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Is The Atlantic Ocean Colder Than The Pacific
Jerome Namias Former Research Astronomer, Scripps Institute of Oceanography, University of California, San Diego, La Jolla, 1970–77; former Director, Extended Forecasting Division, National Atmospheric Administration, National …
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Clifford A. Barnes Former Professor Emeritus of Oceanography at the University of Washington, Seattle. Author of many articles about the sea.
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In recent days, the massive search for a submarine that went missing while descending into the North Atlantic to examine the wreckage of the Titanic has refocused on the question: who should pay for the full investigation?
Scientists say that the submarine Titan has suffered a serious accident that could have killed its pilot and four passengers immediately during the high tide in the North Atlantic Ocean.
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One day after discovering that the Titan has sunk, officials search the seas for clues and identify the international accident investigator;
Rescuers in a remote part of the Atlantic race race against time to find the missing ship before five people on a mission to document the Titanic’s wreckage run out of oxygen.
The landmass of the Atlantic Ocean is about one-fifth of the Earth’s surface at about 31,568,000 square kilometers (81,760,000 sq mi) and therefore 32,870,000 square kilometers (85,133,000 sq mi).
The Atlantic Ocean is 11,962 meters (3,646 ft) deep and 27,493 meters (8,380 ft) deep in the Puerto Rico Trench, north of the island of Puerto Rico.
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A prominent feature of the Atlantic Ocean is the Mid-Atlantic Ridge, a large central ridge that runs the entire length of the Atlantic Ocean, making up the middle third of the ocean and extending 1,600 miles. ) in width. In some areas of the Mid-Atlantic it rises above the ocean and forms islands.
The surface water of the North Atlantic Ocean has a higher salinity than any other ocean, reaching a value of more than 37 parts per million at latitudes from 20° to 30° N. The salinity value of the Atlantic Ocean is highest in the North Atlantic, at 35.5 parts per thousand, and lowest in the South Atlantic, at 34.5 parts per thousand.
Every year, the Atlantic Ocean provides millions of tons of fish and other seafood for human consumption, including lobster, haddock, cod, mackerel, herring, menhaden, scallops, shrimp, mussels, oysters, and mussels. blue
The Atlantic Ocean, a body of salt water that covers about one-fifth of the Earth’s land area and separates the continents of Europe and Africa in the east and North America and South America in the west. The name of the sea, derived from Greek mythology, means “Sea of Atlas”. It is the second largest after the Pacific Ocean.
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The Atlantic Ocean is generally S-shaped and narrow relative to its length. The landmass of the Atlantic Ocean is 31,568,000 square kilometers (81,760,000 sq mi), with a total area of 32,870,000 square kilometers (85,133,000 sq mi). ). It is 11,962 meters (3,646 feet) deep and 27,493 meters (8,380 feet) deep in the Puerto Rico Trench, in the northern part of the island of Puerto Rico.
The width of the ocean varies greatly from east to west. There are 2,060 miles (3,320 km) between Newfoundland and Ireland; in the south it extends more than 3,000 kilometers before narrowing again, so that the distance between Cape Sao Roca, Brazil, and Cape Palmas, Liberia, is only 1,770 kilometers. In the south it widens again and is bordered by a gentle sea near the island; between Cape Horn and the Cape of Good Hope, the sea meets the border with the South Sea at 60°S latitude and extends for about 3,200 km (5,200 km wide).
Although it is not the largest ocean in the world, the Atlantic Ocean has a very large area. The continent on both sides of the Atlantic tends to slide towards it, so that it receives the waters of most of the great rivers of the world; among them are the Saint Lawrence, Mississippi, Orinoco, Amazon, Rio de la Plata, Congo, Nigeria, Loire, Rhine, Elbe and major rivers that flow into the Mediterranean, Black and Baltic seas. Unlike the South Atlantic, the North Atlantic is rich in islands, coastlines and rivers. The latter includes the Caribbean Sea, the Gulf of Mexico and the Gulf of St. Lawrence, and the Hudson and Baffin Bays in the west and the Baltic, North, Mediterranean and Black Seas in the east.
This article is about the nature and character of man and the Atlantic Ocean in general. For a detailed discussion of the ocean’s physical and mechanical properties and the geology of the Atlantic Ocean,
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Different boundaries have been used to define mainly the northern, but also the southern boundary of the Atlantic Ocean. There is no universally accepted agreement. In the north, the situation is even more complicated because the Arctic Ocean is often considered an ocean based on the Atlantic Ocean. That’s because the Arctic Basin – from the Bering Ranges across the North Pole to Svalbard and Greenland – is like a semi-enclosed basin (that is, surrounded by land, which hosts a large number of rivers and streams). , has a large share of the continent, and relatively small). However, in this article the Arctic Ocean is considered a special case.
Attempts to define the boundaries of the open water between the Atlantic and North Seas often rely on arbitrary line connections or alignments; the two most common latitudes are 65°N and the Arctic Circle (66°30′N). An arbitrary method is to draw a line from Greenland to Iceland following the Greenland-Iceland Rise and from Iceland to the Faroe Islands near the Faroe-Iceland Rise, then north of the Faroe Islands at relatively low altitudes from the Våring Plain to the coast of western Norway somewhere around 70°N. Perhaps the most appropriate way to set the boundary is to follow the difference between the waters characteristic of the Arctic and the Atlantic: the warm and salty waters of the Norwegian Sea formed the Atlantic Ocean, and the cold waters, from the bottom of the Greenland Sea to the Arctic.
The southern limit of the Atlantic Ocean is uncertain, although the name Atlantic Ocean is given to the waters south of 60°S latitude around Antarctica. The most recognized boundary between the South Atlantic Ocean and the Indian Ocean is a line running south from Cape Agulhas, in southern Africa, to the meridian of 20°E to 60°S. The Pacific Ocean passes through the Drake Passage between Cape Horn at the tip of South America and the Antarctic Peninsula.
A prominent feature of the Atlantic floor is the Mid-Atlantic Ridge, a large central ridge that runs the length of the Atlantic Ocean, reaching about one-third of the way up the ocean floor and about 1,600 miles wide. This feature, although large in size, is only part of the Atlantic Ocean.
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In some areas of the Mid-Atlantic it rises above the ocean and forms islands. Iceland, rising from its summit, is rent by the extension of the central plain. To the east and west of the mountain, at 12,000 and 18,000 meters (3,700 to 5,500 feet) below sea level, the plains seem to be relatively flat, but parts of the land are as mountainous as the Mid-Atlantic Mountains, while other parts are very flat. The first is the mountains; the latter are hellish valleys formed above a vast expanse of mud filled with deep depressions. Large ancient volcanoes are found singly or in rows in the plains; they rise to join and sometimes, islands.
When the continents meet and the mid-Atlantic ridge is left behind, one encounters first the abyssal plain and then the smooth, flowing surface of the continent. These wide channels are at a height of 8,000 to 15,000 feet (2,400 to 4,500 meters) at
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