Ocean uptake of CO2, resulting from increasing atmospheric CO2 concentrations, reduces surface ocean pH and carbonate ion concentrations, an impact that was overlooked in the TAR.
E.g., given that the net radiative balance at the top of the atmosphere remains negative, which certainly indicates continued warming, Trenberth's studies suggest deep
ocean uptake of most of the recent heating.
However,
the ocean uptake of heat would also act to «bank» the heat, accumulating it through the spike period, prolonging the recovery of surface temperature beyond the demise of the methane spike itself.
Ocean uptake of CO2 slows the rate of anthropogenic climate change but comes at the cost of ocean acidification.
Here is their difficulty: If they invoke the deep
ocean uptake of heat (without proof) this looks like handwaving but also means that the time to equilibrium could be very long such that the next 100 years is governed by the transient sensitivity not the equilibrium value.
However, current understanding suggests that, unless substantial ocean circulation changes occur, plankton growth remains roughly unchanged because it is limited mostly by environmental factors, such as nutrients and light, and not by the availability of inorganic carbon it does not contribute significantly to
the ocean uptake of anthropogenic CO2.
If the tropics temperature reduced by 1C and the Antarctic remained the same of reduced somewhat less,
ocean uptake of CO2 would increase by ~ 10 PPM initially for some unit of time until it eached some equilibrium.
«In our mor recent global model simulations the ocean heat - uptake is slower than previously estimated,
the ocean uptake of carbon is weaker, feedbacks from the land system as temperature rises are stronger, cumulative emissions of greenhouse gases over the century are higher, and offsetting cooling from aerosol emissions is lower.
Air Pollution and Materials • Increased acid deposition • Increased photochemical smog • Degradation of outdoor paints and plastics Fig, p. 488 Global Warming • Accelerated warming because of decreased
ocean uptake of CO2 from atmosphere by phytoplankton and CFCs acting as greenhouse gases
• Accelerated warming because of decreased
ocean uptake of CO2 from atmosphere by phytoplankton and CFCs acting as greenhouse gases
The ocean uptake of excess atmospheric carbon dioxide, the excess above preindustrial levels driven by human emissions, causes well - understood and substantial changes in seawater chemistry that can affect marine organisms and ecosystems.
Cumulative land and
ocean uptake of carbon for the period 1850 - 2005.
Maybe if we had kept on talking about adding carbonic acid to the air (instead of using the modern vocabulary whereby we add carbon dioxide to the air), we would have been talking all along about
ocean uptake of carbonic acid and ocean acidification would have been an obvious consequence.
This too is questionable, as there are reasons to think
the ocean uptake of heat varies at different time scales and may be influenced by ENSO, the Pacific Decadal Oscillation (PDO), and the Atlantic Multi-decadal Oscillation (AMO).
As to
ocean uptake of heat, the novice might ask, «how come that didn't happen so obviously a in the past?
In these experiments the climate sensitivity was 2.7 deg C for a doubling of CO2, the net aerosol forcing from 1940 to 2000 was around -0.7 W / m2 (55 % of the total forcing, -1.27, from 1850 to 2000), and
the ocean uptake of heat was well - matched to recent observations.
[Response: I'm sure Eric won't mind me stepping in with some questions for you instead — 1) why do you keep insinuating that terrestrial and
ocean uptake of anthropogenic CO2 is somehow not accepted by mainstream scientists?
The centre runs research programmes in climate variability and change, the monitoring of sea levels,
ocean uptake of carbon dioxide, and Antarctic marine ecosystems.
Not exact matches
The researchers were able to test their hypothesis that stronger winds were driving the
ocean heat
uptake by putting the observations
of wind behavior into climate models.
«No one would ever have predicted from first principles that increasing CFCs would have the effect
of decreasing
uptake of ocean CO2,» says Andrew Watson
of the University
of East Anglia, UK.
The iron deprivation means that estimates
of global
ocean carbon
uptake are probably 2 to 4 percent too high, the group reports in the August 31 Nature.
This was due to a combination
of factors: a less active sun, higher levels
of cooling aerosols from volcanoes and Asian factories, and increased heat
uptake by the
oceans.
Dr. Houghton and colleagues conclude that the greater certainty in atmospheric carbon measurements has led to an increased certainty in the calculated rate
of carbon
uptake by land and
oceans.
Upper -
ocean processes dissipate heat, transport nutrients and impact the
uptake of carbon dioxide — making circulation a critical driver
of biological activity in the
ocean.
Ocean acidification, another change caused by the
oceans»
uptake of carbon dioxide, also hurts corals.
