Not exact matches
Random fluctuations and three physical reasons come into question to explain this: The
model calculations are based on different amounts of radiant energy from the sun that impinge on Earth's surface and are stored as a result of the greenhouse effect, e.g. due to
atmospheric carbon dioxide.
In a recent paper titled, «Demarcating circulation regimes of synchronously rotating terrestrial planets within the habitable zone,» my co-authors and I analyze a set of climate
model calculations to examine the dependence upon stellar effective temperature of the
atmospheric dynamics of planets as they move closer to the inner edge of the habitable zone.
They looked at precipitation and
atmospheric circulation among other factors before determining that the
model was accurately portraying regional climate and informing global climate
calculations.
The study used three climate
models that handle the basic
atmospheric calculations and physics in different ways.
Our estimate is based primarily on our review of a series of
calculations with three - dimensional
models of the global
atmospheric circulation, which is summarized in Chapter 4.
Marcus, why do you assume that one can't use steady state
calculations for
modeling the levels of
atmospheric CO2?
The point I should have made in # 41 is that back - of - the - envelope
calculations that imply 1st order
models of the type dCO2 = a * E --(CO2 - CO2 (0)-RRB- / tau are not well constrained by the Mauna Loa
atmospheric CO2 data.
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).
The direct radiative forcing
calculation is based on an empiric al equation derived from well - established
atmospheric radiative energy transfer
models and serves as a first - order proxy for global warming impact.»
The scenarios makes some stabs at
atmospheric concentration growth rates based on emission growth rates; and it is the
atmospheric values that are the
model input and the focus of all
calculation and discussion.
Simpson began with a gray - body
calculation, Simpson (1928a); very soon after he reported that this paper was worthless, for the spectral variation must be taken into account, Simpson (1928b); 2 - dimensional
model (mapping ten degree squares of latitude and longitude): Simpson (1929a); a pioneer in pointing to latitudinal transport of heat by
atmospheric eddies was Defant (1921); for other early energy budget climate
models taking latitude into account, not covered here, see Kutzbach (1996), pp. 354 - 59.
The Hotspot, according to all
model calculations, is simply an
atmospheric amplification of a surface trend, a consequence of the physics of the tropical atmosphere.
Recent
calculations of
atmospheric sensitivity to increased concentrations of CO2 in the atmosphere are based on observations and provide values for sensitivity that are much lower than previous versions that were based on
models.
Model calculations suggest that almost half of the global cloud condensation nuclei in the
atmospheric boundary layer may originate from the nucleation of aerosols from trace condensable vapours4, although the sensitivity of the number of cloud condensation nuclei to changes of nucleation rate may be small5, 6.
1950s: Research on military applications of radar and infrared radiation promotes advances in radiative transfer theory and measurements = > Radiation math — Studies conducted largely for military applications give accurate values of infrared absorption by gases = > CO2 greenhouse — Nuclear physicists and chemists develop Carbon - 14 analysis, useful for dating ancient climate changes = > Carbon dates, for detecting carbon from fossil fuels in the atmosphere, and for measuring the rate of ocean turnover = > CO2 greenhouse — Development of digital computers affects many fields including the
calculation of radiation transfer in the atmosphere = > Radiation math, and makes it possible to
model weather processes = >
Models (GCMs)-- Geological studies of polar wandering help provoke Ewing - Donn model of ice ages = > Simple models — Improvements in infrared instrumentation (mainly for industrial processes) allow very precise measurements of atmospheric CO2 = > CO2 green
Models (GCMs)-- Geological studies of polar wandering help provoke Ewing - Donn
model of ice ages = > Simple
models — Improvements in infrared instrumentation (mainly for industrial processes) allow very precise measurements of atmospheric CO2 = > CO2 green
models — Improvements in infrared instrumentation (mainly for industrial processes) allow very precise measurements of
atmospheric CO2 = > CO2 greenhouse.