Samudra Arktik
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Samudra di Bumi |
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Samudra Arktik adalah samudra yang terletak di daerah Kutub Utara, merupakan yang terkecil dari 5 samudra dunia (setelah Samudra Pasifik, Samudra Atlantik, Samudra Hindia, dan Samudra Selatan), dan yang terdangkal.
It occupies a roughly circular basin and covers an area of about 14,090,000 km² (5,440,000 sq mi). Nearly landlocked, the ocean is surrounded by the land masses of Europe, Asia, North America, and Greenland and a number of islands, as well as by the Barents, Beaufort, Chukchi, Kara, Laptev, East Siberian, Lincoln, Wandel, Greenland, and Norwegian seas. It is connected to the Pacific Ocean by the Bering Strait and to the Atlantic Ocean through the Greenland Sea.
An underwater ocean ridge, the Lomonosov ridge, divides the Arctic Ocean into two basins: the Eurasian, or Nansen, Basin, which is between 4,000 and 4,500 m (13,000 and 15,000 ft) deep, and the North American, or Hyperborean, Basin, which is about 4,000 m deep. The topography of the ocean bottom is marked by fault-block ridges, plains of the abyssal zone, ocean deeps, and basins.
The greatest inflow of water comes from the Atlantic by way of the Norwegian Current, which then flows along the Eurasian coast. Water also enters from the Pacific via the Bering Strait. The East Greenland Current carries the major outflow. Temperature and salinity vary seasonally as the ice cover melts and freezes. Ice covers most of the ocean surface year-round, causing subfreezing temperatures much of the time. The Arctic is a major source of very cold air that inevitably moves toward the equator, meeting with warmer air in the middle latitudes and causing rain and snow. Little marine life exists where the ocean surface is covered with ice throughout the year. Marine life abounds in open areas, especially the more southerly waters. The ocean's major ports are the Russian cities of Murmansk and Arkhangelsk (Archangel). The Arctic Ocean is important as the shortest air route between the Pacific coast of North America and Europe.
Daerah
Kebanyakan badan air di daerah utara Lingkaran Arktik
Koordinat Geografis
90 00 N, 0 00 E
Referensi Peta
Daerah Arktik
Area
- total:14.056 million km²
- catatan: termasuk Teluk Baffin, Laut Barents, Laut Beaufort, Laut Chukchi, Laut Siberian Timur, Laut Greenland, Teluk Hudson, Selat Hudson, Laut Kara, Laut Laptev, Northwest Passage, Sungai Back's dan other tributary bodies of water
Perbandingan Area
Sedikit kurang dari 1.5 kali ukuran luas Amerika SerikatUS
Garis pantai
45,389 km
Iklim
Polar climate characterized by persistent cold and relatively narrow annual temperature ranges; winters characterized by continuous darkness, cold and stable weather conditions, and clear skies; summers characterized by continuous daylight, damp and foggy weather, and weak cyclones with rain or snow
Daerah
Central surface covered by a perennial drifting polar icepack that averages about 3 meters in thickness, although pressure ridges may be three times that size; clockwise drift pattern in the Beaufort Gyral Stream, but nearly straight-line movement from the New Siberian Islands (Russia) to Denmark Strait (between Greenland and Iceland); the icepack is surrounded by open seas during the summer, but more than doubles in size during the winter and extends to the encircling landmasses; the ocean floor is about 50% continental shelf (the highest percentage of any ocean) with the remainder a central basin interrupted by three submarine ridges (Alpha Cordillera, Nansen Cordillera, and Lomonosov Ridge)