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Drainage information was derived from SOI toposheet.
Useful information was derived from both approaches, although the RSM fit better to the experimental results.
The last information was derived from the the reports of National Statistics Service of Greece (Tables 1, 5).
Land use classes were derived from Landsat-TM data while topographic information was derived from DTED data.
All the information was derived from expert knowledge developed over more than 12 years of agronomic experiments in Madagascar.
Protein-ligand atomic contact information was derived from a "nonredundant dataset" (NRD) of over 3000 X-ray crystal structures of protein-ligand complexes.
In this case, prior information was derived from the worldwide database of unrest at calderas similar to CFc (Newhall and Dzurisin 1988).
The comparison reveals a good match of the pattern of changes of both parameters; however, more detailed information was derived from the Earth observation data.
The incident solar wind and associated magnetic field information was derived from the five-minute resolution data of the Advanced Composition Explorer (ACE) satellite which was at a distance of 240 R e from the Earth in the sunward direction.
The map also shows the glacial limits for the Late Wisconsinan and for the maximum extent of ice prior to Late Wisconsinan time; this information was derived from many of the source maps cited in Soller.
The subcellular localization information was derived from Swiss-Prot annotations which are based on experimental evidence.
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