Here, using fully coupled global climate model integrations, in addition to radiative
transfer model calculations, the authors confirm the existence of such a negative RFTOA: INST over parts of Antarctica in response to an in - stantaneous quadrupling of CO2.
Not exact matches
Which then has its own problems for the self - sustainability
model that Arsenal adopts, because if you believe some of the AST
calculations, it means there's about # 30million for
transfers available in the summer.
Because of the expense of doing the Venus radiative
transfer calculation, there hasn't been much
modelling of the Venus general circulation.
A particular emphasis of Hayward's research is on combining hydrodynamic simulations of galaxy formation with radiative
transfer calculations to create «forward
models» of observable quantities, such as images and spectra, that can be directly compared with data from telescopes such as the Hubble Space Telescope.
Why It Matters: Climate
models involve millions of
calculations on such things as air flow, heat
transfer, and movement of moisture through the atmosphere.
The Coefficient 5.35 in the formula RF = 5.35 ln (CO2 / CO2 - orig) comes from basic physical principles based on radiation
transfer calculations using complex
models, as the note in table 6.2 so clearly shows.
«A Global Average
Model of Atmospheric Aerosols for Radiative
Transfer Calculations.»
A
model simulation is just a series of
calculations, each of which can only
transfer information.
So the 3.7 W m - 2
calculation for global radiative forcing could be refined perhaps by an improved experimental design (not necessarily by improved radiative
transfer models) running RT
models at each grid cell over the globe, over the diurnal cycle and the annual cycle for say 30 years, for the two different CO2 concentrations, such a detailed
calculation would refine the 3.7 value.
Iacono, M. J., J. S. Delamere, E. J. Mlawer, M. W. Shephard, S. A. Clough, and W. D. Collins (2008), Radiative forcing by long - lived greenhouse gases:
Calculations with the AER radiative
transfer models, J. Geophys.
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.»
When you get to
models, the radiative
transfer calculations are highly parameterized and those parameterizations have been known to have been wrong in the past for some
models.
TOAA is also relevant to reducing the large errors associated with numerical
calculation in climate
models of the
transfer of heat and moisture between ocean and atmosphere.
The Wm - 2 you quote are
calculations made from radiative
transfer models.
You could divide up the geography into numerous cells, each with numerous layers of atmosphere; you could divide up the time into many small steps, and work out the dynamics of air masses in a refined way; you could make complex
calculations of the
transfer of radiation through the air; you could construct detailed
models for surface effects such as evaporation and snow cover... but you could not do all these at once.
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.
This is handled differently by different
modelling groups: some specify aerosol properties for purposes only of the radiative
transfer calculations.