2021
DOI: 10.1016/j.jag.2020.102283
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Detecting geothermal anomalies using Landsat 8 thermal infrared remotely sensed data

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Cited by 23 publications
(12 citation statements)
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“…Within the study period (June-October), NDVI was produced with a linear interpolation between observational dates, and therefore NDVI values were retrieved specifically for those dates when mosquito samples were taken and counted. Concerning Landsat 8 LST, no ready-to-use product exists; therefore, it was computed using the methodology described in [27,28]. Due to the fact that the Landsat 8 acquisitions were not available for the desirable days, MODIS daytime LST (MOD11A1v006 product) at 1 km spatial resolution was used to obtain information on the temporal trend of LST between the Landsat 8 acquisition dates (Figure 2).…”
Section: Mosquito Dna Barcodingmentioning
confidence: 99%
“…Within the study period (June-October), NDVI was produced with a linear interpolation between observational dates, and therefore NDVI values were retrieved specifically for those dates when mosquito samples were taken and counted. Concerning Landsat 8 LST, no ready-to-use product exists; therefore, it was computed using the methodology described in [27,28]. Due to the fact that the Landsat 8 acquisitions were not available for the desirable days, MODIS daytime LST (MOD11A1v006 product) at 1 km spatial resolution was used to obtain information on the temporal trend of LST between the Landsat 8 acquisition dates (Figure 2).…”
Section: Mosquito Dna Barcodingmentioning
confidence: 99%
“…The Land Surface Temperature (LST) obtained by remote sensing for an entire city seems better suited to describing this variability than the air temperature measured by a relatively coarse network of local weather stations. LST is not the same as air temperature but is closely related to the near-surface air temperature; it is considered a primary factor affecting the energy exchange of the near-surface layers of the atmosphere (Wang et al 2019;Gemitzi et al 2021). It accurately characterizes the thermal environment at the city scale (Guo et al 2016), and it is widely used to assess UHI effect.…”
Section: Introductionmentioning
confidence: 99%
“…Due to the difficulty in quantitatively measuring the surface temperature due to pixel saturation problems or atmospheric attenuation, some studies are based on determining pixel value thresholds by isolating the background temperature found in each image. The anomalous pixel value may be above average plus a standard deviation (σ), as in [ 24 ], above average +2σ [ 25 ], or with multiple thresholds [ 26 ], since a maximum temperature in one image can represent a normality scenario in another [ 16 , 27 ].…”
Section: Introductionmentioning
confidence: 99%