Sentences with phrase «aerosol precursor emissions»

The SRES scenarios were constructed to explore future developments in the global environment with special reference to greenhouse gases and aerosol precursor emissions.

Not exact matches

Indeed, the reduction in the emission of precursors to polluting particles (sulphur dioxide) would diminish the concealing effects of Chinese aerosols, and would speed up warming, unless this effect were to be compensated elsewhere, for instance by significantly reducing long - life greenhouse gas emissions and «black carbon.»
Global climate models are essential tools for understanding climate change and for developing policy regarding future emissions of greenhouse gases, primary aerosol particles, and aerosol precursor gases.
From the Physical Science Basis: «Shindell et al. (2009) estimated the impact of reactive species emissions on both gaseous and aerosol forcing species and found that ozone precursors, including methane, had an additional substantial climate effect because they increased or decreased the rate of oxidation of SO2 to sulphate aerosol.
The future concentrations of LLGHGs and the anthropogenic emissions of sulphur dioxide (SO2), a chemical precursor of sulphate aerosol, are obtained from several scenarios considered representative of low, medium and high emission trajectories.
• Estimation of future emissions and biogeochemical cycling (including sources and sinks) of greenhouse gases, aerosols and aerosol precursors and projections of future concentrations and radiative properties.
The models used the Intergovernmental Panel on Climate Change's «A1B» mid-range projected emission scenarios for ozone and aerosol precursors, independently calculated the resulting composition change, and then performed transient simulations to 2050 examining the response to projected changes in the short - lived species and to changes in both long - lived and short - lived species together.
«We use 1280 years of control simulation, with constant preindustrial forcings including constant specified CO2, and a five - member ensemble of historical simulations from 1850 — 2005 including prescribed historical greenhouse gas concentrations, SO2 and other aerosol - precursor emissions, land use changes, solar irradiance changes, tropospheric and stratospheric ozone changes, and volcanic aerosol (ALL), following the recommended CMIP5 specifications.
Emissions - Emissions of heat - trapping gases (greenhouse gases), greenhouse - gas precursors, and aerosols associated with human activities.
The emission data on the RCPs were harmonized and downscaled (to a 0.5 × 0.5 grid) for air pollutants, i.e. aerosols and tropospheric ozone precursors.
Consequently, the most advanced climate models now require, in addition to concentrations or emissions of greenhouse gases (CO2, CH4, N2O and halocarbons), emissions of reactive gases and aerosol precursor compounds (SO2, NOx, VOC, BC, OC and NH3), to model atmospheric chemistry and interactions with the climate system.6 For most variables, a sectoral differentiation would improve the quality of the calculations (e.g. from power plants and agricultural burning).
For the runs with different emission and «climate» years, e.g. Em2000Cl1850, emissions of aerosol and ozone precursors are set to 2000, methane amounts for chemistry are set to 2000, but ozone and methane at 2000 do not affect the radiation (i.e. radiation sees 1850 «climate» conditions for everything but aerosols).
They hypothesize that natural emissions of aerosol precursors will increase in a warming climate, causing a negative feedback so as to dampen the warming.
[Response: For any projection for the future of climate, you obviously need a projection of emissions (greenhouse gases, ozone and aerosol precursors, etc.), land use change and so on.
Radiative forcing is a way to quantify an energy imbalance imposed on the climate system either externally (e.g., solar energy output or volcanic emissions) or by human activities (e.g., deliberate land modification or emissions of greenhouse gases, aerosols, and their precursors).
Thus, we have traditionally studied the impact of carbon dioxide separately from the impact of sulphate aerosols and separately from the impacts of the emissions that cause ozone (the «precursors»).
All pieces required for the representation of OA in a global climate model are sketched out with special attention to Secondary Organic Aerosol (SOA): The emission estimates of primary carbonaceous particles and SOA precursor gases are summarized.
We find that the increase in emissions of inorganic aerosol precursors is much larger than the corresponding aerosol increase, reflecting a non-linear atmospheric response.
The climate feedbacks involved with these changes, which are key in understanding the climate system as a whole, include: + the importance of aerosol absorption on climate + the impact of aerosol deposition which affects biology and, hence, emissions of aerosols and aerosol precursors via organic nitrogen, organic phosphorus and iron fertilization + the importance of land use and land use changes on natural and anthropogenic aerosol sources + the SOA sources and impact on climate, with special attention on the impact human activities have on natural SOA formation In order to quantitatively answer such questions I perform simulations of the past, present and future atmospheres, and make comparisons with measurements and remote sensing data, all of which help understand, evaluate and improve the model's parameterizations and performance, and our understanding of the Earth system.
These results suggest that efforts to mitigate atmosphere - related environmental damages should target a broad set of emissions including CO2, methane and aerosol / ozone precursors.
Google «historic SO2 emissions» (an important precursor to anthropogenic aerosol) and the first document to come up is this one.
[Reply: Knowledge of industrial output and typical emissions of said industries; knowledge of emissions of SO2 and other aerosol precursors and the relation with aerosol properties.
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