Now, new evidence from a marine sediment core from the deep Pacific points to
warmer ocean waters around Antarctica (in sync with the Milankovitch cycle)-- not greenhouse gases — as the culprit behind the thawing of the last ice age.
Not exact matches
And
around Antarctica, where even the surface
ocean water is already quite cold and dense, some of that
water in the
ocean depths, which is also carbon rich, eventually
warmed enough so that it became less dense than the
water above it.
The simulations suggest that over decades, these
warming events dramatically perturb the
ocean surface, affecting the flow of the Atlantic Meridional Overturning Circulation, a system of currents that acts like a conveyor belt moving
water around the planet.
If you decouple that ice from where it's grounded — something that currents of
warming water, already circulating
around the Antarctic coast, could do — then
water could flow beneath the inland ice and lubricate its slide into the
ocean.
That
water is relatively
warm and salty compared with other
water in the
ocean, so researchers could map its path upward and
around Antarctica.
Around the Great Barrier Reef,
warming ocean waters are becoming more acidic, bleaching the coral and threatening the rich community of life drawn to the reefs.
Oceanographer Xiao - Hai Yan of the University of Delaware in Newark and
Ocean University of China in Qingdao has studied the Western Pacific
Warm Pool — a body of
water,
warmer and less dense than the surrounding seas, that greatly expands and moves
around the Pacific during an El Niño.
Under normal conditions, the trade winds and
ocean currents in the tropical Pacific travel from the Americas to Asia, maintaining a pool of very
warm water and a related area of intense tropical rainfall
around Indonesia.
The next step was see how those factors were influenced by ENSO; while El Niños and La Niñas are defined by how much
warmer or colder than normal tropical Pacific
ocean waters are, they trigger a cascade of reactions in the atmosphere that can alter weather patterns
around the globe.
El Niño has helped to boost temperatures this year, as it leads to
warmer ocean waters in the tropical Pacific, as well as
warmer surface temperatures in many other spots
around the globe, including much of the northern half of the U.S..
Along one string of sites, or «stations,» that stretches from Antarctica to the southern Indian
Ocean, researchers have tracked the conditions of AABW — a layer of profoundly cold water less than 0 °C (it stays liquid because of its salt content, or salinity) that moves through the abyssal ocean, mixing with warmer waters as it circulates around the globe in the Southern Ocean and northward into all three of the major ocean ba
Ocean, researchers have tracked the conditions of AABW — a layer of profoundly cold
water less than 0 °C (it stays liquid because of its salt content, or salinity) that moves through the abyssal
ocean, mixing with warmer waters as it circulates around the globe in the Southern Ocean and northward into all three of the major ocean ba
ocean, mixing with
warmer waters as it circulates
around the globe in the Southern
Ocean and northward into all three of the major ocean ba
Ocean and northward into all three of the major
ocean ba
ocean basins.
For example, scientists have found that El Niño and La Niña, the periodic
warming and cooling of surface
waters in the central and eastern tropical Pacific
Ocean, are correlated with a higher probability of wet or dry conditions in different regions
around the globe.
Ocean circulation drives the movement of
warm and cold
waters around the world, so it is essential to storing and regulating heat and plays a key role in Earth's temperature and climate.
As the Earth continued to cool from Years 0.1 to 0.3 billion, a torrential rain fell that turned to steam upon hitting the still hot surface, then superheated
water, and finally collected into hot or
warm seas and
oceans above and
around cooling crustal rock leaving sediments.
Ocean currents ferry
warm and cool
water around the globe.
The research published in Nature Communications found that in the past, when
ocean temperatures
around Antarctica became more layered - with a
warm layer of
water below a cold surface layer - ice sheets and glaciers melted much faster than when the cool and
warm layers mixed more easily.
A study published on Monday in Nature Geoscience is among the first to create a detailed snapshot of how
warming ocean waters are eating away at grounding lines
around the continent.
A new paper from the Sea
Around Us Project published in the journal Nature reveals that
warmer ocean temperatures are driving marine species towards cooler, deeper
waters, and this in turn, has affected global fisheries catches.
That's weakening coral reefs
around the world, making them more vulnerable to impacts of
ocean warming and
water pollution.
Hurricanes feed off
warm water and the theory that rising
ocean temperatures are making them stronger than they would otherwise have been has been
around for a long time.
In any year, temperatures
around the world can be nudged up or down by short - term factors like volcanic eruptions or El Ninos, when
warm water spreads over much of the tropical Pacific
Ocean.
The
warm waters of the Pacific
Ocean and the awesome swell certainly make the conditions favourable for surfing
around Port Stephens.
The average
ocean temperature hovers
around 73 degrees in August, making it the
warmest ocean water off the coast of California.
The kids will love splashing
around in the
warm ocean water, but there are plenty of other things to fascinate them while on your family vacation in Costa Rica!
