| English | Hungarian |
| "Baltic Sea Regions" Group | "Balti-tengeri régiók" csoport |
| Baltic Sea States Subregional Cooperation | Balti-tengeri Államok Szubregionális Együttműködése |
| Committee on Safe Seas and the Prevention of Pollution from Ships | a tengeri közlekedés biztonságával és a hajókról történő szennyezés megelőzésével foglalkozó bizottság |
| International Agreement on the Use of INMARSAT Ship Earth Stations within the Territorial Sea and Ports | nemzetközi megállapodás a hajókon telepíthető INMARSAT földi állomások területi vizeken és kikötőkben való használatáról |
| International Convention for the Safety of Life at Sea | SOLAS-egyezmény |
| Law of the Sea Convention | Tengerjogi Egyezmény |
| North Sea-Channel interregional group | "Északi-tenger–La Manche csatorna" régióközi csoport |
| North Sea - English Channel interregional group | "Északi-tenger–La Manche csatorna" régióközi csoport |
| "North Sea" Group | "Északi-tenger–La Manche csatorna" régióközi csoport |
| sea and air transport | tengeri és légi szállítás |
| sea based wind turbine | tengeri létesítmény |
| sea circulation Large-scale horizontal water motion within an ocean. The way energy from the sun, stored in the sea, is transported around the world. The currents explain, for example, why the UK has ice-free ports in winter, while St. Petersburg, at the same latitude as the Shetland Islands, needs ice breakers. Evidence is growing that the world's ocean circulation was very different during the last ice age and has changed several times in the distant past, with dramatic effects on climate. The oceans are vital as storehouses, as they absorb more than half the sun's heat reaching the earth. This heat, which is primarily absorbed near the equator is carried around the world and released elsewhere, creating currents which last up to 1.000 years. As the Earth rotates and the wind acts upon the surface, currents carry warm tropical water to the cooler parts of the world. The strength and direction of the currents are affected by landmasses, bottlenecks through narrow straits, and even the shape of the sea-bed. When the warm water reaches polar regions its heat evaporates into the atmosphere, reducing its temperature and increasing its density. When sea-water freezes it leaves salt behind in the unfrozen water and this cold water sinks into the ocean and begins to flow back to the tropics. Eventually it is heated and begins the cycle all over again | tengerkörforgás |
| United Nations Convention on the Law of the Sea | Tengerjogi Egyezmény |
| Wadden Sea The Wadden sea is a shallow sea extending along the North Sea coasts of The Netherlands, Germany and Denmark. It is a highly dynamic ecosystem with tidal channels, sands, mud flats, salt marshes, beaches, dunes, river mouths and a transition zone to the North Sea, the offshore zone. Most parts of the Wadden Sea, in particular in The Netherlands and Lower Saxony, are sheltered by barrier islands and contain smaller or wider areas of intertidal flats. The present form of the Wadden Sea is the result of both natural forces and action by man. Twice a day, on average, 15 km3 of sea water enter the Wadden sea. With the water from the North Sea, large amount of sand and silt are imported which settle in places with little water movement. During low tides large parts of the Wadden Sea emerge. These so-called tidal flats cover about 2/3 of the tidal area and are one of its most characteristic features. Nowhere in the world can such a large unbroken stretch of tidal flats be found. They accountfor 60% of all tidal areas in Europe and North Africa | Watt-tenger |
| Working Party on the Law of the Sea | tengerjogi munkacsoport |
