Sentences with phrase «for climate stabilisation»

Gerlagh, R., 2006: ITC in a global growth - climate model with CCS: The value of induced technical change for climate stabilisation.

It shows that the energy system is undergoing a broad reorientation toward low - carbon energy and efficiency but investment in key clean energy technologies needs to be further ramped up to put the world economy on track for climate stabilisation.

I think the suggestion has the very good intention of helping policymakers to take appropriate action for climate stabilisation, but to analyse and evaluate INDCs will not be a major category of work for the IPCC.

I, myself, as an economist, I always emphasise the importance of a carbon price: the need that the world must pursue, the policy of a carbon tax to have a meaningful result for climate stabilisation.

Not exact matches

There was a conference held at the begining of this year that went over this sort of thing, it was subtitled «Avoiding Dangerous Climate Change» and you can find the presentation [slides] that were presented at http://www.stabilisation2005.com/programme.html There's a lot of interesting things about possible thresholds, stabilisation levels for CO2 and emission reduction pathways and the potential costs.

Nevertheless, climate sensitivity is part of the puzzle, and it particularly matters if you are interested in stabilisation scenarios, since it indicates what a particular equilibrium CO2 level will mean for equilibrium climate.

Although the small number of impact assessments that evaluate stabilisation scenarios do not take full account of uncertainties in projected climate under stabilisation, they nevertheless provide indications of damages avoided and risks reduced for different amounts of emissions reduction.

«Beyond Kyoto: Energy Dynamics and Climate Stabilisation» suggests how negotiators might address this longer - term objective on a global basis, with due regard for the uncertainties and cost: aiming at low GHG concentrations, but making achievement of these targets conditional on actual costs.

Many don't get this — but it goes for both the temperature targets of ≤ 2 degrees (UN, G8, G21) and ≤ 1.5 degrees (wiser people) and the internationally accepted maximum GHG concentration level of 450 ppm — and for the CO2 stabilisation concentration level of 350 ppm (Hansen and many other climate scientists): if we know «2» is the right answer, we're not that clever when we fail to comprehend 1 +1 is the logical route to getting there.]

For example, stabilisation at 550 ppm (resulting in a temperature increase relative to pre-industrial levels of nearly 2 °C) only reduces the number of people adversely affected by climate change by 30 - 50 % (Arnell, 2006).

It's very clear where the solution space lies for the 2C climate stabilisations, we need to have a very close, very strong cooperation between developed and developing regions.

In January 2006, at the opening of his new Cambridge Centre for Climate Change Mitigation Research, (4CMR), Dr Terry Barker said «It may seem astonishing, but the global climate models, providing governments with estimates of the costs of climate stabilisation are nearly all reliant on one year's data.Climate Change Mitigation Research, (4CMR), Dr Terry Barker said «It may seem astonishing, but the global climate models, providing governments with estimates of the costs of climate stabilisation are nearly all reliant on one year's data.climate models, providing governments with estimates of the costs of climate stabilisation are nearly all reliant on one year's data.climate stabilisation are nearly all reliant on one year's data.»

I believe that as an economist, my advocacy, if you call it that, my advocacy of carbon price is an advocacy to my profession and also is an advocacy for the global benefit resulting from, supposed to be resulting from, climate stabilisations.

«In the real world there is no credible path to climate stabilisation that does not include a substantial role for nuclear power.»

Since any sensible program for global climate change stabilisation involves the purchase of emissions credits from poor countries, achieving both goal together would not cost much more than 5 per cent of global income.

«The consequences of CO2 stabilisation for the impacts of climate change.»

