Most experts agree that the HadCRUT record tends to
under estimate warming because it excludes a large part of the Arctic from its measurement, and the Arctic is warming much faster than most parts of the globe.
Not exact matches
Understanding how layers of air insulate the surface of glaciers, for example, is vital to making accurate
estimates of how fast they will melt — and sea levels will rise — as the Earth
warms under its blanket of greenhouse gases.
The
estimated size of and uncertainty in current observed
warming rates attributable to human influence thus provides a relatively model - independent
estimate of uncertainty in multi-decade projections
under most scenarios.
For example, Sturrock et al. (2011)
estimate that a) Dothistroma needle blight (Dothistroma septosporum or D. pini), whose primary host in Montana is ponderosa pine, will have reduced or increased impacts, depending on
warmer and drier or wetter conditions, respectively; and b) Armillaria root disease (Armillaria spp.), which generally affects Douglas - fir and grand fir, will have increased impacts
under warmer, drier conditions, but no change
under warmer, wetter conditions.
Indeed, if one accepts a very liberal risk level of 50 % for mean global
warming of 2 °C (the guiderail widely adopted) since the start of the industrial age, then
under midrange IPCC climate sensitivity
estimates, then we have around 30 years before the risk level is exceeded.
The importance of a structured
warm up routine should not be
under estimated when it comes to preventing sports injury.
The smallest
warming / sea level rise in TAR figure 5 will place a wide range of human and natural systems
under very considerable pressure (and based on
estimates of the melt - down point for greenland place us teetering on the edge of dangerous climate change).
The
estimated size of and uncertainty in current observed
warming rates attributable to human influence thus provides a relatively model - independent
estimate of uncertainty in multi-decade projections
under most scenarios.
John Tyndal found that water vapor and carbon dioxide were the major greenhouse gases in 1859, and Svante Arrhenius made the first
estimate of global
warming under doubled carbon dioxide in 1896.
Advocates for tackling the issue
under the Montreal treaty expressed disappointment that the Obama administration was taking such a cautious approach to a chemical that could, by some
estimates, account for as much as 30 percent of all atmospheric
warming by 2040.
ESTIMATING THE PERMAFROST - CARBON FEEDBACK ON GLOBAL
WARMING A key uncertainty is the fraction of carbon that might be decomposed
under anaerobic conditions — resulting potentially in methane emissions to the atmosphere.
So, even conservative
estimates of committed
warming indicate that we have to urgently reduce radiative forcing, in other words peak global GHG emissions as soon as possible and then reduce them as quickly as possible by reducing our use of fossil fuels drastically, if we want to have a chance at keeping
warming under 2C.
It's been criticized, and may well not be the last word on the subject, but their
estimate was droughts such as the one that was observed are about 3x more likely
under the observed
warming than in an «unwarmed» world.
Warming of 4 °C would increase central
estimates to more than 1,745 cities and 30 million people
under either assumption.
We
estimate committed
warming based on a distribution of possible transient response coefficient values from Gillett et al. and from future cumulative emissions
under representative concentration pathways (RCPs) 2.6, 4.5, 6.0, and 8.5 (RCP Database version 2.0.5).
By the way, you also conveniently failed to mention that RSS admits that their version 4.0 TLT likely
under -
estimates lower tropospheric
warming [5].
A) UAH TLT is about the same as for ERA - I [6], even though the ERA - I team admits that they
under -
estimate lower tropospheric
warming [7].
The IPCC
estimates a likely upper bound for sea level rise, for instance, at about a meter, but
under much stronger
warming scenarios.
C) There's continuing criticism of UAH's homogenization methods, methods that conveniently seem to almost always
under -
estimate tropospheric
warming and to diverge from other satellite - based
estimates [9].
D) Consistent with UAH's history of conveniently
under -
estimating tropospheric
warming, UAH reduced their tropospheric
warming trend from version 5.6 to version 6 [10].
