Consider a small outward displacement of a fluid element. It adjusts to the ambient pressure while retaining its specific entropy and stellar composition, so an adiabatic process gives . Its excess mass density over the new surroundings is, to first order,
Restoring buoyancy requires this bracket to be positive. With , the Schwarzschild criterion is therefore
Equality is neutral stability. For uniform mean molecular weight, the ideal gas law gives . Since hydrostatic equilibrium pressure decreases outward, the inequality is equivalent to . Dividing the radiative diffusion in a star and hydrostatic equilibrium stellar structure equations gives
This is the stellar radiative temperature gradient test for stellar convective stability.
In the thin upper stellar atmosphere take , and use gas pressure dominance. The prescribed opacity becomes . Dividing the two structure equations then yields
At zero optical depth, the atmospheric boundary has and negligible gas pressure. Integrating from that boundary, with , gives
To locate the onset, put . Logarithmic derivative gives , hence
This starts at zero at the outer boundary and increases inward. It first reaches at
The corresponding optical depth is , so the onset lies inside the stellar atmosphere. This is grey-atmosphere convection onset with thirteenth-power opacity.
Let the interior of the fully convective star have , with spatially constant. At its boundary is fixed, so the atmospheric pressure formula gives
The Stefan–Boltzmann law, with , consequently implies
The ideal gas equation transforms the interior relation into
For completeness, the mass-radius scaling follows by taking and with . Hydrostatic equilibrium and mass conservation reduce to the Lane-Emden equation , with , . Its fixed dimensionless profile gives and . Eliminating gives , or . Thus at fixed stellar composition. Equating this with the atmospheric expression gives , and hence
This Hayashi relation with thirteenth-power opacity concerns the interior of a fully convective star beneath a thin stellar atmosphere. The coefficient may vary between stars; spatially constant specific entropy does not mean equal specific entropy across the whole sequence.
Statistical temperature is defined by , with entropy . Maximizing total entropy when two systems exchange energy makes their derivatives equal, explaining why equal temperature characterizes thermal equilibrium and why a thermometer can measure another system.
For a dilute monatomic ideal gas, Gaussian integration of momenta gives the classical partition function , with . Differentiating its logarithm gives
At fixed volume, gas pressure is proportional to absolute temperature; at fixed pressure its volume is proportional to temperature. A low-density gas thermometer therefore supplies an absolute calibration independent of the gas species in the ideal limit. A liquid-in-glass column responds to the difference between liquid and glass thermal expansion, which need not be exactly linear. Calibration against gas temperatures and correction for expansion nonlinearities improve a simple two-point column scale; an ideal-gas law is not a law of the liquid itself.
For blackbody radiation, the electromagnetic mode density is per volume and frequency interval, including two polarizations. For one photon mode, summing its occupation numbers gives . Differentiation of gives mean energy , so the Planck distribution follows. Converting to wavelength gives spectral radiance
At its maximum, satisfies , whose positive root is . Thus the Wien displacement law is
This calibrates a wavelength-based radiation thermometer and avoids identifying a subjective colour with a universal temperature. A peak per frequency interval has a different numerical location, so the spectral convention must be stated. Real objects require emissivity and atmospheric corrections; fitting a measured spectrum is more informative than choosing its visually brightest colour. Integrating the Planck distribution also gives energy density proportional to and radiative flux proportional to , supplying the complementary Stefan–Boltzmann law calibration.
Use geometrized units with initially, and write , . The given nonextremality assumption makes . Thus the static Killing vector field has a simple zero of its norm at
The exterior is static. For radial null geodesics, , independently of . With , the metric is
which is regular at since . The outgoing null equation is . Inside the future horizon these rays move to smaller radius, while outside they can escape to infinity. Hence the zero is the event horizon. The inner zero of is not another regular Killing horizon: the Killing norm there diverges rather than vanishes. The strict charge bound matters when making the regular extension.
For the Euclidean black-hole regularity condition, continue , consistent with the sign of the given quantum time-translation operator. Set . To leading order and , so the radial–time part of the Euclidean metric is
Introduce the radial proper length coordinate by . Then
The first two terms are a polar plane with angle . Smoothness at its origin requires
A different period would make a conical singularity. The time coordinate is normalized to proper time at infinity, so no further asymptotic redshift factor is needed. The cancellation of proves the charge independence of the Euclidean horizon period under a regular radial conformal factor; this argument would fail at .
To justify the thermal interpretation, analytic continuation of the time-evolution operator gives . Its matrix element is an imaginary-time propagation kernel. Identifying the initial and final configurations and integrating over them takes its trace, giving the Euclidean path integral . In an energy eigenbasis each state has weight , exactly the Boltzmann factor of a canonical ensemble. Thus the geometrically required period is the inverse Hawking temperature. With dimensions restored, an imaginary time period gives . Consequently
Here is mass in ordinary units; for a neutral hole and the physical imaginary-time period is . Bosonic thermal fields are periodic and fermionic fields antiperiodic over that same Euclidean period. The relation to the canonical density operator, not just dimensional reasoning, identifies the temperature.
