The values derived by the ECS represent a stabilization of temperatures, and when systems
like ocean carbon sinks are added to the mix, stabilization can take millennia.
Not exact matches
These sensors could reveal patterns that help explain why the tropical Pacific emits
carbon dioxide, rather than absorbing it
like most of the rest of
ocean.
In addition to temperature, wind, and solar radiation data, the Pacific saildrones are measuring how the
ocean and air exchange gases
like carbon dioxide and oxygen, and they are using Doppler instruments to gauge currents coursing up to 100 meters below the surface.
The researchers also studied variables related to other
ocean plant groups,
like diatoms, which build glass shells that carry
carbon to the deep sea, sequestering it from the atmosphere.
Hurricane - force winds whip the
ocean so fiercely that the seawater belches dissolved
carbon dioxide (CO2) into the atmosphere
like a shaken bottle of soda, scientists have discovered.
The seas» absorption of human - generated
carbon dioxide from the atmosphere is well documented, along with the harm it is causing
ocean creatures
like shellfish.
«Recent studies have shown that there's substantial lateral
carbon exports from these ecosystems toward the coastal
ocean and that is something that we also would
like to understand,» said Vargas.
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.
It survived in hydrogen and
carbon dioxide levels
like those there, and coped with temperatures from 0 °C to 90 °C, and pressures up to 50 Earth atmospheres — both likely to be found in its
oceans (Nature Communications, doi.org/ck2q).
That's a process playing out throughout the Southern
Ocean, but scientists don't have a good grasp on it or how sudden changes
like the loss of a huge hunk of ice will alter
carbon uptake.
In applying them, they found that a more realistic representation of the marine ecosystem helped the
ocean to take up and store
carbon at similar rates regardless of global changes in physical properties,
like temperature, salinity and circulation.
Carbon sinks will become
carbon emitters -
like forests, permafrost, and the
oceans.
C. Carreau, ASPERA - 4 & MAG teams, Venus Express, ESA Annotated image illustrating loss of hydrogen through plasma wake Venus may have lost
oceans of water due to a runaway greenhouse effect which evaporated water into the upper atmosphere, where ultraviolet light dissociated water into ionized atomic hydrogen and oxygen (some later incorporated into
carbon dioxide) that were blown away by the Solar wind due to the lack of a strong magnetic field
like the Earth's (more).
They need to know: what a GHG is and how the GHE works; the
carbon cycle; how climate has changed over the entire geologic history of the planet; how the climate has changed recently (relatively speaking); the main variables of climate
like temperature, rainfall, etc.; the role of the sun, atmosphere and
oceans on climate.
There are other factors (changes in the natural sources of emissions in a warmed environment, changes in the function of traditional
carbon sinks in a warmed environment, tipping points
like increase forest fire activity in a warmed environment, etc.) that also play a significant role in the truly important number, which is accumulation of CO2 / e in the atmosphere and
ocean acidification.
While factors
like the possible climate buffering influence of the
oceans are imperfectly understood, the academy panel said, «if
carbon dioxide continues to increase, the study group finds no reason to doubt that climate changes will result and no reason to believe that these changes will be negligible.»
Flannery's book suggests that covering something
like 9 % of the world's
oceans with seaweed farms could sequester the equivalent of the entire world's
carbon emissions one day.
For example, using chemicals to make the planet more reflective might cool things a bit, but it would do nothing to reduce other greenhouse - gas impacts,
like rising acidity in the
oceans as they absorb more
carbon dioxide.
I'd
like to ask a general question: since the
oceans are taking up about 1/3 of the anthropogenic
carbon emissions, what is the opinion now of the scientific community about when the
ocean surface layers will get saturated and this
carbon sink (on relatively short timescales) will start to diminish?
We continue to see study after study showing the negative effects of too much
carbon dioxide in the atmosphere, in the
oceans, and yet some would
like to believe that's a good thing.
Obviously the «cap and trade» approach to putting out the fire will subsidize all sorts of dubious projects
like carbon - sequestration in the
oceans as the fire still burns.
Because while these may seem
like distinct issues, our
oceans are actually being hit by a double whammy when it comes to
carbon emissions:
Like all such research, the study offers a measure of how little we know of the mechanics of life, atmosphere,
ocean and rock − and, in particular, the
carbon cycle.
As acids go, H2CO3 is relatively innocuous — we drink it all the time in Coke and other carbonated beverages — but in sufficient quantities it can change the water's pH. Already, humans have pumped enough
carbon into the
oceans — some hundred and twenty billion tons — to produce a.1 decline in surface pH. Since pH,
like the Richter scale, is a logarithmic measure, a.1 drop represents a rise in acidity of about thirty per cent.
The study will use a combination of complex computer models to replicate past weather patterns in the Atlantic
Ocean, Caribbean Sea and Gulf, and use the results, along with estimates of future production of man - made greenhouse gases
like carbon dioxide and methane to predict Gulf hurricane activity.
Expecting less than 5 % of Earths surface to filter the air mass from the other 95 % given actual air circulation patterns is patently absurd compared to natural CO2 scrubbing mechanisms
like the biological
carbon cycles, or Henry's law (which is leading to
ocean acidification.
