The ocean is constantly in motion. The energy that arrives into the oceanic system on the planetary scales create large scale mean flows that are constantly breaking down into smaller scales features. The most important source of energy is the differential solar heat, warmer in the equator and colder in the poles. With the water transport, also heat, nutrients, salt, organisms and chemical particles in the ocean are moved, regulating the planet whether, climate and marine ecosystems.
Both large scale and smaller scale oceanic currents, gyres and eddies, transport water masses long distances. Water masses are homogeneous bodies of seawater on their properties. These bodies of water have formed through surface processes that have their origin
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The values of temperature and salinity of the water masses are acquired on the surface and in the mixed layer by heating, cooling, rain, evaporation, wind, waves and currents. Once they sink below the mixed layer, temperature and salinity may be changed only by mixing processes with adjacent water bodies. In these depths the temperature and salinity are conservative properties as there are no significant sources or sinks in the deep ocean. Seen from this perspective the temperature and salinity are not independent variables, and their knowledge allows us to recognize water masses. Oxygen is on the other hand, a non-conservative property, is acquired in surface and and is slowly reduced over time due to oxidation of organic matter and respiration of organisms.
Currents are coherent streams of water moving through the ocean. Currents are primary forced by winds blowing across the ocean surface and by differences in temperature, density and pressure of water. Currents are also governed by Earth rotation and the location of the continents. To study the movements of a volume of water in the ocean, the Newton’s second law (the acceleration to which is subjected a water volume is proportional to the sum of
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The ocean is indeed a turbulent system and the ocean circulation is not a large scale and temporally stable phenomenon; it varies over an almost continuous frequency/wavenumber spectrum with space and time scales ranging from tens to thousands of kilometers and from days to year (Le Traon Pierre-Yves, 1999).
An instantaneous view of the ocean circulation would thus reveal areas of intense and small scale ocean currents almost everywhere and would be dominated by mesoscale variability. In particular, western boundary currents and the ACC are areas of intense mesoscale variability.
Open ocean currents which are part of the large scale gyre circulation are also often intense and narrow currents embedded with mesoscale eddies. At the eastern boundaries, superimposed on the broad equator-ward flow are energetic currents and coastal upwelling currents, which can be highly variable in space and time.
The mesoscale variability is the dominant signal in the ocean circulation. There is not a precise definition of mesoscale variability but it usually refers to a subclass of energetic motions with typical space and time scales of 50 to 500 km and 10 to 100 days.
4. “Monsoons – Definition”: Wind currents that alternated and blew east across the Indian Ocean during the summer and the opposite direction during the
Why Will The Alaskan Way Viaduct Collapse The Alaskan Way Viaduct would collapse in cause of temperature, density changes, and the layers of the Earth. The layers of the Earth are the inner core, outer core the mesosphere, asthenosphere, lithosphere, and the crust including continental and oceanic crust. In the Density Column lab we poured five different liquids into a test tube.
The waves it produces- the large, freak waves in particular- attract surfers and scientists from all across the globe who indulge in the entertainment they produce and the chance to study their patterns. In her book, The Wave: In Pursuit of the Rogues, Freaks, and Giants of the Ocean, Susan Casey follows surfers from all parts of the world and interviews world-renowned scientists to study the ocean’s inner-workings and what makes it so appealing to such a wide array
With this knowledge, we know that the time between a high and a low tide is
“Below, there would be no glint from beer cans and bottles, no windrows of cigarette butts, not plastic cups, bags, or PCB’s, DDT’s, polystyrenes, or other extoic concocts. There would be plenty of sounds in the sea from subtle snaps and sizzles of small crustaceans to warbles, grunts, pops, and hundreds of other variations produced by fish and marine mammals-but no throb of engines, no ping of depth sounders, no low rumble of mechanical or electronics subsea thunder” (Earle 6). In the book of Sea Change: A Message of the Oceans by Sylvia Earle, Sylvia predicts about how the Florida's Gulf Coast use to look like thousands years ago. The way she explained the Florida's Gulf Coast, she compared today's oceans versus how it use to look like.
