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Our results showed that the robot-obtained map corresponded well with a geo-referenced map.
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The risk map corresponds well to field observations on the occurrence of rills and gullies.
The coherence map corresponds well with the map of InSAR height (Fig. 2b).
The coherence map corresponds well with the map of InSAR height (Fig. 2b).
A biomass change map based on interferometry corresponded well to a very accurate map derived from repeated scanning with airborne laser.
A biomass change map based on interferometry corresponded well to a very accurate map derived from repeated acquisitions with airborne laser scanning (ALS).
The models corresponded well with published range maps (Lynch 1979; Eisenberg and Redford 2000; Ridgely and Greenfield 2001) and assessments based upon personal observations in the field (TBS, BM, PJ, CMK, CJS).
In the high-density map, the QTL associated with flowering-related traits corresponded well to the Ppd-B1 locus on chromosome 2B and the VRN-D1 locus (Supplementary Fig. S4).
Moreover, predicted spatial distributions of the total fracture spacing and the uniaxial compressive strength, for example, corresponded well with drill core and tunnel mapping results.
Model errors were acceptable (cross-validated RMSE = 2.04 °C) and the resulting map of apparent temperature, calibrated for a typical hot summer day, corresponded well with past temperature research in the area.
The location of the DArT markers corresponded well to previously published durum wheat DArT maps with a few exceptions.
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CEO of Professional Science Editing for Scientists @ prosciediting.com