Land surface temperature (LST) is a kinetic quantity, independent of wavelength, that represents the thermodynamic temperature of the skin layer of a given surface, i.e. it is a measure of how hot or cold the surface of the Earth would feel to the touch. For ground-based, airborne, and space borne remote sensing instruments LST is the aggregated radiometric surface temperature based on a measure of radiance. Therefore, in the literature, LST is also referred to as (directional) radiometric temperature or skin temperature. When derived from radiometric measurements of remote sensing instruments, LST represents the aggregated radiometric surface temperature of the ensemble of components within the sensor's field of view (Norman and Becker, 1995). This definition has been adopted by various international groups, e.g. CEOS WGCV, GCOS, ESA GlobTemperature, and ILSTE-WG.
Units: The unit of LST is Kelvin [K]. Degree Celsius [°C] is also commonly used.
Norman, G., and Becker, F. (1995). Terminology in thermal infrared remote sensing of natural surfaces. Agricultural and Forest Meteorology, Volume: 77, Issue: 3-4, Pages: 153-166,
DOI: 10.1016/0168-1923(95)02259-Z
Emissivity a wavelength-dependent quantity defined as the ratio of the radiance actually emitted by an isothermal,homogeneous body and the radiance emitted by a black body at the same thermodynamic temperature (Norman and Becker 1995).
Units: Dimensionless.
Validation stage 3 (LPV validation stage hierarchy) - The highest LPV validation stage reached for satellite-derived land surface temperature and emissivity products. While the number of in situ validation stations is indeed limited, 'radiance based-validation' extends available sites considerably. Radiance-based validation uses static in-situ emissivities, e.g. determined from field samples in the lab or simply well known (as for dense vegetation or water) sites. This extends the number of sites sufficiently to be considered globally representative
The purpose of validation is to characterize product uncertainties and to evaluate the performance of retrieval algorithms. Four categories of validation methods (Schneider et al., 2012) are commonly used to assess a satellite LST product's compliance with its specifications:
The above categories complement each other and provide different information about the quality of an LST product. Due to a lack of global reference datasets, methods from all four categories are required to achieve Stage-3 validation status. Over homogeneous sites state-of-the-art satellite LST and ground-based LST are generally expected to agree with each to within 1-2 K.
Current methods and best practises for land surface temperature and emissivity product validation are described in the following documents:
Guillevic, P., Göttsche, F., Nickeson, J., Hulley, G., Ghent, D., Yu, Y., Trigo, I., Hook, S., Sobrino, J.A., Remedios, J., Román, M. & Camacho, F. (2018). Land Surface Temperature Product Validation Best Practice Protocol. Version 1.0. In P. Guillevic, F. Göttsche, J. Nickeson & M. Román (Eds.), Good Practices for Satellite-Derived Land Product Validation (p. 58): Land Product Validation Subgroup (WGCV/CEOS), doi:10.5067/doc/ceoswgcv/lpv/lst.001
Göttsche, F., Olesen, F.S., Høyer, J.L., Wimmer, W., and Nightingale, T. (2017). Fiducial Reference Measurements for Validation of Surface Temperature from Satellites (FRM4STS).Technical Report 3 - A Framework to Verify the Field Performance of TIR FRM. Internal Publication, OFE- D120-V1-Iss-3-Ver-1-ISSUED, Issue 3 Revision 0, page 1-75.
Schneider, P., Ghent, D., Corlett, G., Prata, F., and Remedios, J., 2012. AATSR validation: LST validation protocol. Internal publication, UL-NILU-ESA-LST-LVP Issue 1 Revision 0, page 1-39.
Currently available reference data for satellite-derived LST and emissivity validation are often campaign-based. For a few sites longer time series are available:
A more complete and detailed list of current in-situ LST validation sites is provided here.
Recent Advances in Quantitative Remote Sensing (RAQRS): Symposium organized by the University of Valencia, Spain. 21-25 September 2020, Abstract Deadline: 1 March 2020
LST CCI User Workshop: 24-26 June 2020 at Met Office, UK
AGU Fall Meeting, December 9-13, 2019, Moscone Center, San Francisco, CA, USA. Session GC44C - Taking the Temperature of the Earth: Uncertainties, Trends, and Applications Across All Earth Surface Domains I
The 5th Sentinel-3 Validation Team Meeting, 7-9 May 2019 - ESA/ESRIN, Frascati, Italy.
EGU General Assembly 2019: 'Taking the temperature of the Earth: observing surface temperature across all domains in a changing climate', Session: CL5.13/AS4.30/CR1.8/OS4.28 (Climate: Past, Present, Future), 7-12 April 2019, Vienna, Austria.
2019 Joint Satellite Conference, 28 Sep - 4 Oct 2019, Westin Boston Waterfront Hotel, Boston, MA, USA; submission deadline: 1 Mar 2019.