Not exact matches
Increased
ocean acidification caused
by the absorption of
carbon dioxide causes bleaching, too.
The new report «Lights Out for the Reef», written
by University of Queensland coral reef biologist Selina Ward, noted that reefs were vulnerable to several different effects of climate change; including rising sea temperatures and increased
carbon dioxide in the
ocean, which causes acidification.
Some of the
carbon dioxide in the atmosphere is absorbed
by water in
oceans and rivers.
Thus, methane and
carbon dioxide together, unaccompanied
by carbon monoxide, on a rocky,
ocean - bearing world would best be interpreted as an airtight sign of anoxic life.
Carbon is constantly being recycled throughout the world: It's taken in
by plants as
carbon dioxide, for example, and is dissolved in the
oceans.
One - third of
carbon dioxide emitted
by humans enters the
oceans, making seawater more acidic, the study noted.
The simulations also suggest that the removal of excess
carbon dioxide from the atmosphere
by natural processes on land and in the
ocean will become less efficient as the planet warms.
Fish save the world billions of dollars in damages
by helping store
carbon dioxide in the
oceans
About 2.7 billion years ago, photosynthetic algae in the
oceans started making their mark, taking in
carbon dioxide as fuel and sending the
by - product — oxygen — skyward.
The
carbon they produce when building their chalk plates even helps buffer the increasing acidity in the
ocean caused
by excess
carbon dioxide in the atmosphere.
Oceans are taking in about 90 percent of the excess heat created
by human greenhouse gas emissions, but they're also absorbing some of the
carbon dioxide (CO2) itself.
As humans emit more
carbon dioxide into the atmosphere, more of the gas is absorbed
by the
oceans, gradually making the water more acidic.
But the Southern
Ocean plays a more benign role in the global
carbon budget: Its waters now take up about 50 % of the atmospheric
carbon dioxide emitted
by human activities, thanks in large part to the so - called «biological pump.»
What happens when the world moves into a warm, interglacial period isn't certain, but in 2009, a paper published in Science
by researchers found that upwelling in the Southern
Ocean increased as the last ice age waned, correlated to a rapid rise in atmospheric
carbon dioxide.
New research published today in Nature Geoscience
by Richard Zeebe, professor at the University of Hawai'i — Mānoa School of
Ocean and Earth Science and Technology (SOEST), and colleagues looks at changes of Earth's temperature and atmospheric
carbon dioxide (CO2) since the end of the age of the dinosaurs.
It may takes tens of thousands of years for
oceans to recover from the acidity caused
by increased levels of
carbon dioxide
The U.S. EPA is considering stiffening standards for the
ocean acidification caused
by rising
carbon dioxide levels in the atmosphere
«However,
ocean warming cancelled this benefit of elevated
carbon dioxide by causing stress to the animals, making them less efficient feeders and preventing the extra energy produced
by the plants from travelling through the food web to the fish.
1 One proposal, first suggested in the late 1980s
by oceanographer John Martin of the Moss Landing Marine Laboratories in California, involves seeding
ocean surfaces with iron to promote phytoplankton blooms that will soak up
carbon dioxide, eventually exporting it into the deep
ocean.
As a result — and for reasons that remain unexplained — the waters of the Southern
Ocean may have begun to release
carbon dioxide, enough to raise concentrations in the atmosphere
by more than 100 parts per million over millennia — roughly equivalent to the rise in the last 200 years.
This balance is threatened
by increasing atmospheric
carbon dioxide, which causes
ocean acidification (decreasing
ocean pH).
«That's one reason we care — the
ocean is the biggest sink of
carbon dioxide, and
by looking at nitrogen isotopes we can indirectly look at what draws down
carbon dioxide.»
Acidity may impair movement Previous research has shown that when
carbon dioxide is absorbed
by the
ocean and it becomes more acidic, concentrations of calcium carbonate drop, and that hurts shellfish and corals, which use calcium carbonate to build shells and skeletons.
When
carbon dioxide, CO2, from the atmosphere is absorbed
by the
ocean, it forms carbonic acid (the same thing that makes soda fizz), making the
ocean more acidic and decreasing the
ocean's pH. This increase in acidity makes it more difficult for many marine organisms to grow their shells and skeletons, and threatens coral reefs the world over.
Over the last few centuries, the
ocean has absorbed huge amounts of the
carbon dioxide spewed into the atmosphere
by human activities, such as burning fossil fuels.
