The team would also like to discover at what point a liquid
water ocean forms; whether it forms almost immediately or if it requires a significant buildup of heat first.
Not exact matches
The pattern the
water circulation
forms in that region is called the Indian
Ocean Gyre, one of five of the major ocean gyres of the world that scientists have identified so
Ocean Gyre, one of five of the major
ocean gyres of the world that scientists have identified so
ocean gyres of the world that scientists have identified so far.
Forming in the system's colder outer regions, where volatile compounds such as
water and carbon dioxide freeze out, makes it possible that the planets incorporated those ices and carried them along to a warmer place where they could melt, evaporate, and become
oceans and atmospheres.
This heating ought to be weak, but some unknown process seems to be amplifying it, possibly enough to melt a deep
ocean of liquid
water on Enceladus, or maybe only enough to
form smaller pools of
water within the moon's icy shell.
And across all scales, from very small controlled studies of marine plots to those of entire
ocean basins, maintaining biodiversity — the number of extant species across all
forms of marine life — appeared key to preserving fisheries,
water filtering and other so - called ecosystem services, though the correlation is not entirely clear.
If the planet is covered by an immense amount of
water, the pressure at the bottom of the
ocean will increase to such an extent that
water occurs in the
form of «Ice VII,» which does not exist on Earth.
Another 2016 study found that minerals called carbonates — which need
water to
form — are spread across the dwarf planet, suggesting that Ceres once hosted an ancient
ocean.
Generally speaking, there are two types of crust on Earth: a lighter continental crust that is rich in silicon and constitutes the dry land above sea level, and a denser oceanic crust where
water gathers in the
form of large
oceans.
Research from 2011, led by Hauri, found that the melt inclusions have plenty of
water — as much
water, in fact, as lavas
forming on the Earth's
ocean floor.
Comparing moon rocks to volcanic ones from the
ocean floor shows that Earth's
water may have stuck around even through the giant impact that
formed the moon
The oxygen content of the
ocean may be subject to frequent ups and downs in a very literal sense — that is, in the
form of the numerous sea creatures that dine near the surface at night then submerge into the safety of deeper, darker
waters at daybreak.
Climate change, in the
form of warmer
waters and increasing
ocean acidity, may exacerbate economic uncertainties.
Calcium carbonate has great scientific relevance in biomineralization and geosciences,
forming enormous scales of biological (reefs and
ocean sediments) and geological origin, which bind a huge amount of CO2 and affect the chemistry of
ocean water (1) and, with it, Earth's atmosphere and climate.
«Hurricanes almost always
form over
ocean water warmer than about 80 degrees F. in a belt of generally east - to - west flow called the trade winds.
In addition, now that sea ice blankets the Southern
Ocean off the western Antarctic Peninsula far less than before, more
water is evaporating and
forming precipitation, largely in the
form of snow.
The cemented granules had
formed in the
water, then fused after dropping to the
ocean floor.
Newly developing
ocean basins,
formed by plate tectonics and continental rifting, provide just the right conditions for rapid burial in anoxic
waters.
The warm
waters give up their heat in the bitterly cold regions monitored by OSNAP, become denser, and sink,
forming ocean - bottom currents that return southward, hugging the perimeter of the
ocean basins.
«During the evaporation of the
water from the
ocean, the
water molecules
formed by lighter isotopes will get preferentially evaporated, while during condensation the heavier isotopes will condense more effectively,» he says.
That's because a current of cold
ocean water moves from north to south along the West Coast, cooling the coastal Pacific and removing the threat of hurricanes, which
form only when low pressure systems siphon off the energy from warm
ocean water.
The resulting cold, dense
water sinks and moves northwards,
forming an important part of the global circulation of
ocean water.
When that cold, fresh
water enters the
ocean, it
forms an extra-chilly layer on the
ocean surface around the continent.
His results lend support to the theory that the
oceans were
formed by
water vapour released from the hot interior of the young Earth.
This research not only provides the first clear evidence that microorganisms were directly involved in the deposition of Earth's oldest iron formations; it also indicates that large populations of oxygen - producing cyanobacteria were at work in the shallow areas of the ancient
oceans, while deeper
water still reached by the light (the photic zone) tended to be populated by anoxyenic or micro-aerophilic iron - oxidizing bacteria which
formed the iron deposits.