Most of the islands are just a speck of sand in a great
ocean, with reefs
around it and beautiful
warm water around it, making them seem like paradise.
Leading ice experts in Europe and the United States for the first time have agreed that a ring of navigable
waters has opened all
around the fringes of the cap of sea ice drifting on the
warming Arctic
Ocean.
Ocean waters around Antarctica have
warmed steadily for the past 50 years, but in addition to that, the region's shallow seas are also heating up, more quickly than others.
The current El Niño — a meteorological event in which a band of
warm water develops in the Pacific
Ocean around the equator — is about to peak.
Instead, they discuss new ways of playing
around with the aerosol judge factor needed to explain why 20th - century
warming is about half of the
warming expected for increased in GHGs; and then expand their list of fudge factors to include smaller volcanos, stratospheric
water vapor (published with no estimate of uncertainty for the predicted change in Ts), transfer of heat to the deeper
ocean (where changes in heat content are hard to accurately measure), etc..
Averaging about twelve feet long, they inhabit
warm temperate and tropical
ocean waters around the globe.
At its southeast edge, the circulation
around the feature forces a salinity gradient in the
ocean, with fresher and
warmer waters of the western Pacific lying to its west.
A2) The Sun is the source of all this energy as it is the hottest thing
around, and by the greenhouse explanation above the GHGs redistribute insolation into the
ocean until their heating from above and the tendency for
warm water to rise once again cancel each other out and the new stable (w.r.t. averaging over 24h) vertical gradient is attained.
You can watch the tall thunderstorms following the
warm ocean water as it wanders
around the tropics.»
Even if ALL the
OCEAN ICE
around the POLAR REGIONS does «melt», the newly
warmed sub-artic regions, verdant with streams and rivers, will take up much of the release to increase the proportion of FRESH LIQUID
water available on a now EXTENDED verdant land surface.
The main mechanism for wind - driven mixing into the deep
ocean (down to
around 2000 metres) is via convergence of
warm tropical surface
water in the subtropical
ocean gyres.
A greater - than - normal volume of
warm salty tropical
water was transported north with the current and this was drawn down into the
ocean in the region
around 60 ° N - where dense
water sinking occurs.
The paper discusses that melting ice will decrease the salinity of the
ocean waters around Antarctica, which will cause decreased mixing with the relatively
warmer deep
ocean waters, reducing sea surface temperatures, causing more sea ice to form.
Water Vapour Increase - started
around 1800 in response to the earliest realized
warming occurring after the 30 to 40 year timelag on GHGs» effect due to
ocean thermal inertia.
Ocean oscillations and currents could (and do) cause local effects as
warm and cold
water interchanges, but they can not cause a global effect as they just move energy
around rather than increasing it.
In addition, the
waters around these volcanoes are
warmed by the volcanic activity, creating an exciting species rich area amidst the cold Southern
Ocean, potentially containing species new to science.
Many factors — like the thermohaline circulation, which reverses direction at the poles as
warm salty
water releases heat into the air and sinks down to the bottom — are heavily influenced by the
ocean's salinity, and thus, the movement of freshwater into and
around the Arctic plays an important role in shaping both regional and global climate.
Because only very cold surface
water is able to sink, it is simple to understand that the deep
ocean can never
warm up, regardless of how
warm the surface
ocean around the world may become.
As this heat moves counter-clockwise
around the Arctic
Ocean to the north of Siberia and Alaska, it subducts, that is, it is covered by cold
water that floats above the
warm Atlantic
water.
The fact that the
oceans are
warmer now than they were, say, 30 years ago means there's about on average 4 percent more
water vapor lurking
around over the
oceans than there was, say, in the 1970s.
El Niño is a weather phenomenon where the Pacific trade winds inexplicably falter not just a few days, but for weeks or months causing a band of
warmer than usual
ocean water to develop off the Pacific coast of South America, particularly
around where Peru is.
Global climate change has contributed to the higher sea surface and sub-surface
ocean temperatures, a
warmer and moister atmosphere above the
ocean, higher
water levels
around the globe, and perhaps more precipitation in storms.»
Since that day at Pelican Cays, I have been fortunate to travel to many sites
around the globe, ranging from the
waters of the southern Pacific
Ocean to the crashing surf along the Pacific coast of North America, and what I see matches the observations made by what now is an army of scientists: The Earth's flora and fauna are changing — shifting their geographic locations, altering when they reproduce or dying wholesale — as a result of human - induced global
warming.
In any year, temperatures
around the world can be nudged up or down by short - term factors like volcanic eruptions or El Ninos, when
warm water spreads over much of the tropical Pacific
Ocean.
Climate change is
warming oceans around Earth, evaporating more
water into the atmosphere and feeding storms that could brew into hurricanes.
The
ocean waters of the deep circumpolar current that swirl
around the continent have been getting measurably
warmer and nearer the
ocean surface over the last 40 years, [continue reading...]