Some scientists think that
carbon dioxide released
by the impact would have acidified the
oceans, contributing to the extinctions, so the drill team will look at whether seafloor animals just after the impact were species that tolerate low pH.
As growing
carbon dioxide gas emissions have dissolved into the world's
oceans, the average acidity of the waters has increased
by 30 % since 1750.
Ocean acidification, another change caused
by the
oceans» uptake of
carbon dioxide, also hurts corals.
Pollution of the
ocean by runoff from the land and the fouling of the air with
carbon dioxide (which is warming the
ocean and acidifying it) are accelerating and expanding the threats to the world's coastal waters.
During the spring and summer months, deep
ocean water rich in
carbon dioxide periodically wells up along the California coast when surface waters are pushed offshore
by strong winds.
One of the many downsides of too much
carbon dioxide in the atmosphere is what happens when some of that CO2 is absorbed
by the
oceans.
In July researchers from the National Oceanic and Atmospheric Administration published findings that the
oceans store almost half the anthropogenic
carbon dioxide — the CO2 produced
by humans — released into the atmosphere.
As atmospheric CO2 levels increase from burning fossil fuels, this
carbon dioxide is soaked up
by seawater and makes the
oceans more acidic.
(The
ocean currently absorbs roughly half of the greenhouse gases, primarily
carbon dioxide, that are released
by human activity.)
The uptake of fossil fuel
carbon dioxide (CO2)
by the
ocean increases seawater acidity and causes a decline in carbonate ion concentrations.
To understand where that
carbon dioxide is going, we need precise, comprehensive, ongoing data about
carbon dioxide absorption and emission
by forests, the
ocean and many other regions.
Fake paper fools global warming naysayers The man - made - global - warming - is - a-hoax crowd latched onto a study this week in the Journal of Geoclimatic Studies
by researchers at the University of Arizona's Department of Climatology, who reported that soil bacteria around the Atlantic and Pacific
oceans belch more than 300 times the
carbon dioxide released
by all fossil fuel emission, strongly implying that humans are not to blame for climate change.
High temperatures increase weathering of silicate rocks, and this sucks
carbon dioxide out of the atmosphere and into the
oceans — a process aided
by plants.
«If this conclusion is confirmed
by future observations, it would mean that the coastal
ocean will become more and more efficient at removing
carbon dioxide from the atmosphere,» said Goulven Lurallue, the paper's lead author and a researcher with Université Libre de Bruxelles in Belgium.
By manipulating the acidity of the Biosphere 2
ocean and measuring the resulting growth rates in coral between 1996 and 2003, Langdon proved that
ocean acidification from rising atmospheric
carbon dioxide would radically affect calcium carbonate — shelled marine life (pdf).
The foaming agent could interfere with
ocean ecologies or inhibit the uptake of
carbon dioxide by the
ocean — effectively negating one of the major ways that the world's
oceans fight global warming naturally.
Increased
carbon dioxide in the atmosphere boosts,
by gas - liquid equilibrium, the amount of carbonic acid in the
ocean, which in turn lowers the marine pH level.
There is, therefore, much current interest in how coccolithophore calcification might be affected
by climate change and
ocean acidification, both of which occur as atmospheric
carbon dioxide increases.
The high mortality rate is due to
ocean acidification, partly driven
by carbon dioxide emissions, according to an April 2012 study.
Gregoire created the panel earlier this year to examine the implications of dropping pH levels in seawater, a trend caused
by the
ocean's absorption of
carbon dioxide from the atmosphere.
Some scientists are linking the phenomenon to warmer waters and
ocean acidification caused
by high levels of
carbon dioxide in the atmosphere.
The finding suggests that sea life is already being affected
by changes in the
ocean's chemistry caused
by rising
carbon dioxide levels.
The presence of ample hydrogen in the moon's
ocean means that microbes — if any exist there — could use it to obtain energy
by combining the hydrogen with
carbon dioxide dissolved in the water.
An international team of 27 oceanographers churned through 13 global models and concluded that
carbon dioxide emissions could cause pH levels in the
ocean to drop from an average of 8.1 today to 7.7
by the end of the century.
The work has implications for how
ocean modelers determine the overall amounts of
carbon dioxide taken up
by the
oceans, which is typically performed through oxygen - based measurements.