Not exact matches
Even the 350 - ppm limit for
carbon dioxide is «questionable,» says physicist Myles Allen of the Climate Dynamics Group at the University of Oxford, and focusing instead on keeping
cumulative emissions below one trillion metric tons might make
more sense, which would mean humanity has already used up
more than half of its overall
emissions budget.
His work has shown that limiting
cumulative emissions of
carbon dioxide may be a
more robust approach to climate change mitigation policy than attempting to define a «safe» stabilization level for atmospheric greenhouse gases.
In other words — by 2014 we'd used
more of the
carbon budget than any of the RCPs had anticipated and if we are not confident that the real world is cooler than the models at this level of
cumulative emissions, this means that available
emissions for 1.5 degrees should decrease proportionately.
Holding concentrations or temperature (
more remotely) to a particular target therefore means limiting
cumulative emissions of, say,
carbon over time... a limited amount of time if we are talking about an iterative approach, and over a long period of time if we are talking about reducing the likelihood of some very nasty consequences well after we (but not our grandchildren — if we are lucky enough to have some) are gone.
This is a serious problem in itself, but a
more fundamental problem with the
emission budget concept seems to be
more - or-less unexplored: Do
cumulative carbon emission budgets have a sound scientific foundation?
Armed with our model ensemble projection, a temperature limit (2 °C), exceedance likelihood (33 %) and our «one model, one vote» ensemble interpretation, we find the
cumulative carbon emission where approximately 33 % of our modeled realizations have warmed
more than 2 °C.
They could cut
cumulative carbon dioxide
emissions by 34 billion metric tons,
more than the total
emissions from fossil fuels in this country over six years.
It states that to stand a good chance (a probability of 66 percent or
more) of limiting warming to less than 2 °C since the mid-19th century will require
cumulative CO2
emissions from all anthropogenic sources to stay under 800 gigatons of
carbon.
http://www.nature.com/nature/journal/v458/n7242/abs/nature08019.html Setting a long - term
cumulative carbon limit is
more robust and has a
more predictable effect than trying to control
emission rates.
Each molecule of
carbon dioxide, which is the most important long - lived manmade greenhouse gas, can remain in the atmosphere for as many as 1,000 years, making it
more urgent to cut
emissions in the near future, or face continued
cumulative warming for centuries to come.