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.
However, this new analysis reveals that the northern North Atlantic, the Southern
Ocean and Equatorial Pacific Ocean are all important regions of ocean heat up
Ocean and Equatorial Pacific
Ocean are all important regions of ocean heat up
Ocean are all important regions
of ocean heat up
ocean heat
uptake.
The
uptake of fossil fuel carbon dioxide (CO2) by the
ocean increases seawater acidity and causes a decline in carbonate ion concentrations.
«
Uptake of iron by diatoms is significant compared to what Mother Nature is able to naturally add to the
ocean,» he said.
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.
These variations originate primarily from fluctuations in carbon
uptake by land ecosystems driven by the natural variability
of the climate system, rather than by
oceans or from changes in the levels
of human - made carbon emissions.
Researchers have long known the region is crucial in the
uptake of atmospheric CO2 and that biological processes in the Southern
Ocean influence the global ocean system via northward flowing curr
Ocean influence the global
ocean system via northward flowing curr
ocean system via northward flowing currents.
This is an important advance because nutrient
uptake is a central property
of ocean biogeochemistry, and in many regions controls carbon dioxide fixation, which ultimately can play a role in mitigating climate change.
To address the knowledge gap about the globally - relevant ecosystem process
of nutrient
uptake, researchers worked to identify how different levels
of microbial biodiversity influenced in situ phosphorus
uptake in the Western Subtropical North Atlantic
Ocean.
«A limit to the availability
of iron in this region means that the
ocean is less efficient in its
uptake of atmospheric carbon dioxide,» he said.
«Controlling air pollution will bring huge benefits to human welfare but it may reduce the amount
of nutrients to the surface
ocean and, thus, the
ocean carbon
uptake rate.
Not considering the change in net
uptake of carbon by the
ocean, you can put the following numbers on that (based on Ramanathan and Feng, 2009):
As the
uptake of carbon dioxide has increased in the last century, so has the acidity
of oceans worldwide.
An increased
uptake of carbon by the
oceans (in the hypothetical situation
of stopping all emissions immediately) is not likely to cancel the «unmasked» greenhouse warming in addition to canceling the «committed»
ocean warming.
For the change in annual mean surface air temperature in the various cases, the model experiments show the familiar pattern documented in the SAR with a maximum warming in the high latitudes
of the Northern Hemisphere and a minimum in the Southern
Ocean (due to ocean heat uptak
Ocean (due to
ocean heat uptak
ocean heat
uptake)(2)
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.
Abstract:
Ocean acidification refers to the lowering of the ocean's pH due to the uptake of anthropogenic CO2 from the atmosp
Ocean acidification refers to the lowering
of the
ocean's pH due to the uptake of anthropogenic CO2 from the atmosp
ocean's pH due to the
uptake of anthropogenic CO2 from the atmosphere.
These rising atmospheric greenhouse gas concentrations have led to an increase in global average temperatures
of ~ 0.2 °C decade — 1, much
of which has been absorbed by the
oceans, whilst the oceanic
uptake of atmospheric CO2 has led to major changes in surface
ocean pH (Levitus et al., 2000, 2005; Feely et al., 2008; Hoegh - Guldberg and Bruno, 2010; Mora et al., 2013; Roemmich et al., 2015).
Almost everybody agrees that it has to do with fluctuations in the carbon
uptake by the
oceans, with a number
of theories relying on enhancement
of the biological pump, much along the lines you suggest.
Changing living conditions caused by climate change or
ocean acidification — the decrease
of ocean pH due to the
uptake of human - induced carbon dioxide from the atmosphere — pose serious threats to marine organisms.
Injection
of a large amount
of surface freshwater in either hemisphere has a notable impact on heat
uptake by the
ocean and the internal
ocean heat distribution (Fig. 12).
«We have to consider there are two sides
of the coin: On the one hand, the
uptake of carbon dioxide moderates climate change but, on the other hand, it affects life in the
ocean — with consequences for economy and society.»
Oceanic
uptake of anthropogenic carbon dioxide (CO2) causes pronounced shifts in marine carbonate chemistry and a decrease in seawater pH. Increasing evidence indicates that these changes — summarized by the term
ocean acidification (OA)-- can significantly affect marine food webs and biogeochemical cycles.
Plattner, G. - K., F. Joos, T.F. Stocker, and O. Marchal, 2001: Feedback mechanisms and sensitivities
of ocean carbon
uptake under global warming.
The oceanic
uptake of anthropogenic CO2 leads to a gradual acidification
of the
ocean.