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![Figure 8. Vertical residuals vs % Vertical residual [m]](https://thumb-ap.123doks.com/thumbv2/123dok/3243734.1397690/4.595.52.288.151.327/figure-vertical-residuals-vs-vertical-residual-m.webp)
![Figure 14. Vertical displacement detection [m]](https://thumb-ap.123doks.com/thumbv2/123dok/3243734.1397690/5.595.324.516.396.521/figure-vertical-displacement-detection-m.webp)
![Figure 16. Coordinates differences [m]– mass market receiver and geodetic antenna](https://thumb-ap.123doks.com/thumbv2/123dok/3243734.1397690/6.595.56.291.460.593/figure-coordinates-differences-mass-market-receiver-geodetic-antenna.webp)
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In partnership with the World Bank's OpenDRI and with the technical collaboration of ITHACA, a non-profit association that works on acquisition, management and
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XL-5/W3, 2013 The Role of Geomatics in Hydrogeological Risk, 27 – 28
The platform, successfully tested using an autonomous robot, import the tracking data of each team or mobile means sent to the field, the coordinates of points
Broadly speaking active 3D imaging sensors that can be used for close-range applications can be categorized into the following classes (see more details in Guidi
We highlight the effectiveness of high resolution DTMs derived by terrestrial laser scanner survey for the automatic recognition of geomorphic signatures of erosion or
The analysis carried out in this study, applying the bi- dimensional hydro-morphological model MIKE21C and the mono-bidimensional model SOBEK, indicates that
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XL-5/W3, 2013 The Role of Geomatics in Hydrogeological Risk, 27 – 28
We define the pressure as the combination of probability and risk elements; this means, that we assess the degree of influence of pressure and threat and we combine with the degree
