Still, our understanding has a wide range of projections, particularly
for high emissions scenarios as Jevrejeva et al. (2014) illustrates.
Still, our understanding has a wide range of projections, particularly
for high emissions scenarios as Jevrejeva et al. (2014) illustrates.
However, this rise in wind potential is only projected
for a high emissions scenario (RCP8.5).
The projections for the end of the century (2081 - 2100) are approximately 5.6 °F for the lower emissions scenario and 8.5 °F
for the higher emissions scenario (see Ch.
The 12Billion figure is used
for the highest emissions scenario RCP 8.5 RCP 6 is around 10 Billion and RCP 4.5 is 8.5 B..
«
For the high emissions scenario, it is likely that the frequency of hot days will increase by a factor of 10 in most regions of the world», said Thomas Stocker the other Co-chair of Working Group I. «Likewise, heavy precipitation will occur more often, and the wind speed of tropical cyclones will increase while their number will likely remain constant or decrease».
Not exact matches
The best estimates of the increase in global temperatures range from 1.8 to 4.0 degrees C
for the various
emission scenarios, with
higher emissions leading to
higher temperatures.
The researchers analyzed climate suitability projections over time
for 513 species across 274 national parks, under a
high and low greenhouse gas
emission scenario.
However, under the
high shift
scenario — based on mode shifting and policies that encourage denser development and the substitution of telecommunications
for travel — the United States could drop its
emissions much faster to 280 megatons of CO2 by 2050.
On the
high end, recent work suggests that 4 feet is plausible.23, 3,6,7,8 In the context of risk - based analysis, some decision makers may wish to use a wider range of
scenarios, from 8 inches to 6.6 feet by 2100.10,2 In particular, the
high end of these
scenarios may be useful
for decision makers with a low tolerance
for risk (see Figure 2.26 on global sea level rise).10, 2 Although scientists can not yet assign likelihood to any particular
scenario, in general,
higher emissions scenarios that lead to more warming would be expected to lead to
higher amounts of sea level rise.
For the IPCC's
highest emissions scenario, the top end of the range goes up to 0.98 m.
Normalized well - to - wake GHG
emissions for low -, baseline - and
high -
emission cases
for jet fuel pathways under different land use change
scenarios.
Red, black, and blue lines represent the percentages of highly climate change vulnerable species under
high (A2), mid-range (A1B) and low (B1)
emissions scenarios for birds (A), amphibians (B) and corals (C)
for 1975 — 2050 and 1975 — 2090.
The Met Office Hadley Centre (Hadley Centre
for Climate Prediction and Research) climate change model, Hadley Centre Coupled Model, version 3 (HadCM3)[53], a coupled atmosphere - ocean general circulation model, was used
for the time intervals 2020, 2050 and 2080 (note these date represent a time windows of ten years either side of the time interval date, i.e. 2020 is an average of the years 2010 — 2029, 2050
for 2040 — 2059 and 2080
for 2070 — 2089), under three
emission scenarios of the IPCC Special Report on Emissions Scenarios (SRES)[54]: scenario A1B (maximum energy requirements; emissions differentiated dependent on fuel sources; balance across sources), A2A (high energy requirements; emissions less than A1 / Fl) and B2A (lower energy requirements; emissions greater
scenarios of the IPCC Special Report on
Emissions Scenarios (SRES)[54]: scenario A1B (maximum energy requirements; emissions differentiated dependent on fuel sources; balance across sources), A2A (high energy requirements; emissions less than A1 / Fl) and B2A (lower energy requirements; emissions greater
Emissions Scenarios (SRES)[54]: scenario A1B (maximum energy requirements; emissions differentiated dependent on fuel sources; balance across sources), A2A (high energy requirements; emissions less than A1 / Fl) and B2A (lower energy requirements; emissions greater
Scenarios (SRES)[54]:
scenario A1B (maximum energy requirements;
emissions differentiated dependent on fuel sources; balance across sources), A2A (high energy requirements; emissions less than A1 / Fl) and B2A (lower energy requirements; emissions greater
emissions differentiated dependent on fuel sources; balance across sources), A2A (
high energy requirements;
emissions less than A1 / Fl) and B2A (lower energy requirements; emissions greater
emissions less than A1 / Fl) and B2A (lower energy requirements;
emissions greater
emissions greater than B1).
I think it is important to stress that with the current growth of fossil fuel
emissions we are above the
highest IPCC
emissions scenario (RCP 8.5), at least
for fossil fuel combustion.
