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Infrared Emissivity Sources

Spectral Libraries

ASTER Spectral Library Version 1.2

The ASTER spectral library includes data from three other spectral libraries: the Johns Hopkins University (JHU) Spectral Library the Jet Propulsion Laboratory (JPL) Spectral Library, and the United States Geological Survey (USGS - Reston) Spectral Library.

MODIS UCSB Emissivity Library

Emissivity measurements of natural and manmade materials that may be used as a source of spectral emissivities at the component level in the TIR BRDF models to calculate the scene emissivities. Samples of emissivity spectra are separated into four categories:
  • Water, ice, and snow
  • Soil and Minerals
  • Vegetation
  • Manmade materials

LOPEX - Leaf Optical Properties Experiment

An experiment was organized in the Joint Research Centre at Ispra during the summer of 1993 in which a data set associating visible / infrared spectra of vegetation elements (leaves, conifer needles, stems, etc) with physical measurements and biochemical analyses was constructed. About 70 leaf samples representative of more than 50 species of woody and herbaceous plants (4 Gymnosperms, 9 Monocotyledons, and 37 Dicotyledons) were obtained from trees, crops and plants in the area of the JRC

Infrared Emissivity Atlases

UW/CIMSS Baseline Fit Global Infrared Land Surface Emissivity Database

A global infrared land surface emissivity database with high spectral and high spatial resolution is introduced. For a given month, a spectrum of emissivity from 3.7 to 14.3 micron is available from this database for every latitude/longitude point globally at 0.05 degree resolution.

CIMSS AIRS Spectral Variance Emissivity Dataset

A global infrared land surface emissivity dataset retrieved from the AIRS sensor aboard NOAA AQUA satellite.

EUMETSAT LandSAF Land Surface Emissivity (EM)

Land Surface emissivity for SEVIRI/Meteosat (IR) channels and broad-band values within the 3-14 micron band. EM is available for the Meteosat disk, on a pixel-by-pixel basis.

NOAA/NESDIS AIRS Emissivity Global Datasets

1. AIRS emissivity regression derived from 20 AIRS channels then interpolated to all wavelengths.
2. AIRS emissivity physical retrieved then interpolated to all wavelengths.

MODIS LST/Emissivity Product

MODIS Land Surface Temperature and Emissivity (LST/E) products provide per-grid temperature and emissivity values. MOD11B1 and MYD11B1 - daily level 3 LST product at 5km (V4) or 6km (V5) spatial resolution gridded in the Sinusoidal projection.
Emissivity retrieved at MODIS bands 20,22,23,29, & 31-32 (3.75,3.96,4.05,8.55,11.03,12.02 µm) also available in the daily level 3 global CMG LST products (MOD11C1 and MYD11C1) at 0.05o latitude/longitude grids.

The MOD43B1 BRDF/Albedo Model Parameters Product (MODIS/Terra BRDF/Albedo Model_1 16-Day L3 Global 1km SIN Grid) supplies the weighting parameters associated with the RossThickLiSparseReciprocal BRDF model that best describes the anisotropy of each pixel. Model parameters are provided for MODIS spectral bands 1-7 (0.659, 0.865, 0.470, 0.555, 1.24, 1.64, 2.13µm) as well as for three broad bands (0.3-0.7µm, 0.7-5.0µm, and 0.3-5.0µm).

The MODIS Surface-Reflectance Product (MOD 09) is computed from the MODIS Level 1B land bands 1, 2, 3, 4, 5, 6, and 7 (centered at 648 nm, 858 nm, 470 nm, 555 nm, 1240 nm, 1640 nm, and 2130 nm, respectively). The product is an estimate of the surface spectral reflectance for each band as it would have been measured at ground level if there were no atmospheric scattering or absorption.
Coverage: Global land surface (Level 2G, 3)
Spatial/Temporal Characteristics: Bands 1 and 2, 250 m; bands 3-7, 500 m; daylight data only

Infrared Surface Property Modelling

This software code simulates the transfer of solar radiation in a plant canopy and provides accurate estimates of the bidirectional reflectance of such a system as a function of the geometry of illumination and observation, as well as of the physical and structural properties of the canopy.
It can simulate the reflectance of a canopy of finite depth and includes the contribution of the underlying ground surface. This model also allows the plant canopy to be described through such variables as the number, size and orientation of the leaves, as well as the total height of the canopy. A turbid medium approach is used to represent the contribution to the total reflectance due the light scattering at orders higher than one.

Radiative transfer model which calculates the leaf hemispherical reflectance and transmittance from 400 to 2500 nm. Scattering is described by the refractive index of leaf materials (n) and by a parameter characterizing the leaf mesophyll structure (N). Absorption is calculated from the concentrations of the biochimicals and the specific absorption corresponding coefficients.