“…These conditions plus integrals (14) completely coincide with those obtained by Bykov [26], [27], [28] if we transform ellipsoidal to spheroidal coordinates, and have clear geometrical interpretation. The integral for S 1 corresponds to the difference in lengths of the two geodesic curves on η r between two points P 1 = (ξ r , η r , φ 1 ) and P 2 = (ξ r , η r , φ 2 ).…”