LST_DAY represents the daytime land surface temperature derived from thermal infrared bands.
It is widely used for urban heat island studies, drought and energy balance applications.
1. Definition
Land Surface Temperature (LST) is the radiative skin temperature of the land surface,
retrieved from thermal infrared (TIR) satellite measurements.
General Concept
For many products (e.g. MODIS LST), temperature is stored in Kelvin with a scale factor and then
converted to °C:
LST (°C) = LST_raw × scale − 273.15
LST_raw – original LST band value
scale – product scale factor (e.g. 0.02 for MODIS)
Typical Interpretation
Higher LST → hotter surfaces (e.g. bare soil, built-up, asphalt)