meridional plane
1meridional projection — noun : a projection of a sphere on a plane parallel to a meridian plane through the point of projection …
2Astigmatism — An optical system with astigmatism is one where rays that propagate in two perpendicular planes have different foci. If an optical system with astigmatism is used to form an image of a cross, the vertical and horizontal lines will be in sharp… …
3Ray (optics) — Ray of light redirects here. For other uses, see Ray of light (disambiguation). In optics, a ray is an idealized narrow beam of light. Rays are used to model the propagation of light through an optical system, by dividing the real light field up… …
4Cardinal point (optics) — For other uses, see Cardinal point (disambiguation). In Gaussian optics, the cardinal points consist of three pairs of points located on the optical axis of an ideal, rotationally symmetric, focal, optical system. For ideal systems, the basic… …
5Cromwell Current — Contents 1 Townsend Cromwell 2 Discovery 3 Detailed data 4 …
6Optical aberration — v · d · e Optical aberration …
7ASIE - Géographie physique — L’Asie est le plus vaste des continents: 44 millions de kilomètres carrés. Elle s’étend sur 75 degrés de latitude et, en tenant compte des îles, sur 92 degrés (de la Severnaïa Zemlia, ou Terre du Nord, 810 de latitude nord, à l’île Roti, 110 de… …
8GEOGRAPHICAL SURVEY — Names The name Ereẓ Israel (the Land of Israel) designates the land which, according to the Bible was promised as an inheritance to the Israelite tribes. In the course of time it came to be regarded first by the Jews and then also by the… …
9Ethereal being — Water nymph by John Collier, 1923. Ethereal beings, according to some belief systems and occult theories, are mystic entities that usually are not made of ordinary matter. Despite the fact that they are believed to be essentially incorporeal,… …
10Primitive equations — The primitive equations are a set of nonlinear differential equations that are used to approximate global atmospheric flow and are used in most atmospheric models. They consist of three main sets of equations: # Conservation of momentum :… …
