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originally posted by: raymundoko
a reply to: Greven
Did you read the source or the referenced publication in that source?
originally posted by: raymundoko
a reply to: swanne
JRod is lying anyway. I've never done what he claims, he just gets lost in technical jargon.
originally posted by: raymundoko
Bro, you don't even understand this thread...
a reply to: jrod
The recent publication of the teams from CNRS and TROPOS in Environmental Science & Technology provides indications how the climate models in the important details of the influence of isoprene could be improved.
The oceans seem to produce significantly more isoprene, and consequently affect stronger the climate than previously thought.
The atmospheric chemists from France and Germany, however, could now show that isoprene could also be formed without biological sources in surface film of the oceans by sunlight and so explain the large discrepancy between field measurements and models
More isoprene is apparently produced on the border between ocean and atmosphere than previously thought. The gas contributes to the formation of clouds and has therefore influence on the global climate.
Do you not think the scientists who study this have taken this into consideration in their current modeling?
Seriously, do you really think the experts, the scientists who have studied this for decades somehow missed this, and thus the models and predictions are now all flawed?
It is a reasonable and logical deduction that our addiction to burning fossil fuels caused a warming effect.
originally posted by: mbkennel
originally posted by: raymundoko
a reply to: mbkennel
Did you misread the post as well? The post does not contest warming, only that catastrophic climate models have to be adjusted and will no longer be catastrophic.
The original research doesn't present evidence that the climate sensitivity predictions will be down by a large amount, or any significant amount at all.
I'm not an expert on this obviously but I've found a recent review paper on isoprene and climate. Text on page 6123 describes the positive forcing from isoprene, meaning that it contributes net to warming, and not cooling, and therefore if true isoprene levels in the future are higher than current models, the change is towards a result of more warming.
www.researchgate.net...
probably the more important isoprene oxidation pathway (
Tar-
aborelli et al., 2009
). Removal of OH reduces the rate of conversion
of NO
2
to nitric acid (HNO
3
) and thus contributes to the efficacy of
O
3
production.
Understanding of the OH-oxidation pathway is clearly incomplete:
field measurements at Amazonian sites show that above-canopy
concentrations of isoprene are lower than implied by leaf-level
emission measurements (
Greenberg et al., 2004
) but at the same time
OH concentrations are higher than would be expected at estimated
levels of isoprene emission if isoprene removal were taking place
through the OH-oxidation pathway (
Carslawetal.,2001;Tanetal.,
2001; Thornton et al., 2002; Karl et al., 2007; Kuhn et al., 2007; Butler
et al., 2008; Ganzeveld et al., 2008; Lelieveld et al., 2008; Hofzuma-
haus et al., 2009
).
Lelieveld et al. (2008)
have suggested that OH is
recycled during isoprene oxidation, thus maintaining high levels of OH
while removing isoprene. However, the proposed mechanism appar-
ently leads to an unrealistically low isoprene mixing ratios (
Butler
et al., 2008
).
Hofzumahaus et al. (2009)
have suggested that OH-
recycling may take place without involving reactions with NO
2
,which
would result in removal of isoprene without increasing O
3
production
and would this be consistent with observed isoprene mixing ratios.
The efficacy of OH-recycling is also important for atmospheric CH
4
concentration. OH is the major atmospheric sink for CH
4
and thus an
increase in isoprene concentration, by reducing OH concentration, will
increase the lifetime of CH
4
. However, if OH-recycling is significant
then the importance of isoprene as a sink for CH
4
will be lowered.
Model experiments to quantify the impact of isoprene on
atmospheric chemistry under modern (i.e. late 20th century)
climate conditions have shown that isoprene increases tropo-
spheric O
3
by about 4 ppb over the oceans, 8 ppb over tropical land
areas and 8–12 ppb over land in the mid-latitudes (
Wang and
Shallcross, 2000
). Similar impacts on atmospheric chemistry, and
its implications for climate, have been shown by
Folberth et al.
(2006)
, who estimated that this addition to the tropospheric O
3
burden produces a global mean radiative forcing of 0.09 W m
2
.
The magnitude of the radiative forcing is greatest in the tropics,
where the isoprene emissions are highest, with values of up to
0.15 W m
2
.
Folberth et al. (2006)
also show that isoprene produces
an 8% (or 0.7
10
5
molecules cm
3
) reduction in the global mean
OH concentration, which effectively prolongs the global mean
lifetime of CH
4
by seven months, and thus enhances the climatic
importance of CH4
In any case, consider this: suppose climate sensitivity (defined in terms of global temperature) were zero (it isn't). Does that mean that everything's OK? Surely not---given the known increases in energy forcing it means that the weather & climate patterns would still have to adjust by a substantial amount which could still pose significant problems.
This study clearly points toward a global impact of the interfacial chemistry at the air−sea interface. The existence of organic films on the ocean surface due to biological activities influences therefore air−sea exchanges in an unexpected significant manner, as interfacial photosensitized chemistry may represent a significant source of isoprene in the absence of any biological sources in the marine boundary layer.
