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Observation of a local gravity potential isosurface by airborne lidar of Lake Balaton, Hungary

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Figure

Figure 1. Map of the study area, including quasi-geoid heights, bathymetry of Lake Balaton and flight pattern
Figure 2. (a) Map of lidar-measured ellipsoidal water surface heights (inside flight strip outlines) and modeled gravity potential isosurfaceheight (background raster) with the same elevation color scheme
Figure 3. Scatterplot of water surface ellipsoidal heights (cor-to lidar height model resolution was used for this graph
Figure 4. Water-level recordings with respect to LMLL of all 9water-level gauges around Lake Balaton, during the 4 flight days.Triangles in the map depict the water gauges (colour coded to thewater level graphs), rectangles crossing all graphs show actual flighttimes of lidar strips.
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