The Pacific Ocean is
the largest and deepest of Earth's five oceanic divisions. It extends from the Arctic Ocean in
the north to the Southern Ocean (or,
depending on the definition, to Antarctica)
in the south, and is bounded by the continents of Asia and Australia in the west and the Americas in
the east.
At 165,250,000 square kilometers (63,800,000 square miles) in area (as defined with a southern Antarctic border), the largest division of the World Ocean and the hydrosphere covers about 46% of Earth's water surface and about 32% of the planet's total surface area, larger than its entire land area (148,000,000 km2 (57,000,000 sq mi)). The centers of both the water hemisphere and the Western Hemisphere, as well as the oceanic pole of inaccessibility, are in the Pacific Ocean.
The Pacific Ocean's mean depth is 4,000 meters (13,000 feet). The Challenger Deep in the Mariana Trench, located in the northwestern Pacific, is the deepest known point in the world, reaching a depth of 10,928 meters (35,853 feet). The Pacific also contains the deepest point in the Southern Hemisphere, the Horizon Deep in the Tonga Trench, at 10,823 meters (35,509 feet). The third deepest point on Earth, the Sirena Deep, is also located in the Mariana Trench.
Due to the effects of plate tectonics, the Pacific Ocean is currently shrinking by roughly 2.5 cm (1 in) per year on three sides, roughly averaging 0.52 km2 (0.20 sq mi) a year. By contrast, the Atlantic Ocean is increasing in size.
Along the Pacific Ocean's irregular western margins lie many seas, the largest of which are the Celebes Sea, Coral Sea, East China Sea (East Sea), Philippine Sea, Sea of Japan, South China Sea (South Sea), Sulu Sea, Tasman Sea, and Yellow Sea (West Sea of Korea). The Indonesian Seaway (including the Strait of Malacca and Torres Strait) joins the Pacific and the Indian Ocean to the west, and Drake Passage and the Strait of Magellan link the Pacific with the Atlantic Ocean on the east. To the north, the Bering Strait connects the Pacific with the Arctic Ocean.
The Pacific Ocean has most of the islands in the world. There are about 25,000 islands in the Pacific Ocean. Many tropical storms batter the islands of the Pacific. The lands around the Pacific Rim are full of volcanoes and often affected by earthquakes. Unknown Tsunamis, caused by underwater earthquakes, have devastated many islands and in some cases destroyed entire towns.
Pacific Oceans
and Heat Uptake
Ocean heat
content (OHC) or ocean
heat uptake (OHU) is the energy absorbed and stored by oceans. To calculate the ocean heat content, it is
necessary to measure ocean temperature at
many different locations and depths. The North Pacific, North Atlantic,
the Mediterranean, and the Southern Ocean all
recorded their highest heat observations for more than sixty years of global
measurements.
In 2021 scientists from around the world revealed that, per their measurement, the world oceans are hotter than ever recorded for the sixth straight year. “One way to think about this is the oceans have absorbed heat equivalent to seven Hiroshima atomic bombs detonating each second, 24 hours a day, 365 days a year.” Scientifically, the data shows that the oceans heated up by about 14 zettajoules.
In 2023, the world's oceans were again the hottest in the historical record and exceeded the previous 2022 record maximum. The five highest ocean heat observations to a depth of 2000 meters occurred in the period 2019–2023.
With improving observation in recent decades, the heat content of the upper ocean has been analyzed to have increased at an accelerating rate. Changes in ocean temperature greatly affect ecosystems in oceans and on land.
Concentrated releases in association with high sea surface temperatures help drive tropical cyclones, atmospheric rivers, atmospheric heat waves and other extreme weather events that can penetrate far inland. Altogether these processes enable the ocean to be Earth's largest thermal reservoir which functions to regulate the planet's climate; acting as both a sink and a source of energy.
Current trends phenomenon
of Climate Change
Marine Heatwave
A marine heatwave is a period of abnormally high sea surface temperatures compared to the typical temperatures in the past for a particular season and region. Unlike heatwaves on land, marine heatwaves can extend over vast areas, persist for weeks to months or even years, and occur at subsurface levels. It is clear that the ocean is warming as a result of climate change, and this rate of warming is increasing.
A marine heatwave is a period of abnormally high sea surface temperatures compared to the typical temperatures in the past for a particular season and region. Unlike heatwaves on land, marine heatwaves can extend over vast areas, persist for weeks to months or even years, and occur at subsurface levels. It is clear that the ocean is warming as a result of climate change, and this rate of warming is increasing.
The Blob
The Blob is a large mass of relatively warm water
in the Pacific Ocean off the coast of North America that was
first detected in late 2013 and continued to spread throughout 2014 and 2015.
It is an example of a marine heatwave. Sea surface temperatures indicated that the Blob persisted into
2016, but it was initially thought to have dissipated later that year.
The Blob was first detected in October 2013 and early 2014 by Nicholas Bond and his colleagues at the Joint Institute for the Study of the Atmosphere and Ocean of the University of Washington. It was detected when a large circular body of seawater did not cool as expected and remained much warmer than the average normal temperatures for that location and season.
In 2015 the atmospheric ridge causing the Blob finally disappeared. The Blob vanished shortly after in 2016. However, in its wake are many species that will take a long time to recover. Although the Blob is gone for now, scientists predict that similar marine heat waves are becoming more common due to the Earth's warming climate. Residual heat from the first blob in addition to warmer temperatures in 2019 lead to a second Blob scare. However, it was quelled by a series of storms that cooled the rising temperatures.
Caused of
increasing heat in Pacific Ocean
Environment
The Northwestern Pacific
Ocean is most susceptible to micro plastic pollution due to its proximity to
highly populated countries like Japan and China. The quantity of small plastic
fragments floating in the north-east Pacific Ocean increased a hundredfold
between 1972 and 2012. The ever-growing Great Pacific Garbage
Patch between California and
Japan is three times the size of France. An estimated 80,000 metric tons of
plastic inhabit the patch, totaling 1.8 trillion
pieces.
Nuclear
waste
From 1946 to 1958, Marshall Islands served
as the Pacific Proving Grounds, designated by the United States, and played
host to a total of 67 nuclear tests conducted
across various atolls. Several nuclear weapons were
lost in the Pacific Ocean, including one-megaton bomb that was lost during
the 1965
Philippine Sea A-4 incident.
Deep
sea mining
An emerging threat for the
Pacific Ocean is the development of deep-sea mining.
Deep-sea mining is aimed at extracting manganese nodules that
contain minerals such as magnesium, nickel, copper, zinc and cobalt. The
largest deposits of these are found in the Pacific Ocean between Mexico and
Hawaii in the Clarion Clipperton fracture zone.
Options for
reducing impacts
To
address the root cause of more frequent and more intense marine heatwaves, climate
change mitigation methods are needed to curb the increase in global
temperature and in ocean
temperatures.