Not exact matches
While the
Earth loses most of its heat through plate recycling (the formation and subduction of new crust inherent in plate tectonics), Venus probably loses its internal heat
by surface volcanism and
by conduction through its crust.
Heat is passed (largely
by conduction) back to the
Earth's land and sea surface from the atmosphere (there is also some re-radiation of LWIR back to the surface from the lower reaches of the atmosphere).
Temperature tends to respond so that, depending on optical properties, LW emission will tend to reduce the vertical differential heating
by cooling warmer parts more than cooler parts (for the surface and atmosphere); also (not significant within the atmosphere and ocean in general, but significant at the interface betwen the surface and the air, and also significant (in part due to the small heat fluxes involved, viscosity in the crust and somewhat in the mantle (where there are thick boundary layers with superadiabatic lapse rates) and thermal conductivity of the core) in parts of the
Earth's interior) temperature changes will cause
conduction / diffusion of heat that partly balances the differential heating.
(Within a typical atmosphere, as on
Earth, heat transport
by conduction and molecular mass diffusion are relatively insignificant for bulk transport (there is some role in smaller - scale processes involving particles in the air), except when the net radiative flux and convective flux are very very small (not a condition generally found on
Earth).
Re 40 simon abingdon — there is very little mass loss to space (can be significant for evolution of conditions over geologic time or in more extreme conditions, but not for
Earth like conditions over the timescales over which climatic equilibrium is determined), and latent and sensible heat are transported
by conduction and convection and mass diffusion, which can't significantly extend outside the atmosphere.
6 Transfer of Energy Through Space Once the Sun's energy reaches
Earth, it travels through different materials
by conduction, convection, and radiation.
The atmosphere is warmed primarily
by conduction and convection at the
Earth's surface, not
by radiation — standard school physics.
At normal
Earth temperatures heat loss is mostly
by conduction and convection, radiation only dominates at much higher temperatures.
Such temperature changes at the
Earth's solid surface then propagate into the subsurface
by heat
conduction through the soil and rock.»
As to the absorption of long - wave radiation from the
earth's surface, while it may be true that carbon dioxide and water together do absorb certain frequency ranges of that radiation, I don't think that that matters a whole lot because most of the heat from the surface is transported to the top of the troposphere
by conduction, convection and latent heat of vaporization of water during the day.
The atmosphere is mainly warmed up
by the
Earth mass thru evaporation, convection,
conduction, radiation not
by greenhouse gasses or gases.
«the atmosphere is warmed
by conduction from
Earth's surface, this lapse or reduction in temperature is normal with increasing distance from the conductive source.»
Because the atmosphere is warmed
by conduction from
Earth's surface, this lapse or reduction in temperature (is?)
«The
Earth's internal thermal energy flows to the surface
by conduction at a rate of 44.2 terawatts (TW), and is replenished
by radioactive decay of minerals at a rate of 30 TW.»
Sensible heat flux is the process where heat energy is transferred from the
Earth's surface to the atmosphere
by conduction and convection.
The warming primarily occurs
by conduction from the
earth's surface directly to the atmosphere.
However there would then be more
conduction, convection and on
Earth more evaporation from the surface for an increased upward energy flow which would work to maintain the lapse rate set
by sun and pressure.
«in an isotropic non GHG world, the net would be zero, as the mean
conduction flux would equalize, but in our
earth it is still nearly zero» if the atmosphere were isothermal at the same temperature as the surface then exactly the downwelling radiation absorbed
by the surface would be equal to the radiation of th surface absorbed
by the air (or rather
by its trace gases) and both numbers would be (1 - 2E3 (t (nu)-RRB--RRB- pi B (nu, T) where t (nu) is the optical thickness, B the Planck function, nu the optical frequency and T the temperature; as the flow from the air absorbed
by the surface is equal to the flow from the surface absorbed
by the air, the radiative heat transfer is zero between surface and air.
Somehow, largely
by conduction, convection and latent heat, and such means other than
by radiation, heat flows from the
earth's surface to somewhere, where it is then radiated into space.
«Here on
Earth, environmental heat is transferred in the air primarily
by conduction (collisions between individual air molecules) and convection (the circulation or bulk motion of air).»
From his membrane around a volume / mass below TOA, quite appropriate to observe that neither convection nor
conduction can ultimately cool planet
Earth surrounded
by space.
There may be convection and
conduction within the atmosphere (up to about 10 Km as found
by E. O. Hulburt in 1931), but between the
Earth (including the atmosphere) and «space», heat is transferred via radiation since space is a vacuum (you need matter for
conduction and convection, also shown
by Hulburt in 1931).