According to Muehlenbachs, rocks that
formed in early
oceans should reflect this excess if comets or meteorites contributed more than 5 to 10 per cent of the
water in the primordial
oceans.
And it increases the amount of light reaching Arctic surface
waters, spurring the growth of phytoplankton, tiny organisms that
form the base of the Arctic
ocean food chain.
Wendy Panero, associate professor of earth sciences at Ohio State, and doctoral student Jeff Pigott are pursuing a different hypothesis: that Earth was
formed with entire
oceans of
water in its interior, and has been continuously supplying
water to the surface via plate tectonics ever since.
The dipole consists of a warmer than average band of
water between northern Australia and Java that
forms in conjunction with an unusually cold band of
water running northwest into the Indian
Ocean from Australia's west coast.
The discovery, involving cold, extra salty
water — brine — that
forms within openings in sea ice, adds to our understanding of how ice sheets interact with the
ocean, and may improve our ability to forecast and prepare for future sea level rise.
In 2015, James Head at Brown University and Michael Carr at the US Geological Survey estimated that the equivalent of a global
ocean a few hundred metres deep was needed to explain all the geological features that look like they were
formed by
water.
If
water temperatures in the Atlantic are higher than normal, as they are now, hurricanes, which feed off warm
ocean water, are more likely to
form.
Thus, when ice caps
form,
ocean water bears a higher ratio of the heavier isotope.
Then colder
water is pumped from 800 to 1,000 meters below the
ocean surface to condense the steam back into liquid
form.
This is why it's unlikely that anything alive is more likely to be swimming in the depths of a strange
ocean than creeping around above
water on frozen orbs, even though the complexity of that life (like the stromatolites and creepy blind life
forms thriving around undersea hot -
water vents) could be limited by how much light can reach so far into the abyss.
More likely, the
water would have
formed an
ocean occupying almost half of Mars» northern hemisphere, in some regions reaching depths greater than a mile (1.6 kilometers).
Many organic molecules needed for life could even have
formed below the
ocean floor from interactions between minerals and circulating hot
water driven these hydrothermal ven systems.
Water constantly moves through a vast global cycle, evaporating from lakes and
oceans,
forming clouds, precipitating as rain or snow, then flowing back down to the
ocean.
«This
form of graphene is extremely resistant to biofilm formation, which has promise for places like
water - treatment plants, oil - drilling operations, hospitals and
ocean applications like underwater pipes that are sensitive to fouling,» says Tour.
Most of the
water is in liquid
form, meaning these planets are primarily
ocean!
These mineral particles likely
formed in scalding
water bubbling from rock below the moon's ice - capped
ocean, new lab studies suggest.
As the hurricane
forms, deeper
water in the
ocean is driven to the surface.
We also know that Mars once had free - flowing
water, too, in the
form of lakes and rivers, and potentially
oceans as well.
It is the dense
waters formed by this process that set up the deep
ocean current patterns.
The sinkhole is also where the freshwater supplying the subterranean estuary comes from — rainfall and salt
water from the
ocean feed into it to
form the distinct
water layers found there.
Corals, too, face direct threat from
ocean acidification, which, as it robs
ocean water of carbonate ions, impedes their ability to
form skeletons.
In particular, carbonic acid is
formed and hydrogen ions are released, and as a result the pH of the
ocean surface
waters decrease (making them more acidic).
This constant flexing of Europa by Jupiter's immense gravity melts its interior in the same way it melts that of neighboring moon Io, in essence keeping the
water ice layers in the interior of Europa in a liquid state that
form a global underground
ocean.
Deltas
form as rivers empty their
water and sediment into another body of
water, such as an
ocean, lake, or another river.
The planets» densities, now known much more precisely than before, suggest that some of them could have up to 5 percent of their mass in the
form of
water — about 250 times more than Earth's
oceans.
During glaciation,
water was taken from the
oceans to
form the ice at high latitudes, thus global sea level drops by about 120 meters, exposing the continental shelves and
forming land - bridges between land - masses for animals to migrate.