Modelling interactions between terrestrial and
atmospheric systems requires coupling successional models to biogeochemical models and physiological models that describe the exchange of water and energy between vegetation and the atmosphere at fine time - scales.
Not exact matches
«Stabilizing or reducing
atmospheric carbon dioxide concentrations, therefore,
requires very deep reductions in future emissions to compensate for past emissions that are still circulating in the Earth
system,» the draft report says.
Analyzing such
systems, whether they are on the surface of a catalyst, a microbial community, or
atmospheric aerosols, and understanding their impact
requires tools that can accurately identify and quantify hundreds of molecules,» said Dr. Julia Laskin, a PNNL chemist, who has been advancing the frontiers of the Nanospray Desorption Electrospray Ionization Mass Spectrometry, nicknamed nano - DESI, for the last 3 years.
The inertia of energy
system infrastructure, i.e., the time
required to replace fossil fuel energy
systems, will make it exceedingly difficult to avoid a level of
atmospheric CO2 that would eventually have highly undesirable consequences.
Requires the Climate Service Program to: (1) analyze the effects of weather and climate on communities; (2) carry out observations, data collection, and monitoring of
atmospheric and oceanic conditions; (3) provide information and technical support to governmental efforts to assess and respond to climate variability and change; (4) develop
systems for the management and dissemination of data; (5) conduct research to improve forecasting and understanding of weather and climate variability and change and its effects on communities; and (6) develop tools to facilitate the use of climate information by local and regional stakeholders.
Stabilizing
atmospheric concentrations of greenhouse gases will
require a radical transformation of the global energy
system over coming decades.
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).
Most CM experiments based on RCPs will be driven by greenhouse gas concentrations (Hibbard et al. 2007).8 Furthermore, many Earth
system models do not contain a full
atmospheric chemistry model, and thus
require exogenous inputs of three - dimensional distributions for reactive gases, oxidant fields, and aerosol loadings.
And The Economist also seems blissfully unaware that stabilizing anywhere near 450 ppm
atmospheric concentration of CO2 would
require immediate and sustained action to replace the world's fossil fuel
system with one based on carbon - free energy — precisely the kind of aggressive action this piece seems designed to undercut.
The UN protocol
requires every nation on earth to reduce their
atmospheric emissions of greenhouse gas to 94.8 % of 1990 levels to «prevent dangerous anthropogenic interference with the climate
system.»
The inertia of energy
system infrastructure, i.e., the time
required to replace fossil fuel energy
systems, will make it exceedingly difficult to avoid a level of
atmospheric CO2 that would eventually have highly undesirable consequences.
«Reducing the wide range of uncertainty inherent in current model predictions of global climate change will
require major advances in understanding and modeling of both (1) the factors that determine
atmospheric concentrations of greenhouse gases and aerosols, and (2) the so - called «feedbacks» that determine the sensitivity of the climate
system to a prescribed increase in greenhouse gases.»
The current warming trend can not be due to «natural variability» because at present both ocean temperatures and land temperatures are warming which
requires an external forcing and land temperatures are warming faster than ocean temperatures which can not occur with internal variability of the ocean -
atmospheric system.