Not really, because the one real hard fact that we know
about atmospheric methane is that it's concentration isn't rising very quickly.
Not exact matches
Ice core records show
atmospheric methane levels plunged from
about 700 parts per billion to just 500 ppb at the time of their extinction.
Since
methane can cause
about 20 times as much
atmospheric warming as carbon dioxide, curbing
methane would help slow global warming.
For months of weekly press conferences, reporters had been asking
about Curiosity's analyses of
atmospheric methane on Mars.
The amount of
atmospheric methane has remained relatively stable for
about a decade, but concentrations began to rise again in 2007.
Patrick Crill, an American biogeochemist at Stockholm University, says ice core data from the past 800,000 years, covering
about eight glacial and interglacial cycles, show
atmospheric methane concentrations between 350 and 800 parts per billion in glacial and interglacial periods, respectively.
In fact, while
methane is a
atmospheric characteristic of giant gas planets like Jupiter, the only brown dwarf found to even have a trace of
methane was Gliese 229 B, which orbits a reddish, M - class dwarf located
about 20 light - years away from Earth.
... The Earth's
atmospheric methane concentration has increased by
about 150 % since 1750, and it accounts for 20 % of the total radiative forcing from all of the long - lived and globally mixed greenhouse gases (these gases don't include water vapor which is by far the largest component of the greenhouse effect).
«We know rather little
about how much
methane comes from different sources and how these have been changing in response to industrial and agricultural activities or because of climate events like droughts,» says Hinrich Schaefer, an
atmospheric scientist at the National Institute of Water and
Atmospheric Research (NIWA) in New Zealand, who collaborates with Petrenko.
Near Titan's surface,
about 5 percent of the
atmospheric molecules are
methane, the fraction decreasing with altitude.
Raymond Pierrehumbert, an Oxford University
atmospheric physics professor who believes cutting carbon dioxide emissions is more urgent than cutting
methane emissions, said Howarth's research offers little new information
about the role of natural gas production in global warming.
Re # 17, it seems that the isotopic signature of
atmospheric methane could tell you something
about it's source.
and 1998 snippets
Methane now contributes
about 20 % to the increased direct radiative forcing by greenhouse gases compared to preindustrial times [Shine et al., 1995] Oxidation of CH4 in the troposphere produces carbon monoxide (CO), can lead production of ozone (03), and involves
atmospheric oxidant, the hydroxyl radical (OH).
I think I know what you mean here but in the context of the previous Much Ado
about Methane article with discussion of the difference between
atmospheric lifetime of a CO2 molecule vs. lifetime of an increase in concentration, this could also be put more clearly.
This is
about as far as one could get from high levels (relative to most
atmospheric concentrations) of
methane over large areas high in the atmosphere in the Arctic where there is very little (direct) human activity.
Methane has a
atmospheric lifespan of
about a decade.
Since the onset of the Industrial Revolution in
about 1750, however,
atmospheric methane concentrations shot up to
about 1800 parts per billion and are continuing to rise.
It follows that an
atmospheric composition of
about 8 %
methane gives one 360 - 430 degrees of heating, with a fainter sun and a slightly lower albedo.
According to the report,
atmospheric methane had reached
about 1845 parts per billion (ppb) in 2015, 2.5 times greater than in the pre-industrial era, while nitrous oxide was at 328ppb, 1.2 times above historic levels.
The amount of
atmospheric methane had remained relatively stable for
about a decade, but concentrations began to rise again in 2007.
Using SCIAMACHY satellite data as well as ground - based measurements from 2003 to 2009, researchers found that the region where Arizona, New Mexico, Colorado, and Utah intersect had
atmospheric methane concentrations equivalent to
about 1.3 million pounds of emissions a year.
Industry, with the full support of the administration, continues the fait accompli of radically expanded natural gas fracking across the country, with serious unresolved issues
about fugitive
atmospheric methane emissions and the potential for contamination of drinking water aquifers — and with no adequate federal regulatory structure in place.
Perhaps the author should educate himself
about the dwell time of
atmospheric methane, it is approximately 12 years.
BTW, I wonder
about how the
methane release paper you linked to has been impacted by the rather sudden change in
atmospheric methane growth rate (near zero)... that seems not to have been anticipated, AFAIK.
The first place I recall reading
about the breakdown of
methane in water was from: Revelle, Roger (1983), «Methane hydrates in continental slope sediments and increasing atmospheric carbon dioxide,» Changing Climates, Report of the Carbon Dioxide Assessment Committee, pp. 252 — 261, National Academy Press, Washington
methane in water was from: Revelle, Roger (1983), «
Methane hydrates in continental slope sediments and increasing atmospheric carbon dioxide,» Changing Climates, Report of the Carbon Dioxide Assessment Committee, pp. 252 — 261, National Academy Press, Washington
Methane hydrates in continental slope sediments and increasing
atmospheric carbon dioxide,» Changing Climates, Report of the Carbon Dioxide Assessment Committee, pp. 252 — 261, National Academy Press, Washington, D. C.
The
atmospheric methane concentration rose from the preanthropogenic until
about the year 1993, at which point it rather abruptly plateaued.
«Shakhova notes that the Earth's geological record indicates that
atmospheric methane concentrations have varied between
about.3 to.4 parts per million during cold periods to.6 to.7 parts per million during warm periods.
For example, the direct radiative effect of a mass of
methane is
about 84 times stronger than the same mass of carbon dioxide over a 20 - year time frame [22] but it is present in much smaller concentrations so that its total direct radiative effect is smaller, in part due to its shorter
atmospheric lifetime.
[39] A 2014 analysis, however, states that although
methane's initial impact is
about 100 times greater than that of CO2, because of the shorter
atmospheric lifetime, after six or seven decades, the impact of the two gases is
about equal, and from then on
methane's relative role continues to decline.
Methane has an
atmospheric lifetime of
about 12 years and a global warming potential of 28 over a hundred - year period.