Landsat Surface Temperature Scaling: Kelvin, Celsius and QA
The Landsat Collection 2 Level-2 surface-temperature encoding uses a documented conversion to Kelvin.
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The Landsat Collection 2 Level-2 surface-temperature encoding uses a documented conversion to Kelvin.
Brightness temperature is derived from measured radiance under a blackbody-equivalent convention.
Optical reflectance and radar scattering observe different interactions with the surface.
Texture features describe spatial patterns in radar intensity rather than a new physical band.
Radar wavelength affects scattering interactions with vegetation structure and surface roughness.
Temporal SAR statistics summarize scattering variability across acquisitions.
InSAR uses phase differences to estimate motion projected along the radar line of sight under a processing model.
Coherence measures the consistency of complex radar observations over a local estimation support.
A SAR intensity ratio compares calibrated power between observations.
Smooth open water often produces low backscatter in suitable radar geometry, making intensity useful for flood screening.
Radar incidence angle influences the observed scattering and the ground footprint.
Polarization describes the transmitted and received electric-field orientation.
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