Since the dawn of man, human beings have been obsessed with the ocean. There’s something about the literal sea of mystery, that incredibly vast unknown that fascinates us and appeals to our inquisitive nature and insatiable lust for knowledge. For millennia, mankind has sailed the seas in search of treasure, monsters, and adventure (although the first two haven’t always been found, the third is almost always obtained). Despite the fact our nautical technology is the best that it has ever been, the human race has explored less than five percent of the ocean and it is unlikely that we will scrape double digits any time soon. While we may be able to navigate our way across the ocean’s surface, much of what lies beneath our boats and cruise ships
The cooled air over the land moves in to take the place of the rising warm air over the water. That is how bodies of water can affect the
If you mess with the oceanic current in a major way, creating a shift even if thought to be a small one, later down the line, the after effect is a very dangerous and costly thing to keep control of, because you cannot control the nature of things not within your control. This control had not been given unto man as the animals and living things had been. Then without their prior knowledge, the Japan nuclear power plant exploded, and had not been properly cleaned up but covered up for the ongoing damage increasing the filth that oceans life would have to endure until it reaches the next and so on. A floating garbage collection reported seen from space.
Moore was sailing through the pacific when he realized that something was around him, something not of nature but of man. Moore stated, “It’s just that I couldn’t survey the surface of the ocean for any period of time while standing on deck without seeing some anthropogenic debris, something that was human in origin, float by. Not necessarily a large something, but just something” (Greenberg). The “something” that he found was broken down bits of plastic that had gone through a gyre. In the Pacific Ocean a gyre is wind and currents that circulate the water in a clockwise motion.
Continental drift makes the Earth’s climate change in many ways, ocean currents being one of them. When a continent is close to a large body of water, the water averages the temperature and administers more moisture. The ocean currents are responsible for moving water around the Earth. If land masses move closer to the North Pole, the
Disappearances of many air and sea travels over the Atlantic led many people to believe that there is a specific area of the ocean where an abundance of mysterious disappearances take place. However, some think there is a logical explanation to the madness. In February of 1954, a man named Vincent Gaddis came up with a conspiracy to explain the disappearances. Vincent Gaddis’ way of thinking is that, there had been an abundance of airline and sea travels,lost in the Bermuda Triangle.
A. There are other ways also that affects the ocean through global warming. Plenty of things that are happening to the ocean are associated to global warming. One important thing is warm water which is caused from global warming and it is harming and killing algae in the
Convection current are found in many places from the atmosphere to the ocean even in the earth's interior. Convection in the atmosphere are responsible for the distribution of heat from the warm equatorial regions to the higher
The Moon is tethered to the Earth by gravity, orbiting once every day. For the Moon to take a full cycle, it takes 27.322 days to rotate once on its axis from a New Moon or Dark Moon to, Waxing Crescent, First Quarter, Waxing Gibbous, Full Moon, Waning Gibbous, Third Quarter, Waning Crescent, and back to the New Moon. Our moon gives the ocean currents due to its gravity pulling the oceans into a wavy mess, acting like a magnet to a steel ball behind a sheet of paper, it will pull it and move it, but won’t take it off the ground due to it being to far away. But this pull gives us something called Tides, when it’s high tide, the Moon is either above that area of ocean or on the other side of the world, pulling both sides of the Earth seas (as
Energy produced by fossil fuel is largely responsible for carbon emissions, Nox’s and Sox’s leading to global warming. Concerted actions are required on the planet regarding to reduction in consumption of fossil fuels and to mitigate the carbon emission. Ocean energy can be produced from blowing wind, current of ocean, tidal waves, thermal, gradients in salinity as well as from the sources of ocean plankton. Ocean energy which has a large potential faces, some interdisciplinary; complications which are to be overcome like automation, cost reduction, speculation, instructress, environmental impacts and so forth. In future, areas that can explore the Marine Renewable Energy seascape through viable plan include proceed material, automation, informatics