Oceans
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Oceans | |
---|---|
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Location | Earth |
Type | Saltwater |
Primary inflows | Rivers, underwater springs |
Primary outflows | Evaporation, water cycle |
Catchment area | Global |
Basin countries | Worldwide |
Surface area | Approximately 361 million square kilometers |
Average depth | Average: 3,688 meters |
Max. depth | 10,994 meters (Mariana Trench) |
Water volume | Approximately 1.332 billion cubic kilometers |
Shore length1 | 377,000 kilometers |
Islands | Thousands |
Settlements | Coastal cities worldwide |
1 Shore length is not a well-defined measure. |
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The oceans cover about 71% of the Earth's surface and are a major component of the planet's hydrosphere. Comprising the largest habitat on Earth, oceans are integral to life, influencing the weather and climate patterns, supporting a diverse range of biomes and ecosystems, and providing vital resources including food, minerals, and energy.
Composition and characteristics[edit | edit source]
Oceans are primarily composed of salt water with an average salinity of about 3.5%. This salinity can vary in different areas due to the influx of freshwater from rivers, rainfall, and melting ice. The oceans are also rich in minerals and provide habitats through various physical features such as coral reefs, seamounts, trenches, and volcanic islands.
Ocean zones[edit | edit source]
The ocean can be divided into different zones:
- The Epipelagic zone (sunlight zone) extends from the surface to about 200 meters. It is where most of the visible light exists and photosynthesis can occur.
- The Mesopelagic zone (twilight zone) stretches from 200 meters to 1,000 meters. Light diminishes significantly in this zone, and the pressure increases.
- The Bathypelagic zone (midnight zone) ranges from 1,000 meters to 4,000 meters. It is characterized by complete darkness and very high pressures.
- The Abyssopelagic zone and Hadalpelagic zone are deeper still, with the latter found in deep oceanic trenches.
Marine life[edit | edit source]
Oceans are home to a diverse array of marine life, from microscopic plankton to the largest mammals on Earth, such as the blue whale. Marine organisms play crucial roles in the biogeochemical cycles that regulate the Earth's environment.
Human interaction[edit | edit source]
Human activities impact the oceans through fishing, marine pollution, and the extraction of marine resources. Climate change also affects ocean temperatures, sea levels, and ocean currents, which in turn affect global climate systems.
Conservation[edit | edit source]
Efforts to conserve and sustainably manage the oceans include marine protected areas, regulations on overfishing, and initiatives to reduce marine pollution. International agreements such as the United Nations Convention on the Law of the Sea (UNCLOS) play a crucial role in the governance of global ocean resources.
See also[edit | edit source]
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Contributors: Prab R. Tumpati, MD