9.3.1 Global Mean Response 9.3.1.1 1 % / yr CO2 increase (CMIP2) experiments 9.3.1.2 Projections of future climate from forcing scenario experiments (IS92a) 9.3.1.3 Marker scenario experiments (SRES) 9.3.2 Patterns of Future Climate Change 9.3.2.1 Summary 9.3.3 Range of Temperature Response to SRES Emission Scenarios 9.3.3.1 Implications for temperature of stabilisation of greenhouse gases 9.3.4 Factors that Contribute to the Response 9.3.4.1 Climate sensitivity 9.3.4.2 The role of climate sensitivity and ocean heat uptake 9.3.4.3 Thermohaline circulation changes 9.3.4.4 Time - scales of response 9.3.5 Changes in Variability 9.3.5.1 Intra-seasonal variability 9.3.5.2 Interannual variability 9.3.5.3 Decadal and longer time - scale variability 9.3.5.4 Summary 9.3.6 Changes of Extreme Events 9.3.6.1 Temperature 9.3.6.2 Precipitation and convection 9.3.6.3 Extra-tropical storms 9.3.6.4 Tropical cyclones 9.3.6.5 Commentary on changes in extremes of weather and climate 9.3.6.6 Concclimate from forcing scenario experiments (IS92a) 9.3.1.3 Marker scenario experiments (SRES) 9.3.2 Patterns of Future Climate Change 9.3.2.1 Summary 9.3.3 Range of Temperature Response to SRES Emission Scenarios 9.3.3.1 Implications for temperature of stabilisation of greenhouse gases 9.3.4 Factors that Contribute to the Response 9.3.4.1 Climate sensitivity 9.3.4.2 The role of climate sensitivity and ocean heat uptake 9.3.4.3 Thermohaline circulation changes 9.3.4.4 Time - scales of response 9.3.5 Changes in Variability 9.3.5.1 Intra-seasonal variability 9.3.5.2 Interannual variability 9.3.5.3 Decadal and longer time - scale variability 9.3.5.4 Summary 9.3.6 Changes of Extreme Events 9.3.6.1 Temperature 9.3.6.2 Precipitation and convection 9.3.6.3 Extra-tropical storms 9.3.6.4 Tropical cyclones 9.3.6.5 Commentary on changes in extremes of weather and climate 9.3.6.6 ConcClimate Change 9.3.2.1 Summary 9.3.3 Range of Temperature Response to SRES Emission Scenarios 9.3.3.1 Implications for temperature of stabilisation of greenhouse gases 9.3.4 Factors that Contribute to the Response 9.3.4.1 Climate sensitivity 9.3.4.2 The role of climate sensitivity and ocean heat uptake 9.3.4.3 Thermohaline circulation changes 9.3.4.4 Time - scales of response 9.3.5 Changes in Variability 9.3.5.1 Intra-seasonal variability 9.3.5.2 Interannual variability 9.3.5.3 Decadal and longer time - scale variability 9.3.5.4 Summary 9.3.6 Changes of Extreme Events 9.3.6.1 Temperature 9.3.6.2 Precipitation and convection 9.3.6.3 Extra-tropical storms 9.3.6.4 Tropical cyclones 9.3.6.5 Commentary on changes in extremes of weather and climate 9.3.6.6 ConcClimate sensitivity 9.3.4.2 The role of climate sensitivity and ocean heat uptake 9.3.4.3 Thermohaline circulation changes 9.3.4.4 Time - scales of response 9.3.5 Changes in Variability 9.3.5.1 Intra-seasonal variability 9.3.5.2 Interannual variability 9.3.5.3 Decadal and longer time - scale variability 9.3.5.4 Summary 9.3.6 Changes of Extreme Events 9.3.6.1 Temperature 9.3.6.2 Precipitation and convection 9.3.6.3 Extra-tropical storms 9.3.6.4 Tropical cyclones 9.3.6.5 Commentary on changes in extremes of weather and climate 9.3.6.6 Concclimate sensitivity and ocean heat uptake 9.3.4.3 Thermohaline circulation changes 9.3.4.4 Time - scales of response 9.3.5 Changes in Variability 9.3.5.1 Intra-seasonal variability 9.3.5.2 Interannual variability 9.3.5.3 Decadal and longer time - scale variability 9.3.5.4 Summary 9.3.6 Changes of Extreme Events 9.3.6.1 Temperature 9.3.6.2 Precipitation and convection 9.3.6.3 Extra-tropical storms 9.3.6.4 Tropical cyclones 9.3.6.5 Commentary on changes in extremes of weather and climate 9.3.6.6 Concclimate 9.3.6.6 Conclusions

The topics addressed include critical thresholds and key vulnerabilities of the climate system, impacts on human and natural systems, socioeconomic costs and benefits of emissions pathways, and technological options for meeting different stabilisation levels of greenhouse gases in the atmosphere.

On climate change, they note that restricting the global temperature change to 2 ºC with a fair degree of confidence would require stabilisation at 400 ppm CO2 equivalent (CO2 itself is at 380 already, but «equivalent» includes other GHG's and the negative effects of sulphates; see here for more).

Projections for four CO2 - stabilisation profiles using a simple climate model (SCM) tuned to seven AOGCMs (IPCC, 2001c, Figure SPM - 6; IPCC, 2001a, Figure 9.17).

The energy demand of 5 star houses is projected to vary significantly in the range of -30 % to 100 % by 2050 and -50 % to 350 % by 2100 for A1B, A1FI and 550ppm stabilisation emission scenarios, depending on the regional climates.

Uncertainty in the equilibrium climate sensitivity creates uncertainty in the expected warming for a given CO2 - eq stabilisation scenario.

The stabilisation may create a favourable climate for implementing the blockchain technology.