Measuring O2 and calculating land and
ocean carbon sinks
«(C) the carbon cycle, including impacts related to the thawing of permafrost, the frequency and intensity of wildfire, and terrestrial and
ocean carbon sinks;
This appears to be due to an underestimate of land or
ocean carbon sinks in some ESMs.
About half of the current carbon dioxide emissions are taken up by land and
ocean carbon sinks.
The discussion talks explicitly about how diminishing terrestrial and
ocean carbon sinks over time require reduced CO2 emissions from fossil fuels / land use to achieve stabilization goals at various levels (e.g. 550 ppmv of CO2 in the atmosphere).
«(C) the carbon cycle, including impacts related to the thawing of permafrost, the frequency and intensity of wildfire, and terrestrial and
ocean carbon sinks;
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.
MacGilchrista, G. A., A. Naveira Garabatoa, T. Tsubouchib, S. Baconb, S. Torres - Valdes and K. Azetsu - Scott, 2014: The Arctic
Ocean carbon sink.
Use this form to email «Southern
Ocean carbon sink filling up fast» to someone you know: http://www.abc.net.au/science/articles/2007/05/18/1926751.htm?
That means Co2 is not supposed to be going back into
the ocean carbon sink, not releasing from it.
We don't know whether or not natural sinks have grown in recent decades... — McKinley et al., 2017 «The sum of the available evidence indicates that variability in
the ocean carbon sink is significant and is driven primarily by physical processes of upwelling, convection, and advection.
Not exact matches
Massachusetts
ocean waters are biologically diverse, support the Bay State's traditional fishing industry, and act as natural
carbon sinks.
The study contradicts earlier inferences that the Southern
Ocean's
carbon sink has been weak in the 21st century.
Although the
oceans are currently the greatest
carbon sink, terrestrial
carbon sinks also play a significant role in keeping the
carbon out of the atmosphere.
For example, soil is second only to
oceans as the planet's largest
carbon sink, while agriculture and land use changes represent the second largest source of greenhouse gas emissions.
When the creatures die, they
sink to the
ocean floor, effectively sequestering that
carbon for hundreds or even thousands of years.
«To put this in some kind of context, if those small scale eddies did not increase with wind stress then the saturation of
carbon dioxide in the Southern
Ocean sink would occur twice as rapidly and more heat would enter our atmosphere and sooner.»
In the report, an international team of climate scientists warns policy - makers that levels of
carbon dioxide in the atmosphere are at the extreme end of predictions made only in 2007, and that natural CO2
sinks such as
oceans are becoming saturated.
At various points in Earth's history, dust fell into the
ocean and fed algae, which gobbled up
carbon dioxide and
sank to the bottom of the sea, taking greenhouse gas with them and cooling the world.
«The amount of
carbon that you can
sink into the Southern
Ocean is much less than I expected.»
«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.»
When phytoplankton die, their
carbon - based bodies
sink to the
ocean floor, where they can remain for millions of years.
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.
You report on a successful trial of
ocean iron - seeding to promote plankton growth and potential
carbon sequestration via the
sinking...
We have shown that hydrothermal vent fluids contain almost none of the organic
carbon which accumulates in the
oceans, which means that vents are a
sink for this unreactive «stored»
carbon.»
Some of this
carbon then
sinks to the bottom of the
ocean when the phytoplankton die, locking it away in the deep sea for thousands of years.
The approach ranked as the study's least viable strategy, in part because less than a quarter of the algae could be expected to eventually
sink to the bottom of the
ocean, which would be the only way that
carbon would be sequestered for a long period of time.
Dr Jeff Hawkes, the lead author of this study, from the NOC said: «There has been a long outstanding question about whether hydrothermal vents are a source or
sink of organic
carbon to the
oceans.
Humans do emit only a fraction of the 750 gigatons of CO2 that move through the atmosphere each year, but small changes in the total amount can overwhelm so - called
carbon «
sinks» such as the
ocean, resulting in important, and cumulative, changes in the atmosphere.
The relationship between our future
carbon dioxide emissions and future climate change depends strongly on the capacity of the
ocean -
carbon sink.
This has been particularly true of the
ocean -
carbon sink.
For assessing the global
ocean -
carbon sink, McKinley and her co-authors from the National Oceanic and Atmospheric Administration (NOAA) Pacific Marine Environmental Laboratory, NCAR and the University of Colorado Boulder used the model to establish a long - running climate scenario from historical data.
Here, the
ocean -
carbon sink has increased, absorbing more
carbon dioxide.
We're better able to see when human activity begins to affect the
ocean -
carbon sink,» she explains.
«What we find is that observations today are not sufficient to be able to see change in the
ocean -
carbon sink,» McKinley explains.
«New climate model better predicts changes to
ocean -
carbon sink.»
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.
«It essentially means that, through multiple means, in a world with mixotrophs, more organic
carbon is
sinking into the deep
ocean than in a world without mixotrophs,» Follows says.
Then, when these microscopic creatures die, they would
sink to the bottom of the
ocean and take the
carbon with them.
«The faster a particle
sinks, the more likely its
carbon will be stored in the
ocean for centuries,» she says.
These more substantial organisms, compared to smaller and lighter plankton, were more capable of
sinking to the
ocean floor, as
carbon - containing detritus.
Once these leave the euphotic zone,
sinking into the
ocean depths, the
carbon can be sequestered for a season or for centuries.
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.
«It is a good average but it doesn't describe the dynamics of the system where the
ocean might be a good
carbon sink,» he notes.
Carbon - containing microorganisms began to
sink to the bottom of the
oceans, where they created
carbon - rich rocks.
Here was a gigantic laboratory flask with a whole tropical forest and an
ocean inside it — models of what many scientists suspected were the two biggest
carbon sinks in the world.
The north Atlantic
Ocean is globally important, as it is a
sink for atmospheric
carbon dioxide, said Eric Achterberg, chief scientist for the research cruise and lead author of the study.
That shift of the coastal
ocean from
carbon source to
sink, quantified for the first time in the Dec. 5, 2013, issue of the journal Nature, suggests coastal areas are a key component of the global
carbon budget, the scientists say.
The «land -
ocean aquatic continuum», has not previously been considered an important
carbon sink.