1 S1 Text. Appendix. 2 A rotation by an angle about an axis defined by the unit vector k (k x , k y , k z ) is geometrically 3 described by the rotation matrix [1] 4 cos (1 cos 2 )k x2 Rk ( ) (1 cos )k x k y k z sin (1 cos )k x k z k y sin (1 cos ) k x k y k z sin cos (1 cos 2 ) k y2 (1 cos )k y k z k x sin (1 cos ) k x k z k y sin (1 cos ) k y k z k x sin cos (1 cos 2 ) k z2 5 Let the 0xyz reference frame rotate with the camera. The optical axis defines the y-axis, with the 6 7 8 camera at the origin. The pan axis is vertical and fixed. The x-axis coincides with the tilt axis, which is horizontal, pans with the camera and is always perpendicular to the camera's optical axis. The camera is horizontal at the starting position, as depicted in Fig. 2 in the main text. 9 10 Consider the case where the camera is vertically tilted by an angle (the minus sign means a downward tilt) and simultaneously rotated by a pan angle . From the point of view of the camera its 11 orientation is described by a rotation Ru ( ) followed by a rotation RRu ( ) v ( ) . The unit vector 12 u (1,0,0) defines the tilt axis, v (0,0,1) is the z-axis unit vector and the unit vector Ru ( ) v 13 14 defines the vertical direction, i.e. the pan axis, after the tilt rotation. For example, point A, on the seafloor, has initial coordinates (l1 , y A0 , h) ; after the camera is rotated its coordinates become 15 16 17 sin xA l1 cos y A RRu ( ) v ( ) Ru ( ) y A0 sin cos cos cos z h sin sin cos sin A 0 l1 sin y A0 cos h Proceeding analogously for points B, C and D, after the complete rotation the coordinates of the four seafloor points become x A l1 cos y A0 sin y A l1 cos sin y A0 cos cos h sin z l sin sin y sin cos h cos 1 A0 A 18 xB l1 cos ( y A0 L1 )sin yB l1 cos sin ( y A0 L1 ) cos cos h sin z l sin sin ( y L )sin cos h cos 1 A0 1 B xC l2 cos yC 0 sin yC l2 cos sin yC 0 cos cos h sin z l sin sin y sin cos h cos C0 C 2 xD l2 cos ( yC 0 L2 )sin yD l2 cos sin ( yC 0 L2 ) cos cos h sin z l sin sin ( y L )sin cos h cos C0 2 D 2 1 (A1) 19 Relative to equation (1) in the main text, equation (A1) accounts for the more general case where y A 0 20 may not be equal to yC 0 – both coordinates are equal to f d in (1). The distances AB L1 and 21 CD L2 are also not necessarily the same. Since the image plane I remains at y f , the coordinates for the projected points on the picture are obtained in a similar fashion as for equation (2) in the main text: 22 23 24 x A z A xB z B xC z C xD z D f l1 cos y A0 sin l1 cos sin y A0 cos cos h sin f l1 sin sin y A0 sin cos h cos l1 cos sin y A0 cos cos h sin f l1 cos ( y A0 L1 ) sin l1 cos sin ( y A0 L1 ) cos cos h sin f l1 sin sin ( y A0 L1 ) sin cos h cos l1 cos sin ( y A0 L1 ) cos cos h sin f l2 cos yC 0 sin l2 cos sin yC 0 cos cos h sin f l2 sin sin yC 0 sin cos h cos l2 cos sin yC 0 cos cos h sin f l2 cos ( yC 0 L2 ) sin l2 cos sin ( yC 0 L2 ) cos cos h sin f l2 sin sin ( yC 0 L2 ) sin cos h cos l2 cos sin ( yC 0 L2 ) cos cos h sin (A2) 25 26 The camera’s rotation moves the vanishing point of the projected laser lines relative to the image center to a new position ( xV , zV ) , as depicted in Fig. 4a in the main text. The vanishing point V’ is by 27 definition the intersection point of the straight lines [A’B’] and [C’D’], described respectively by 28 z ( x xA ) / cot 1 z A z ( x xC ) / cot 2 zC 29 where the “perspective” angles 1 and 2 (see Fig. 4a in the main text) are obtained by generalizing 30 equation (3) in the main text to the present case, cot 1 x A xB l1 cos h sin sin z A z B h cos cot 2 xD xC l2 cos h sin sin z D zC h cos 31 (A3) (A4) 32 From (A3) it follows that ( xV xA ) / cot 1 z A ( xV xC ) / cot 2 zC applies at V’. Solving for 33 xV and using (A2) together with (A4), it results that 