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originally posted by: jrodDo you not think the scientists who study this have taken this into consideration in their current modeling?
Are you just trying to cast doubt on the overwhelming consensus of what the actual experts say about climate change and man's role here?
originally posted by: raymundoko
Source: Leibniz Institute for Tropospheric Research
Abiotic source of Isoprene discovered:
Lyon/ Leipzig. The oceans seem to produce significantly more isoprene, and consequently affect stronger the climate than previously thought. This emerges from a study by the Institute of Catalysis and Environment in Lyon (IRCELYON, CNRS / University Lyon 1) and the Leibniz Institute for Tropospheric Research (TROPOS), which had studied samples of the surface film in the laboratory. The results underline the global significance of the chemical processes at the border between ocean and atmosphere, write the researchers in the journal Environmental Science & Technology.
Our current climate models which predict catastrophic climate change estimate ~2 Megatons of Isoprene a year, however this study shows that this abiotic source alone produces ~3.5 Megatons a year.
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.
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.
originally posted by: raymundoko
Source: Leibniz Institute for Tropospheric Research
Abiotic source of Isoprene discovered:
Lyon/ Leipzig. The oceans seem to produce significantly more isoprene, and consequently affect stronger the climate than previously thought. This emerges from a study by the Institute of Catalysis and Environment in Lyon (IRCELYON, CNRS / University Lyon 1) and the Leibniz Institute for Tropospheric Research (TROPOS), which had studied samples of the surface film in the laboratory. The results underline the global significance of the chemical processes at the border between ocean and atmosphere, write the researchers in the journal Environmental Science & Technology.
Our current climate models which predict catastrophic climate change estimate ~2 Megatons of Isoprene a year, however this study shows that this abiotic source alone produces ~3.5 Megatons a year.
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.
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.
originally posted by: mbkennel
originally posted by: raymundoko
Source: Leibniz Institute for Tropospheric Research
Abiotic source of Isoprene discovered:
Lyon/ Leipzig. The oceans seem to produce significantly more isoprene, and consequently affect stronger the climate than previously thought. This emerges from a study by the Institute of Catalysis and Environment in Lyon (IRCELYON, CNRS / University Lyon 1) and the Leibniz Institute for Tropospheric Research (TROPOS), which had studied samples of the surface film in the laboratory. The results underline the global significance of the chemical processes at the border between ocean and atmosphere, write the researchers in the journal Environmental Science & Technology.
Our current climate models which predict catastrophic climate change estimate ~2 Megatons of Isoprene a year, however this study shows that this abiotic source alone produces ~3.5 Megatons a year.
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.
Laymans terms: This finding means the earth will heat up nowhere nearly as fast as models predicted it would.
It doesn't mean that at all. Why would it?
Note that this process was occurring before human civilization of course.
They will have to be adjusted to take this finding into account.
True, and let's see what it does. It may make the understanding of clouds better, and improve the regional predictions of climate.
The overall physical forcing from additional greenhouse gases is still in effect.
originally posted by: raymundoko
a reply to: Greven
Why do you join in climate discussions if you don't even know the answer to that question?
originally posted by: Greven
Do explain how much isoprene cools the atmosphere.
How does the potential additional 3.5 megatonnes of isoprene compare to human emissions of over 30 gigatonnes of carbon dioxide?
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.
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
originally posted by: raymundoko
My response was to your first part implying you don't know how isoprene cools the atmosphere. It's a disingenuous question because even armchair researchers know the answer. Your intent was clear.
originally posted by: Greven
Do explain how much isoprene cools the atmosphere.
How does the potential additional 3.5 megatonnes of isoprene compare to human emissions of over 30 gigatonnes of carbon dioxide?
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.