Uncertainty in these projections due to potential future climate change effects
on the ocean carbon cycle (mainly through changes in temperature, ocean stratification and marine biological production and re-mineralization; see Box 7.3) are small compared to the direct effect of rising atmospheric CO2 from anthropogenic emissions.
The regional arrays provide a sampling of ocean conditions around the world that is designed to produce an integrated data set that can be used to address questions related to physical - biogeochemical coupling in eddies, phytoplankton phenology (cyclic and seasonal phenomena), nutrient supply, and climate effects
on ocean carbon cycling in selected regions.
MBARI news release on summer experiments Greenhouse - gas research by MBARI oceanographer Peter Brewer Department of Energy research
on ocean carbon disposal
Not exact matches
«Greenhouse gas emissions are going to go through the roof with a project of this kind,» said Wilderness Committee National Campaign Director Joe Foy «From escaped methane at the drill sites to the massive
carbon emissions required to cool the gas, to more escaped methane
on the long trip across the
ocean to Asia and then the emissions from burning the gas.
There was a shared sentiment that Alberta must be careful not to try to «boil the
ocean» but instead focus
on a few important levers: best - in - continent
carbon pricing with a trigger mechanism linked to oil prices, energy efficiency measures and infrastructure were identified as good areas to focus
on.
The current Wikipedia entry
on air pollution, for example, now asserts that pollution includes: «
carbon dioxide (CO2)-- a colorless, odorless, non-toxic greenhouse gas associated with
ocean acidification, emitted from sources such as combustion, cement production, and respiration.»
Nutiva is focused
on regenerative agriculture so it can sequester
carbon from the atmosphere and
oceans, putting it into the soil so the soil can hold more water, use less fertilizer and enhance nutritional elements in foods.
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.
Paris 2015 may be the last chance to agree
on global
carbon dioxide reductions before there are so many greenhouse gases in the air and the
oceans that things get really nasty.
«For example, [measuring] chlorophyll a will give you information about how much biological activity is going
on, and eventually more information about the concentration of
carbon dioxide within the
ocean and the atmosphere,» said Yoshihisa Shirayama, executive director of research at the Japan Agency for Marine - Earth Science and Technology in Tokyo.
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.
Rising anthropogenic, or human - caused,
carbon dioxide in the atmosphere may have up to twice the impact
on coastal estuaries as it does in the
oceans because the human - caused CO2 lowers the ecosystem's ability to absorb natural fluctuations of the greenhouse gas, a new study suggests.
Ocean acidification, which is a direct consequence of increased atmospheric
carbon dioxide levels, is expected to have a deleterious effect
on many marine species over the next century.
An international team examining the impact of
ocean acidification
on coral has found that a key reef - building coral can, over a relatively short period of time, acclimate to a doubling of atmospheric
carbon dioxide levels.
Previously, he has shown that the rocks beneath the
oceans could be home to the largest population of prokaryotes
on Earth, and account for one tenth of all living
carbon.
Balmy
ocean waters are putting the squeeze
on phytoplankton, tiny plants that collectively fix as much
carbon dioxide as all terrestrial greenery combined.
In fact, it will take many thousands of years for the excess
carbon dioxide to completely leave the atmosphere and be stored in the
ocean, and the effect
on temperature and sea level will last equally long.»
This global biological recordbased
on daily observations of
ocean algae and land plants from NASAs Sea - viewing Wide Field - of - View Sensor (SeaWiFS) missionwill enable scientists to study the fate of atmospheric
carbon, terrestrial plant productivity and the health of the
oceans food web.
But what has not been calculated before is the impact that the copepod's long journey and hibernation at depth has
on the ability of the
ocean to store
carbon dioxide removed from the atmosphere.
Bowen says the two relatively rapid
carbon releases (about 1,500 years each) are more consistent with warming
oceans or an undersea landslide triggering the melting of frozen methane
on the seafloor and large emissions to the atmosphere, where it became
carbon dioxide within decades.
Dust from the Sahara Desert provides most of the iron found in the Atlantic
Ocean, according to research that also sheds light
on how the
oceans help sequester
carbon dioxide
Studies
on coral, mollusks, and other
ocean denizens are helping to paint a picture of what the future might entail for specific species, should
carbon emissions continue to increase.
This newest threat follows
on the heels of overfishing, sediment deposition, nitrate pollution in some areas, coral bleaching caused by global warming, and increasing
ocean acidity caused by
carbon emissions.
However, scientists can't predict precisely what effect the
carbon dioxide currently being pulled into the
ocean from the atmosphere will have
on climate.
For example, he has said in recent years that vast
carbon dioxide emissions might ultimately cause a runaway greenhouse effect like
on Venus that would boil the
oceans and make Earth uninhabitable, the Times reported.
On Earth,
oceans absorb
carbon dioxide from the atmosphere and deposit it as carbonate rock.