In between the atmosphere and what we release, there is the
ocean which acts
like a buffer or think a battery which first soaks up most of released
carbon.
«
Like climate change,
ocean acidification is a growing global problem that will intensify with continued
carbon dioxide emissions and has the potential to change marine ecosystems and affect benefits to society,» the report said.
Instead, world leaders have pandered and caved to the powerful fossil fuel lobby: rubber stamping massive
carbon - intensive infrastructure, unlocking billions of tonnes of new
carbon in hard - to - reach places
like the deep offshore
ocean, the arctic, or hard - to - extract resources
like tar sands, and proceeded to design energy policy around scenarios incompatible with a safe global climate.
Instead, world leaders have pandered and caved to the powerful fossil fuel lobby: rubber stamping massive
carbon - intensive infrastructure, unlocking billions of tonnes of new
carbon in hard - to - reach places
like the deep offshore
ocean,
And while indicators
like ocean heat content may respond more quickly or dramatically to the
carbon emissions that cause climate change, surface temperature is more closely related to the effects of climate change — and the effects, after all, are what climate policies at any level are intended to ease.
«[The research] demonstrates that proposed technological solutions,
like CDR, to the problems of global warming and
ocean acidification are no substitute for reducing
carbon emissions, which remains the safest and most reliable path for avoiding dangerous climate change.»
In tranquil, well - behaved parts of the
ocean like near the Galapagos, it would be probably easier to document changes in the
carbon content of the upper
ocean than it would be on land.
«natural causes can only produce — volcanoes popping off and things
like that and coming out of the
ocean — only produce about one gigaton per year, so there's just no question that human activity is producing a massively large proportion of the
carbon dioxide.»
Transparent jellyfish -
like creatures known as a salps, considered by many a low member in the
ocean food web, may be more important to the fate of the greenhouse gas
carbon dioxide in the
ocean than previously thought.
When atmospheric
carbon dioxide is absorbed into the
ocean, it reacts to produce carbonic acid, increasing the acidity of seawater and diminishing the amount of a key building block (carbonate) used by marine species
like shellfish and corals to make their shells and skeletons.
And natural causes can only produce — volcanoes popping off and things
like that and coming out of the
ocean — only produce about one gigaton per year, so there's just no question that human activity is producing a massively large proportion of the
carbon dioxide.
For me, that means I'd
like to see it broken down, which Coby has done well so far, by (these are just examples i'd
like to see): Factors and evidence supporting or effectively debunking a)
ocean acidity, which in itself has produced a number of alarming effects including less saline density in turn causing a slowing of thermohaline circulation (such as the gulf stream) b) photosynthesis -
carbon sinks vs. sources or any direction that you'd
like to take using what science knows CO2 to have an effect on.
Broader economic approaches, however, can attach monetary values to non-market impacts, referred to as externalities, placing an economic value on ecosystem services
like breathable air,
carbon capture and storage (in forests and
oceans) and usable water.
Carbon - removal strategies, as the name implies, remove
carbon dioxide from the atmosphere and store it through various means, such as in soils, trees, underground reservoirs, rocks, the
ocean and even products
like concrete and
carbon fiber.
This change in patterns of deep -
ocean sedimentation will result in a curious, dark band of carbonate - free rock — rather
like that which is seen in sediments from the Palaeocene - Eocene thermal maximum, an episode of severe greenhouse warming brought on by the release of pent - up
carbon 56m years ago.
The combination of all these forces — consumption, deforestation, agriculture and food, emissions — underscores more than ever the value of a comprehensive measure
like the Ecological Footprint that takes into account all competing demands on the biosphere, including CO2 emissions and the capacity of our forests and
oceans to absorb
carbon.
The first place that
carbon moves from the atmosphere into the
ocean is at its sun - warmed surface, where microscopic floating plants called phytoplankton consume
carbon dioxide for energy (just
like grass and trees).
Acting
like a massive sponge, the
oceans pull from the atmosphere heat,
carbon dioxide and other gases, such as chlorofluorocarbons, oxygen and nitrogen and store them in their depths for decades to centuries and millennia.
The main
carbon sink is
ocean calcareous phytoplankton
like coccolithophores, and diatoms.
It may address a more narrow issue
like ocean acidification or the
carbon cycle.
Acting
like a massive sponge, the
ocean pulls from the atmosphere heat,
carbon dioxide, and other gases (e.g., chlorofluorocarbons, oxygen, and nitrogen) and stores them in their depths for decades to centuries and millennia.
A central hurdle is that
carbon dioxide accumulates in the atmosphere
like unpaid credit card debt as long as emissions exceed the rate at which the gas is naturally removed from the atmosphere by the
oceans and plants.
Including a match with other observations
like the mass balance, the 13C / 12C and 14C / 12C trends, the oxygen balance, the increase of
carbon species in the
ocean surface and vegetation, etc...
That sounds
like a lot, but it only adds up to the equivalent emissions of about 200 cars annually (900 tonnes), and is a drop in the
ocean compared to the 40 billion tonnes or so of
carbon humans put into the atmosphere every year.