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. 2008 Sep 3;8(9):5397–5425. doi: 10.3390/s8095397

Table 1.

Description of the three NDVI NOAA-AVHRR data sets used in this study [adapted from 27, 30, 31, 34, Los personal communication, updated version of 36, 64, 69, 70].

PAL GIMMS FASIR
Data Set Origins (and its spatial resolution) NOAA-AVHRR GAC 1B (4 km) NOAA-AVHRR GAC 1B (4 km) Radiance in PAL dataset (8 km) [32]
Instrument and change in times 7, 9, 11, 14 7, 9, 11, 9 (descending), 14, 16 7, 9, 11, 14
Known temporal span 1981-2001 1981-2006 1982-1999
Temporal resolution 10 days 15 days 10 days
Spatial resolution 8 km 8 km 8 km
Spatial compositing Forward, nearest neighbor mapping. Selection of the 4 km pixel with the maximum NDVI value for the 8 km output bin. Only pixels within 42° of nadir are considered. Forward, nearest neighbor mapping. Selection of the 4 km pixel with the maximum NDVI value for the 8 km output bin. Inherited from PAL series.
Temporal compositing Maximum NDVI values composition of the 10-days images [60]. Maximum NDVI values composition of the 15-days images [60]. Inherited from PAL series.
Radiometric corrections Calibration with pre-flight constants modified by degradation over time [61], based on the use of desert invariant calibration targets. NOAA-7 to NOAA-14 channels 1 and 2 calibrations using the Vermote and Kaufman parameters [62]. NOAA-16 channels calibrations using pre-flight values. Data further adjustment using invariant desert targets [28]. Data correction following the Los technique of invariant desert targets [28].
Viewing and illumination corrections No specific corrections have been applied. Correction of illumination and viewing angle effects using the adaptive empirical mode decomposition (EMD) method [63]. Correction of illumination and viewing angle effects with Bidirectional Reflectance Distribution Function (BRDF) techniques for Pathfinder radiances [64].
Cloud corrections Based on Cloud Advanced Very High Resolution Radiometer (CLAVR) algorithm [65]. Based on thermal band. Based on thermal band and reconstruction of tropical evergreen broadleaf vegetation data with a maximum filter.
Stratospheric aerosols correction No corrections. Volcanic aerosol correction for 1982-1984 and 1991- 1994 [66, 67]. Volcanic aerosol correction for 1982-1984 and 1991-1994 [66].
Molecular absorption and scattering corrections Ozone absorption from the Total Ozone Mapping Spectrometer (TOMS) data set, and Rayleigh scattering [68]. No corrections. Inherited from PAL series.
Manual checking On every layer of the composite files. On navigation accuracy, data drop outs, bad scan lines, and other strange values. On navigation accuracy, data drop outs, bad scan lines, and other strange values.
Noise attenuation Not applied. Removal of noise and attenuation of cloud and missing pixels effects with Kriging interpolation. Replacement of extreme outliers and missing data with the long-term mean. Posterior restoration of outliers caused by cloud interferences and short-term atmospheric effects through Fourier Adjustment.
Scaling procedures Not applied. Match with SPOT Vegetation NDVI data during overlapping period [34]. Data extrapolation for winter needleleaf evergreen areas.