INFLUENCE OF CALIBRATION PARAMETERS ON

Camera Calibration Parameters AIR UW value std. dev. value std. dev. Principal distance mm 25.801 0.006 26.208 0.002 Principal Point x mm −0.026 0.002 −0.058 0.003 Principal Point y mm −0.144 0.003 −0.207 0.002 K 1 1.842e-004 1.2e-006 1.663e-004 6.1e-007 K 2 −3.030e-007 7.4e-009 −2.582e-007 3.4e-009 K 3 - - - - P 1 - - 6.582e-006 1.2e-006 P 2 - - 1.620e-005 8.7e-007 Table 3. Comparison between camera calibration in water UW and in air. Only statistically significant additional parameters are computed. a b Figure 8. a Radial and b decentering distortion curves: the curves in red are related to the camera calibration in air, the curves in blue to the camera calibration underwater. A distortion map displays according to a colour scale map the difference between the ideal pixel position no distortion and the actual pixel position due to the influence of radial and decentring distortions determined through camera calibration. As depicted in the figure and expected, the maximum difference is reached at the borders, whose magnitude is comparable with the differences highlighted in the distortion curves. An asymmetric behaviour can be also observed, likely due to the small in-plane misalignment between the lens entrance pupil and dome surface centre of curvature, slightly bigger along the Y axis. Figure 9. Difference between in air and in water distortion maps.

5. INFLUENCE OF CALIBRATION PARAMETERS ON

UNDERWATER 3D OBJECT RECOSTRUCTION The previous sections have shown that misalignment between dome port centre and lens EP modifies the lens distortion and, in particular, can introduce a decentring component. While up to now the investigation has been concentrated in image space, the aim of the following analysis is to expand the results in object space. In particular, the study aims at understanding if neglecting the decentring distortion produces relevant deformation in the reconstructed object. In the followings, two peculiar case studies are presented: the first experiment is designed to resemble a typical cultural heritage acquisition, with a small object surveyed at a big image scale with a circular and closed camera network; the second case involves the acquisition of an elongated body, surveyed with an aerial-like camera network with the inclusion of convergent images. 5.1 Ancient amphora – circular camera network The ancient amphora height ≈ 50cm shown in Figure 10a is employed as test object and is measured and reconstructed both in air and underwater. The acquisition in air, considered the reference or ground truth to verify the underwater results, is carried out using a DSLR Nikon D750 camera with a 50 mm lens and a ground sample distance GSD of about 0.1 mm. The system used underwater is the NiMAR pressure housing with dome lens port and the Nikon D300 with 24mm lens presented before. The acquisition of the amphora is realised in the pool immediately after Fig. 10b, in the same environmental conditions and camera settings i.e., fixed focusing distance of the underwater calibration Section 4, obtaining a GSD of about 0.3 mm. Different calibration procedures for the underwater acquisition are tested and verified against the reference object: a. Full pre-calibration: the images are oriented using as camera calibration parameters the full set Table 3 derived from the underwater system calibration presented in Section 4. b. Pre-calibration with only radial distortion: the images are oriented using another set of parameters derived from the underwater calibration, solving only for radial distortion. c. Structure from motion SfM self-calibration: a self- calibrating bundle adjustment is performed to estimate in This contribution has been peer-reviewed. doi:10.5194isprsarchives-XL-3-W4-127-2016 132 one-step solution both camera calibration parameters with only radial distortion and image orientation. The dense image matching is performed both for the reference and three underwater calibration approaches at ¼ of the original image resolution i.e., double of the original GSD. From the dense point clouds, polygonal mesh models are generated with a mean spatial resolution of 0.5 mm. Figure 11a and Figure 11b show a detail of the in-air reference model and underwater calibration procedure a. The comparisons with the reference model do not highlight either significant deformation in the geometry or substantial differences between the different underwater calibration approaches. As an example, the differences between the in-air model and the model from method a and c are shown in Figure 11c and Figure 11d, respectively. In all the cases 95 of differences are within ±0.5 mm. 5.2 Elongated ship gash – aerial-like camera network In 2012, the Italian cruise ships “Costa Concordia” partially sunk off the coast of a small island in the Mediterranean Sea after the collision against a rock. The produced 60m long gash was situated on the above-the-water side of the stranded ship and extended at the current waterline 4m above and 4m below the sea surface. The technique developed for surveying and modelling the ship part interested by the collision Fig. 12a is detailed presented in previous works Menna et al., 2013; Nocerino, 2015. Here, the analysis is focused on the underwater camera calibration and its influence in object space when an elongated object is measured. For the Costa Concordia, the same underwater camera system under investigation NiMAR pressure housing with dome lens port and the Nikon D300 with 24mm lens is used and also in this case, decentring distortion parameters are statistically significant. About 800 underwater images are taken according to a photogrammetric aerial-like strip scheme, with 4 overlapping strips at different depths, assuring a forward overlap of ca. 80 along strip and a sidelap of ca. 40 between two adjacent strips. Convergent images are also included in the camera network. The mean object distance is 3m, providing a GSD of about 0.7 mm. The underwater mesh in Figure 12a is obtained including the decentring distortion. To show the influence of neglecting decentring component in the bundle adjustment, in Figure 12b the Euclidean distances in meters for the processing with and without decentring distortion parameters are presented as colour map. The differences reach a maximum value of about 6 cm.

6. CONCLUSIONS