To investigate how different climate trajectories might influence climate change vulnerability, we assessed species using
high (A2), moderate (A1B) and low (B2) IPCC SRES
emissions scenarios for 2050 and 2090 [20](Figure 4; Supporting Methods in Supporting Information S1).
best estimate
for it's lowest
emissions scenario and 4.0 C... best estimate
for it's
highest emissions scenario
I think it is important to stress that with the current growth of fossil fuel
emissions we are above the
highest IPCC
emissions scenario (RCP 8.5), at least
for fossil fuel combustion.
page 30: «Current carbon dioxide
emissions are, in fact, above the
highest emissions scenario developed by the Intergovernmental Panel on Climate Change (IPCC), implying that if we stay the current course, we're heading
for even larger warming than the
highest projections from the IPCC.»
For RCP8.5 [the high emissions scenario and warming track in the illustration above] by 2100, the combination of high temperature and humidity in some areas for parts of the year will compromise normal activities, including growing food or working outdoors (high confidenc
For RCP8.5 [the
high emissions scenario and warming track in the illustration above] by 2100, the combination of
high temperature and humidity in some areas
for parts of the year will compromise normal activities, including growing food or working outdoors (high confidenc
for parts of the year will compromise normal activities, including growing food or working outdoors (
high confidence).
If Dr. Hansen never imagined
Scenario A as being a real possibility
for the next 20 years, I guess indicated by his description «
Scenario A, since it is exponential, must eventually be on the
high side of reality in view of finite resource constraints and environmental concerns, even though the growth of
emissions in
Scenario A (~ 1.5 % yr - 1) is less than the rate typical of the past century (~ 4 % yr - 1)» then his subsequent comment (PNAS, 2001) «Second, the IPCC includes CO2 growth rates that we contend are unrealistically large» seems to indicate that Dr. Hansen doesn't support some of the more extreme SRES
scenarios.
This has implications
for future
scenario's, as a lower sensitivity
for CO2 (and a
higher for solar) means that there will be less warming
for the same CO2
emissions (assuming no large excursions of solar).
He did flag that he was using RCP8.5 projections, which are the
highest emissions trajectory of the 4
scenarios developed
for AR5 (comparable to A2
scenario in IPCC AR4, which has the
highest CO2
emissions in the near - term if I understand it correctly).
When talking to the media, some have been tempted to push beyond what the science supports — focusing on the
high end of projections of global temperatures in 2100 or highlighting the scarier
scenarios for emissions of greenhouse gases.
Since 1990, observed sea level has followed the uppermost uncertainty limit of the Intergovernmental Panel on Climate Change (IPCC) Third Assessment Report (TAR), which was constructed by assuming the
highest emission scenario combined with the
highest climate sensitivity and adding an ad hoc amount of sea - level rise
for «ice sheet uncertainty» (1).
In your posting abve, you said that the
highest temperature of the range I'd quoted
for quoted
for 2030 «is attached to the A1T
scenario that has more aggressive sulphate
emission reduction than the other SRES
scenarios.»
The Summary
for Policymakers of that report said that â $ œThe
higher projected temperatures [than in the previous Assessment Report] are due primarily to the lower projected sulphur dioxide
emissions in the SRES
scenarios relative to the IS92
scenarios.»
Leaving the Paris accord and failing to meet our commitment — as Trump intends — puts the world on track
for a «
higher emissions»
scenario that leads to unimaginable impacts.
«My view is that a Chinese target of a 40 percent reduction in carbon
emissions intensity between 2005 and 2020 would be a continuation of historical trends,» said Jim Watson, from the Tyndall Centre
for climate change research in Britain [and whose report on China's carbon
scenarios we've discussed on this blog; see previous post «Tyndall Centre Climate Report:
High Hopes
for Low Carbon»].
For the study, the researchers used a set of 10 global climate models to simulate future changes in wind power under a
high future
emissions scenario (known as RCP8.5) and a moderate
emissions scenario (known as RCP4.5).
The mean
high temperature projections
for 2050 and 2100 were derived from a suite of 28 climate models (CMIP5 / Oak Ridge National Laboratory) under IPCC
emissions scenario RCP8.5, averaged over November 22 - 28
for 2030 - 2049 and 2080 - 2099, respectively.»
For example, stormwater across the city of Milwaukee recently showed
high human fecal pathogen levels at all 45 outflow locations, indicating widespread sewage contamination.87 One study estimated that increased storm events will lead to an increase of up to 120 % in combined sewer overflows into Lake Michigan by 2100 under a very
high emissions scenario (A1FI), 57 leading to additional human health issues and beach closures.
