Estimation of Land Surface Temperature From MODIS Data for the Atmosphere With Air Temperature Inversion Profile

Abstract

Air temperature inversion (ATI), which usually occurs at the near surface boundary layer in the atmosphere, influences the thermal path atmospheric upwelling and downwelling radiances. Because it is difficult to determine the occurrence of temperature inversion from satellite data, the influence of ATI on the retrieval of land surface temperature (LST) was not considered in the development of LST retrieval algorithm. This paper aims to analyze and reduce the influence of ATI on LST retrieval in the generalized split-window (GSW) algorithm. The GSW coefficients are reparameterized by using the ATI profiles from the thermodynamic initial guess retrieval cloud-free database. Comparison of the root-mean-square errors calculated before and after using the reparameterized coefficients in the GSW algorithm from the numerical simulations showed that the LST retrieval accuracy could be improved by 0.71 K for viewing zenith angle equivalent to 60°. Intercomparisons using the moderate resolution imaging spectroradiometer products MOD11_L2/MYD11_L2 and in situ LST measured at the Hailar field site in northeastern Inner Mongolia, China, showed that the LST retrieval accuracy could be improved by 0.4 K using the reparamerization coefficients in the GSW algorithm when the atmosphere is occurred by ATI.

Keywords

• Air temperature inversion (ATI)
• generalized split-window (GSW) algorithm
• land surface temperature (LST)
• moderate resolution imaging spectroradiometer (MODIS)