RTTOV (radiative transfer code)
Given an atmospheric profile of temperature, variable gas concentrations, cloud and surface properties RTTOV calculates radiances and brightness temperatures. The only mandatory input is water vapour. Optionally ozone, carbon dioxide, nitrous oxide, methane and carbon monoxide can be variable with all other constituents assumed to be constant. The range of temperatures and water vapour concentrations over which the optical depth computations are valid depends on the training datasets which were used. The spectral range of the RTTOV9.1 model is 3-20 micrometres (500 – 3000 cm-1) in the infrared.
Surface emissivity model which parameterizes surface emissivity. FASTEM2 computes the surface emissivity averaged over all facets representing the surface of the ocean and an effective path correction factor for the down-welling brightness temperature. FASTEM2 is applicable for frequencies between 10 and 220 GHz, for earth incidence angles less than 60 degrees.
- Eyre J. R. 1991 A fast radiative transfer model for satellite sounding systems. ECMWF Research Dept. Tech. Memo. 176 (available from the librarian at ECMWF).
- Matricardi, M., F. Chevallier and S. Tjemkes 2001 An improved general fast radiative transfer model for the assimilation of radiance observations. ECMWF Research Dept. Tech. Memo. 345. http://www.ecmwf.int/publications
- Saunders R.W., M. Matricardi and P. Brunel 1999 An Improved Fast Radiative Transfer Model for Assimilation of Satellite Radiance Observations. Quart. J.Royal Meteorol. Soc., 125, 1407-1425.
- http://nwpsaf.eu/deliverables/rtm RTTOV homepage
- http://research.metoffice.gov.uk/research/interproj/nwpsaf/rtm/rttov_applications/simulated_imagery.html Example use of RTTOV with the Unified Model
- http://cimss.ssec.wisc.edu/itwg/groups/rtwg/fastrt.html Exaplanation of tangent linear, adjoint and K radiative transfer models.