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AU - Mia, Md Bodruddoza

AU - Bromley, Chris J.

AU - Fujimitsu, Yasuhiro

PY - 2012/8/1

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N2 - Thermal infrared (TIR) data from available, daytime, Landsat-TM/ETM+ satellite imagery, supported by ground measurements, were used in this study to investigate changes between 1990 and 2011 in the radiative component of the anomalous surface heat flux emitted from the 0.5km2 Karapiti thermal area, at Wairakei Geothermal Field, Taupo, New Zealand. The geothermal radiative heat flux (net RHF), of subsurface origin, was then assessed by subtracting the re-radiated heat flux that is of solar origin, as determined using coincident satellite imagery at two external sites. The total net RHF decreased by about 7MW from 1990 to 2011. Results of a vegetation index study, using ratios of two (visible) spectral bands, implied that the area of healthy vegetation at Karapiti has progressively increased during this period. This supports the evidence for a decrease in geothermal heat flux, because the health of thermally-stressed vegetation is inversely related to shallow ground temperature. Although images of apparent land-surface temperature (LST) show large variations with time, this is attributable to ambient temperature change. Spot ground estimates of heat flux using a calorimeter also showed, on average, a decreasing trend of heat fluxes between 2000 and 2009, although several sites showed stable heat fluxes. Further supporting evidence came from repeated ground-based temperature-depth profiles, which showed that the near-surface boiling point depth lowered in levels at most sites between 2000 and 2011, although several sites located in actively-steaming bare-ground (~98°C at ~0.1m depth) remained relatively stable. In conclusion, satellite imagery and supporting ground-based evidence suggest a pattern of gradual decline (despite some time and spatial variations) in overall heat fluxes over the past decade from the Karapiti thermal area. An analysis of satellite infrared data provides a useful and cost-effective option for monitoring of the total radiative component of surface heat-loss from relatively large areas of steaming ground, such as at Karapiti.

AB - Thermal infrared (TIR) data from available, daytime, Landsat-TM/ETM+ satellite imagery, supported by ground measurements, were used in this study to investigate changes between 1990 and 2011 in the radiative component of the anomalous surface heat flux emitted from the 0.5km2 Karapiti thermal area, at Wairakei Geothermal Field, Taupo, New Zealand. The geothermal radiative heat flux (net RHF), of subsurface origin, was then assessed by subtracting the re-radiated heat flux that is of solar origin, as determined using coincident satellite imagery at two external sites. The total net RHF decreased by about 7MW from 1990 to 2011. Results of a vegetation index study, using ratios of two (visible) spectral bands, implied that the area of healthy vegetation at Karapiti has progressively increased during this period. This supports the evidence for a decrease in geothermal heat flux, because the health of thermally-stressed vegetation is inversely related to shallow ground temperature. Although images of apparent land-surface temperature (LST) show large variations with time, this is attributable to ambient temperature change. Spot ground estimates of heat flux using a calorimeter also showed, on average, a decreasing trend of heat fluxes between 2000 and 2009, although several sites showed stable heat fluxes. Further supporting evidence came from repeated ground-based temperature-depth profiles, which showed that the near-surface boiling point depth lowered in levels at most sites between 2000 and 2011, although several sites located in actively-steaming bare-ground (~98°C at ~0.1m depth) remained relatively stable. In conclusion, satellite imagery and supporting ground-based evidence suggest a pattern of gradual decline (despite some time and spatial variations) in overall heat fluxes over the past decade from the Karapiti thermal area. An analysis of satellite infrared data provides a useful and cost-effective option for monitoring of the total radiative component of surface heat-loss from relatively large areas of steaming ground, such as at Karapiti.

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