Under a scenario where
warming is kept below 2 °C by 2050, annual adaptation costs are
estimated at US$ 35 billion per year.
Our analysis also leads to a relatively low and tightly - constrained
estimate of Transient Climate Response of 1.3 — 1.8 °C, and relatively low projections of 21st - century
warming under the Representative Concentration Pathways.
The following figure, which presents the FTA's
estimates of habitat converted to cropland as of 2100, shows that the amount of habitat lost to cropland may well be least
under the richest - but -
warmest scenario (A1FI), but higher
under the cooler (B1 and B2) scenarios.
In fact,
under reasonable alternative assumptions, one of the models used to
estimate the SCC provides a negative
estimate of the SCC — implying that there are net benefits to global
warming, which would argue for subsidizing, not taxing, CO2 emissions.
All I know is that Schmidt, Santer, et al seem to agree that the climate models over predicted the
warming because the models
under -
estimated negative forcing due to stratospheric aerosols.
We
estimate that anthropogenic influence has caused a more than 60-fold increase in the likelihood of the extreme
warm 2013 summer since the early 1950s, and project that similarly hot summers will become even more frequent in the future, with fully 50 % of summers being hotter than the 2013 summer in two decades even
under the moderate RCP4.5 emissions scenario.
The results can give us projections of future global
warming under a variety of scenarios, and also give us an
estimate of the global climate sensitivity.
Of course, that study is just one of many on how much carbon reduction is optimal, but even more conservative
estimates show there's still plenty of ground to make up if the goal is keeping global
warming under 2 degrees.
A) c02 is a ghg B) humans are putting c02 into the air C) if we increase c02 the planet will
warm, D) we have uncertain
estimates for the amount of
warming E) we take the
under bet.
Somewhat related, Snyder
estimates the global average temperature during the previous interglacial (Eemian) to be
warmer than now, whereas e.g. Hansen et al (2016,
under review) argue that they are similarly
warm.
Bottom: Provided for reference,
estimated amount of carbon that would
warm the planet approximately 2 °C (Allen et al., 2009; uncertainty
estimate in this value discussed in this reference) and
estimated total amount of carbon to be released by the year 2100
under business - as - usual scenarios (IPCC, 2007c).
The Arctic is
under - represented in surface temperature datasets and this could affect
estimates of global
warming.
Current results continue to be fairly consistent with my personal theory, that man - made CO2 may add 0.5 - 1C to global temperatures over the next century (below alarmist
estimates), but that this
warming may be swamped at times by natural climactic fluctuations that alarmists tend to
under -
estimate.
A study
under the auspices of University of Alaska Fairbanks doubles
estimates of methane released from an important oceanic source which may be «leaking» the potent global
warming gas as permafrost melts.
There are also indications that the» hiatus» is related to increased
warming in the deep oceans (Balmaseda et al. 2013) and that the
estimate of the global mean has been underestimated due
under - reporting of the recent
warming in the Arctic (Cowtan and Way 2014).
This is especially critical because studies have
estimated a reduction in Atlantic dust cover of 40 to 60 %
under a doubled carbon dioxide climate, which, on the basis of model runs with an equivalent reduction of the mean dust forcing, could result in an additional 0.3 ° to 0.4 °C
warming of the northern tropical Atlantic.»
I still believe that CO2 levels are rising largely due to human activities and that they contribute to net mean
warming, though not anywhere near the amount
estimated by the official climate Team, and far less than natural processes not
under human control.
Question: given these givens, please provide your best
estimate of the trajectory of
warming under various scenarios.
While global dimming may be causing us to
under -
estimate the amount of global
warming, other effects may be causing us to over-
estimate it.
Quirke: In one of your posts, you mentioned that your best
estimate for
warming under a business as usual scenario — which I guess is unsuccessful mitigation and somewhere between the IPCC's RCP 6.5 and 8.5 emissions scenarios — is 3 °C by 2100.