This model is integrated
for the period 1961 — 1990 (baseline) and the future time period 2071 — 2100 (
High emission scenario, A2).
Model projections
for precipitation changes are less certain than those
for temperature.12, 2 Under a
higher emissions scenario (A2), global climate models (GCMs) project average winter and spring precipitation by late this century (2071 - 2099) to increase 10 % to 20 % relative to 1971 - 2000, while changes in summer and fall are not expected to be larger than natural variations.
Soil moisture 12 inches below ground projected through 2100
for a
high greenhouse gas
emissions scenario.
The energy system reference cases used
for future greenhouse gas (GHG)
emission pathways in climate change research are a case in point: baseline
emission scenarios commonly project levels of coal combustion many times
higher than current reserve estimates by the year 2100.
These range from decreases of 10 - 15 % over much of the industrialized Northern Hemisphere
for the mid-range
scenario to CO increases worldwide under the
high -
emission projection, with the largest changes over central Africa (20 - 30 %), southern Brazil (25 - 40 %) and South and East Asia (20 - 50 %).
The name «Nevada» is Spanish
for «snow - capped,» but winter temperatures in the county are projected to average just shy of 50oF by late century under a
high emissions scenario, which could leave mountainous areas like Donner Summit covered in brown, not white.
Using the Coupled Model Intercomparison Project (CMIP5) ensemble, Jascha Lehmann from Germany's Potsdam Institute
for Climate Impact Research and colleagues rolled climate forward to 2100 and looked at the change in storm tracks under a
high carbon - dioxide -
emissions scenario.
«Our modeling shows that a
high emissions scenario could reduce global fishing revenue by an average of 10 percent, while a low
emissions scenario could reduce revenues by 7 percent,» said study co-author Rashid Sumaila, a professor at UBC's Institute
for the Oceans and Fisheries and Liu Institute
for Global Studies.
It's worth noting that despite the significant role
for CCS in its
scenarios, the IEA says under a 2C or
higher path: «Coal - fired power plants with CCS become too carbon intensive at a certain point, since 10 - 15 % of their
emissions are not captured.»
With unabated
emissions (and not only
for the
highest scenario), the IPCC estimates that by the year 2300 global sea levels will rise by 1 — 3 meters.
In general, the lowest
emissions are found
for the
scenario with the most stringent climate policy (RCP2.6) and the
highest for the
scenario without climate policy (RCP8.5), although this does not apply to all regions, at all times.
The shading indicates a measure of uncertainty about future sea level
for two different
scenarios — a low
emissions scenario where carbon
emissions are rapidly cut (blue RCP 2.6) and a
high emissions scenario with no carbon cuts (red RCP 8.5).
Projections from process - based models of global mean sea level (GMSL) rise relative to 1986 — 2005 as a function of time
for two
scenarios — RCP2.6, a low
emissions scenario, and RCP 8.5, a
high emissions scenario.
2: Our Changing Climate, Key Messages 5 and 6).4, 10 A range of model projections
for the end of this century under a
higher emissions scenario (A2), averaged over the region, suggests about 5 % to 20 % (25th to 75th percentile of model projections) increases in winter precipitation.
The main result of the paper, as highlighted in the abstract, is that
for the
highest -
emissions RCP8.5
scenario predicted warming circa 2090 [7] is about 15 %
higher than the raw multimodel mean, and has a spread only about two - thirds as large as that
for the model - ensemble.
But if we listen to her argument
for inaction, that
high emissions scenario is exactly what we'll get.
Both wetland drying and the increased frequency of warm dry summers and associated thunderstorms have led to more large fires in the last ten years than in any decade since record - keeping began in the 1940s.9 In Alaskan tundra, which was too cold and wet to support extensive fires
for approximately the last 5,000 years, 105 a single large fire in 2007 released as much carbon to the atmosphere as had been absorbed by the entire circumpolar Arctic tundra during the previous quarter - century.106 Even if climate warming were curtailed by reducing heat - trapping gas (also known as greenhouse gas)
emissions (as in the B1
scenario), the annual area burned in Alaska is projected to double by mid-century and to triple by the end of the century, 107 thus fostering increased
emissions of heat - trapping gases,
higher temperatures, and increased fires.
Figure 22.5: Projections
for average annual ground temperature at a depth of 3.3 feet over time if
emissions of heat - trapping gases continue to grow (
higher emissions scenario, A2), and if they are substantially reduced (lower
emissions scenario, B1).