This would represent a new chemical photosensitized source of precursors for radicals and aerosols, while our current understanding points only to biological sources for such unsaturated compounds.
originally posted by: mbkennel
a reply to: raymundoko
OK, perhaps I don't. I saw that isoprene is a forcing, and the first post was a study showing that over the ocean the isoprene emissions may be higher than previously believed.
What is your interpretation, and do you have references from the literature supporting this that I could read?
originally posted by: raymundoko
a reply to: jrod
No, MKBennel confused a portion of an unrelated paper that discussed where radiative forcing was the highest (between the tropics) that also discussed Isoprene levels. The paper was NOT saying isoprene causes warming. It did say that Isoprene can destroy Ozone when nox isn't present.
OH is the major atmospheric sink for CH4 and thus an increase in isoprene concentration, by reducing OH concentration, will increase the lifetime of CH4.
Model experiments to quantify the impact of isoprene on atmospheric chemistry under modern (i.e. late 20th century) climate conditions have shown that isoprene increases tropo-spheric O3by about 4 ppb over the oceans, 8 ppb over tropical land areas and 8–12 ppb over land in the mid-latitudes (Wang and Shallcross, 2000). Similar impacts on atmospheric chemistry, and its implications for climate, have been shown by Folberth et al. (2006), who estimated that this addition to the tropospheric O3 burden produces a global mean radiative forcing of 0.09 W m2. The magnitude of the radiative forcing is greatest in the tropics, where the isoprene emissions are highest, with values of up to 0.15 W m2.Folberth et al. (2006)also show that isoprene produces an 8% (or 0.7105molecules cm3) reduction in the global mean OH concentration, which effectively prolongs the global mean lifetime of CH4 by seven months, and thus enhances the climatic importance of CH4.
originally posted by: raymundoko
a reply to: Greven
pubs.acs.org...
This study clearly points toward a global impact of the interfacial chemistry at the air−sea interface. The existence of organic films on the ocean surface due to biological activities influences therefore air−sea exchanges in an unexpected significant manner, as interfacial photosensitized chemistry may represent a significant source of isoprene in the absence of any biological sources in the marine boundary layer.
Photosensitized production of functionalized and unsaturated organic compounds at the air-sea interface
This would represent a new chemical photosensitized source of precursors for radicals and aerosols, while our current understanding points only to biological sources for such unsaturated compounds.
originally posted by: raymundoko
Laymans terms: This finding means the earth will heat up nowhere nearly as fast as models predicted it would. They will have to be adjusted to take this finding into account.
Overall, the three media reports misinterpret to an alarming extent the findings of the study, co-author Dr Christian George from the University of Lyon tells Carbon Brief:
We didnt make any statement about cooling effects. We showed just a new small detail that might have an impact on the forming processes of clouds.
It is unlikely that higher-than-thought levels of isoprene are a factor in the recent slowdown in global surface temperature rise, as Delingpoles article claims.
In fact, as isoprene only hangs around in the atmosphere for less than a month, its impact is mostly limited to regional or continental-scale climates, George says.
Similarly, these new findings are unlikely to affect projections for global temperature rise in the future, says George, though they will contribute to fine-tuning estimates on smaller geographical scales:
Our study is a new brick that should help understanding our complex world, by providing new knowledge on air-sea exchanges, but it definitively does not question climate change, it just helps us understand its impact.
The scientific evidence on manmade climate change is clear, concludes George, and their results do not cast any doubt on this:
There is no question that the global climate will become warmer. The question is just how much, how fast and how the effects will change our lives.
So, if the oceans are producing more isoprene than scientists thought, could this pose a serious threat to manmade global warming theory, as Delingpole claims? The answer is “no”, Prof Piers Forster tells Carbon Brief, in no uncertain terms:
To say that it is potentially important for climate change is so far from the mark as to be quite crazy.
The story followed in the footsteps of similar articles on the Register and Breitbart, two websites which have a history of publishing climate sceptic articles. The Register said the new research meant there isn’t as much urgency about the matter [climate change] as had been thought. While a Breibart article by James Delingpole claimed it presents “further proof” that the reason that all that predicted global warming has failed to materialise is that it has been countered by the planets natural cooling effects.
The Express and Breitbart quoted Benny Peiser, director of the Global Warming Policy Foundation, a climate sceptic lobby group, as saying: Here is more evidence…that climate models…should never have been trusted in the first place.”
While model simulations suggest the oceans produce around 1.9m tonnes of isoprene per year, the results of the new study suggest the ocean surface could produce between 0.2-3.5m tonnes of additional isoprene.
But the paper isnt saying that isoprene levels are getting higher, just that theyve always been high, Forster says:
The natural aerosol cooling could be 100 times bigger than our current estimate, but it would make no difference to climate change as it would stay more-or-less constant with time.
Second, the paper refers to the amount of isoprene, not the extent of its cooling effect, Forster points out.