In a statement published after the experiment was completed, the Alfred Wegener Institute, where Smetacek works, said the results «dampened hopes
on the potential of the Southern
Ocean to sequester significant amounts of
carbon dioxide and thus mitigate global warming.»
This paper outlines a new framework for assessing errors and their impact
on the uncertainties associated with calculating
carbon sinks
on land and in
oceans.
In his letter
on ocean thermal energy conversion (OTEC), Graham Cox suggests it could be used to fertilise surface waters with nutrient - rich deep water to promote plankton growth for
carbon capture (1 December, p 31).
You report
on a successful trial of
ocean iron - seeding to promote plankton growth and potential
carbon sequestration via the sinking...
Ultimately, the group focused its investigation
on the five strategies that appear to hold the most promise: reducing emissions, sequestering
carbon through biological means
on land and in the
ocean, storing
carbon dioxide in a liquefied form in underground geological formations and wells, increasing Earth's cloud cover and solar reflection.
The reason: the world's
oceans and forests, which scientists were counting
on to help hold off catastrophic rises in
carbon dioxide, are already so full of CO2 that they are losing their ability to absorb this climate change culprit.
Your article
on adding iron to patches of
ocean to encourage plankton growth and so capture atmospheric
carbon (21 July,...
«For most of Earth's history, most of this
carbon has been deposited not in the deep
ocean but rather
on the margins of continents.
And while
carbon dioxide is crucial for plant life, the
carbon balance
on Earth is a delicate cycle, with
oceans and land able to absorb only so much CO2.
Titan has diverse,
carbon - rich chemistry
on a surface dominated by water ice, as well as an interior
ocean.
The relationship between our future
carbon dioxide emissions and future climate change depends strongly
on the capacity of the
ocean -
carbon sink.
We would think that if an ice sheet covered the
oceans it would have had an impact
on marine production or photosynthesis and we find no
carbon isotopic evidence for this.
Because
ocean currents play a major role in transporting the planet's heat and
carbon, the ECCO simulations are being used to understand the
ocean's influence
on global climate and the melting of ice in polar regions.
The model also accounted for natural drivers of change, including the direct influence of increased
carbon dioxide
on ocean -
carbon uptake and the indirect effect that a changing climate has
on the physical state of the
ocean and its relationship to atmospheric
carbon dioxide.
In using the model to assess the
ocean -
carbon sink, the researchers assumed a «business as usual»
carbon dioxide emissions trajectory, the Representative Concentration Pathway 8.5 scenario found in the Intergovernmental Panel
on Climate Change for 2006 - 2010, where emissions continue to rise throughout the 21st century.
Now researchers at MIT and Bristol University in the United Kingdom have found that these microscopic, mixotrophic organisms may have a large impact
on the
ocean's food web and the global
carbon cycle.
«Living a «mixotrophic» lifestyle: Some tiny plankton may have big effect
on ocean's
carbon storage.»
The scientists focused
on the
ocean's biological pump, which exports organic
carbon from the euphotic zone — the well - lit, upper
ocean — through sinking particulate matter, largely from zooplankton feces and aggregates of algae.
Deploying new sensors that drift with sometimes strong currents (allowing better measurement of marine snow than sensors placed
on the
ocean floor or tethered to the surface), the team sampled the flora and fauna and measured the amount of falling
carbon material captured to assess the role of the
ocean as a true
carbon sink.
But it would have been nice to hear the authors» thoughts
on recent Japanese proposals to attempt to bioengineer even more productive living coral reefs and plant them in the Pacific to increase the power of the
oceans to absorb
carbon.
An article published in the Global Biogeochemical Cycles
on 20th of February 2018 estimates that solar radiation mineralizes 45 teragrams of terrestrial dissolved organic
carbon in the
ocean.
The research, published in Nature Geoscience and led by researchers from the Université Libre de Bruxelles, the University of Exeter, Laboratoire des Sciences du Climat et l'Environnement, the University of Hawai'i and ETH Zürich, has for the first time shown that increased leaching of
carbon from soil, mainly due to deforestation, sewage inputs and increased weathering, has resulted in less
carbon being stored
on land and more stored in rivers, streams, lakes, reservoirs, estuaries and coastal zones — environments that are together known as the «land -
ocean aquatic continuum».
When
carbon is emitted by human activities into the atmosphere it is generally thought that about half remains in the atmosphere and the remainder is stored in the
oceans and
on land.
Also facing elimination are the Orbiting
Carbon Observatory 3, which would observe
carbon dioxide flows; a mission to the space station that would have supported tests of a spectrometer intended to measure solar reflection; and Plankton, Aerosol, Cloud,
ocean Ecosystem, a satellite that would measure the colors of the
ocean to gauge the global flow of algae and the influence of
ocean aerosols
on cloud formation.