34 xV f 2 tan cos 35 From equation (11) in the main text, inserting f W / 2 tan H / 2 into the last equation yields 36 equation (15) in the main text: xV 37 38 39 zV W tan 2 tan( H / 2) (A6) Next, by adding the two equations in (A4) and solving for h , the general expression for the camera's height relative the ground, equation (22) in the main text, is obtained: h 43 44 (A5) The z-coordinate of the vanishing point is obtained by inserting (A5) into either one of the equations in (A3): 40 41 42 W tan 2 tan( H / 2) cos cos 1 cot 1 cot 2 l cos If z A zC applies (as in Fig. 1c in the main text), it follows from (A2) that y A0 yC 0 l tan (A7) 47 L1 L2 (A8) 48 Thus, let L L1 L2 . From equations (A7) and (A8) follows that the trapezoid [A’B’D’C’] in Fig. 1c 49 corresponds to a parallelogram [ABDC] on the seabed with sides l / cos and L (see Fig. 4b in the 50 main text) and inner angles 90º . Accordingly, the area of [ABDC] is S L l . 51 52 As for the special case of equation (8) in the main text, by similarity of triangles [A0C] and [A’0’C’] it follows that 53 l / cos y A l f 45 46 Analogously, if z B z D then (A9) 54 Note that f d in equation (8) corresponds to y A in (A9) and l is exchanged for l / cos . 55 From (A1) yB y A L cos cos applies, thus, by similarity of triangles [B0D] and [B’0’D’], the 56 general case of equation (9) is 57 58 59 l / cos y A L cos cos l f Combining (A9) and (A10) with (11) yields equation (17) in the main text: l l W L 1 l l 2 tan( H / 2)cos cos 3 (A10) 60 61 In many cases the vanishing point V’ lies outside the picture, as in Fig. 1c in the main text. In such a situation, the coordinates xV and zV must be calculated, so that the cosines of the tilt and pan angles 62 63 may be used in equation (19) in the main text. Therefore, consider the case depicted in Fig. 4a in the main text. At the vanishing point V’ equation (A3) becomes 64 xA xV ( zV z A )cot 1 xV xC ( zV zC )cot 2 65 Adding the two equalities in (A11) and solving for zV yields zV z A 66 67 l d s1 s2 zV z A (A14) Let H be the picture's height. Analogously to equation (11) in the main text, H obeys f H 2 tan(V / 2) Thereby, W H 2 tan( H / 2) 2 tan(V / 2) 74 75 (A13) it follows that (A12) is equivalent to 72 73 (A12) cot 1 s1 / d cot 2 s2 / d 70 71 l cot 1 cot 2 Since (see Fig. 4a in the main text) 68 69 (A11) Inserting this result into equation (A6) and solving for cos yields 2 zV cos 1 H / 2 tan(V / 2) 76 1/2 (A15) 77 Let M be the vertical size of the picture in pixels, so that H / M is the height per pixel. Hence, 78 d mH / M 79 l / s1 s2 n / n1 n2 , equation (A14) becomes and z A M / 2 m0 H / M (see Fig. 4a in the main text). Since 80 zV m0 1 n m H M 2 n1 n2 M 81 82 Inserting this equality into (A15), the cosine of the tilt angle is expressed in terms of pixel quantities directly measurable from the picture, 4 2 m 1 n m 0 cos 1 2 tan(V / 2) M 2 n1 n2 M 83 84 2 x cos 1 V 2 tan( H / 2)cos W xV x A cot 1 cot 1 cot 2 xV xA s1 l s1 s2 Using quantities in pixels (see Fig. 4a in the main text), this last equation becomes xV 1 n0 n1 n W 2 N n1 n2 N 91 92 (A17) which, by the use of (A13), is equivalent to 89 90 1/ 2 Subtracting the two equalities in equation (A11) and solving for xV ' , it follows that 87 88 (A16) which is equation (20) in the main text. Similarly, cos may be obtained from equation (A5): 85 86 1/2 Substituting xV / W into (A17), equation (21) in the main text is obtained: 2 n1 n 1 n0 cos 1 2 tan H / 2 cos 2 N n1 n2 N 93 1/2 (A18) 94 Note that the procedure for obtaining cos and cos (equations (A16) and (A18), respectively) 95 remains valid when V’ is inside the image. 96 97 References 98 1. Elliott JP, Dawber PG. Symmetry in Physics. Vol.1: Principles and Simple Applications. 99 MacMillan; 1990. 100 5