This article was automatically translated from the original Turkish version.
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Oceans, covering approximately 71% of the surface of World, are the planet’s largest water masses. The five major ocean—the Pacific, Atlantic, Indian, Southern, and Arctic Oceans—are not only vast bodies of water but also critical climate regulators, the planet’s largest reservoirs of biological diversity, and pivotal nodes of ecosystems center. The physical and chemical properties of oceans play critical roles in the planet’s heat and gas exchange, while their currents help shape global weather patterns and climate. These massive water masses are also of great importance in terms of biological diversity and ecological balance.
Oceans are distinguished by their physical and chemical characteristics including salinity, temperature, density, and currents like. The average salinity is around 3.5%, but this varies depending on temperature, evaporation, and precipitation levels. As depth increases, temperature decreases and pressure rises. Consequently, different depths of the ocean support distinct ecosystems.
The salinity of ocean water originates from dissolved minerals and ions. The most abundant ions are sodium and chloride, which determine the salty taste of sea water. Salinity is generally higher in equatorial regions and lower near the poles. This is due to higher rates of evaporation in equatorial zones and greater freshwater input from melting ice and precipitation in polar regions sweet.
Ocean surface temperatures can reach up to 30°C in equatorial regions but drop to as low as -2°C at the poles. As one moves from the surface toward deeper layers, temperature declines rapidly, forming a distinct zone known as the thermocline. The thermocline typically occurs between 200 and 1000 meters depth, where temperature decreases sharply.
Ocean currents involve horizontal and vertical movements of water. These currents are driven by various factors including winds, temperature differences, salinity variations, and the Dönme rotation of the Earth. Warm water currents, such as the Gulf Stream, transport warm water from the equator toward the poles, while cold water currents bring cold water from polar regions toward the equator. Deep ocean currents are driven by differences in density movement.
Oceans play a vital role in the global carbon cycle by regulating gas exchange between the atmosphere and water. Marine plants and phytoplankton absorb large quantities of carbon dioxide and produce oxygen. In addition, oceans are among the most biologically diverse ecosystems on Earth row.
Oceans are divided into five distinct layers: the epipelagic (sunlight zone), mesopelagic (twilight zone), bathypelagic (midnight zone), abyssopelagic (deep zone), and hadalpelagic (trenches). Each layer has unique environmental conditions and supports specialized organisms adapted to those conditions day.
Ocean currents regulate temperature distribution and determine regional climates. For example, El Niño and La Niña events in the Pacific can cause major shifts in global weather patterns. Oceans also help mitigate global warming by storing vast amounts of heat.
Modern oceans worldwide face a range of threats stemming from human activities. Some of these include:
Oceans are one of the planet’s largest and most important natural resources. Their physical and chemical properties, biodiversity, and influence on climate make them an inseparable part of the Earth’s ecosystem. However, due to threats from human activities, their ecosystems are under significant danger. Protecting oceans is essential for a sustainable future.

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Physical and Chemical Properties of Oceans
Salinity
Temperature
Currents
The Role of Oceans in Ecosystems
Biodiversity and Ocean Layers
Impact on Climate
Threats Facing Oceans