T10 temperature is Tradiative (band 10 and 11), but not the temperature of the surface (LST). For the temperature of the surface is necessary to apply a single channel or split window equation.
T_Brillo=K_2/ln[K_1/L_λsensor +1]
http://landsat.gsfc.nasa.gov/?p=5689
For LST with single channel equation aplied:
LST(B10L8)=(L_λsensor-L_(λ↑)-τ(1-ε) L_(λ↓))/τε
L_λsensor radiance sensor (energy unit)
L_(λ↑) radiance atmosphere up (energy unit)
L_(λ↓)) radiance atmosphere down (energy unit)
τ transmissivity (adimensional)
ε emissivity (adimensional)
(1) Barsi et al., (2003) on line model
TIRS Landsat 8 (2) Jiménez-Muñoz et al. (2014), good single-channel algorithm
(3) Pasapera y Rivas (2014) General description and aplication L8 TIRS (single and split window the problem is that it is written in Spanish)
T10 temperature is Tradiative (band 10 and 11), but not the temperature of the surface (LST). For the temperature of the surface is necessary to apply a single channel or split window equation.
T_Brillo=K_2/ln[K_1/L_λsensor +1]
http://landsat.gsfc.nasa.gov/?p=5689
For LST with single channel equation aplied:
LST(B10L8)=(L_λsensor-L_(λ↑)-τ(1-ε) L_(λ↓))/τε
L_λsensor radiance sensor (energy unit)
L_(λ↑) radiance atmosphere up (energy unit)
L_(λ↓)) radiance atmosphere down (energy unit)
τ transmissivity (adimensional)
ε emissivity (adimensional)
(1) Barsi et al., (2003) on line model
TIRS Landsat 8 (2) Jiménez-Muñoz et al. (2014), good single-channel algorithm
(3) Pasapera y Rivas (2014) General description and aplication L8 TIRS (single and split window the problem is that it is written in Spanish)