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The maps are then made available for anyone to see online.
The distance maps are then used to reshape the MD energy funnel.
Mineral prospectivity maps are then obtained by combining the results with a geographical information system.
Cortical activities related to orientation maps are then obtained by projection on a suitable cortical Fourier basis.
The resulting LC maps are then used in conjunction with the height information to compute 2D and 3D USCs.
Stability maps are then obtained for clamped free uniform beams as well as clamped free stepped beams.
Similar(18)
Axial (DP) and radial diffusivity (DR) maps were then generated using these data.
Permafrost maps were then derived from MAGT predictions (Data Citation 1: PANGAEA https://doi.org/10.1594/PANGAEA.893881).org/10.1594/PANGAEA.893881
The maps were then used to analyze the system according to three key resilience characteristics.
These maps were then aggregated to MODIS resolution (i.e. 1 km) for comparison.
Wilderness perception maps were then compared with current land use classifications in a spatial overlay.
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