For an evaporation estimate take a neutral, isolated Schwarzschild black hole and approximate its radiated power with the Stefan–Boltzmann law. Its area is , and the photon Stefan-Boltzmann constant is . Substituting the temperature gives
The black-hole evaporation speeds up as the mass decreases. Integrating, rather than dividing the initial rest energy by the initial power, gives
The corresponding initial Hawking temperature is about K. This is the Stefan-Boltzmann estimate of Schwarzschild evaporation time at the level of accuracy requested. Greybody factors and other emitted species alter the numerical coefficient, but not the leading cubic scaling of a large isolated hole. The estimate assumes negligible accretion or ambient radiation absorption; a stellar-mass hole in the present cosmic radiation bath is not currently losing mass at that isolated-hole rate. Finally the semiclassical formula does not describe the Planck-scale endpoint: extrapolating it to zero mass is an estimate of the macroscopic lifetime, not a proof of what the final quantum object is.
Use radiative homology with proton-proton burning and inverse-fourth-power opacity, retaining the composition factors throughout. To distinguish the stellar radius from the stellar gas constant, write them as and . With gas pressure alone, introduce the scale factors
The ideal gas equation gives , and . Substitution into hydrostatic equilibrium and mass conservation gives
so and .
Set . The radiative diffusion in a star equation, with the stipulated opacity, becomes
Here . Thus
The luminosity equation follows from the specific heating rate of the Proton–proton chain:
Consequently
These give all four dimensionless stellar structure equations with their numerical coefficients.
The stellar homology assumption means the dimensionless profiles are shared across the models, not merely that an individual model can be written in dimensionless coordinates. The displayed equations then require and to be fixed. Holding the universal constants and fixed gives
Equating the two cancels and yields . Therefore the radius and mass-luminosity relation are
The mass-independent radius is a consequence of the particular heating and opacity exponents in this model; it is not a general radius law for main-sequence stars.
Initially is the same for all stars. The adopted mean molecular weight also has the same initial value, neglecting its small direct dependence on . Thus . At fixed luminosity, the Stefan–Boltzmann law gives
The stars compared here can have different masses; the luminosity law adjusts the mass to keep fixed.
For the evolution, take the stellar mass as constant and maintain homogeneous composition. The available energy in the remaining hydrogen is , so conservation of energy in the nuclear-powered model gives
This includes the entire mixed hydrogen reservoir, not just the mass in a central burning region.
To determine the turnoff mass of a homogeneously mixed proton-proton-burning population, write the luminosity law as , where
Separating variables, the time to evolve from to is
For a common and , this integral is a positive finite constant independent of . It follows that the turning-off stars satisfy
The integration retains the evolving luminosity and mean molecular weight; replacing by its initial value is unnecessary.
For the Schwarzschild criterion, displace a small gas parcel upwards. Assume its composition is unchanged, it remains in pressure balance with its surroundings, and it moves quickly enough that heat exchange is negligible. The parcel obeys the adiabatic equation of state . Combining this with the ideal gas equation gives , so its adiabatic temperature gradient is .
Let the surrounding temperature gradient be . For an upward displacement , the parcel's temperature relative to its new surroundings is
If , this is negative: the parcel is cooler and, at equal pressure and composition, denser than its surroundings. It therefore sinks back; a downward displacement likewise gives a restoring buoyancy force. If the inequality is reversed, the displaced parcel continues to rise. The stability condition is thus
Equality is the neutral boundary. There is no composition-gradient term because the ideal-gas parcel and the background have the same mean molecular weight.
In the thin upper stellar atmosphere, take a plane-parallel approximation with constant , optical depth increasing inward, and zero overlying pressure . Hydrostatic equilibrium in optical depth gives . The ideal gas equation converts the stipulated opacity into
Define , so the given grey atmosphere relation is . Integrating from the surface gives
This proves the required pressure law. In particular times a function only of and .
For the grey-atmosphere convection onset with density-linear opacity, differentiate the two profiles to obtain the radiative temperature gradient:
It increases monotonically from zero, since , and first reaches the adiabatic temperature gradient at . Therefore
Below this point the radiative stratification is unstable and convection must transport some of the outward energy flux.
At the outer convection boundary, depends only on , so and for fixed . The matching constant in is . Consequently
This temperature form of the polytropic relation follows from an ideal monatomic adiabat; its is not the density-polytrope coefficient in Question 3.
For the deep radiative boundary beneath a power-law-opacity convective envelope, negligible envelope mass and absent local energy generation give and . Divide the radiative temperature equation by the pressure equation to get the stellar radiative temperature gradient
This is the gradient that would be needed if radiation alone carried , and it is the quantity to compare with even while the actual region is convective. The deeper Kramers' opacity law gives . Substituting yields
As rises inward this decreases, so the transition back to a stable radiative interior is at
Thus . Using the outer matching and the Stefan–Boltzmann law,
The mass and radius cancel. Hence, at fixed opacity coefficients and composition,
This uses the same adiabat through the convection zone and distinguishes its inner transition temperature from its outer onset temperature.
Substitute the Killing-flow four-acceleration and stationary pressure into the relativistic Euler equation. It gives
For the equation of state of blackbody radiation, , this becomes . The barotropic hydrostatic first integral therefore gives, on each connected nonvacuum fluid region,
This is the stationary radiation density law. Combining it with the Stefan–Boltzmann law also gives the Tolman–Ehrenfest relation .
At a regular finite free surface, a smooth Killing vector field has finite norm. Hence cannot approach zero there. More globally, its norm has a finite upper bound on a compact regular fluid closure, which bounds the density away from zero whenever . If the timelike norm instead tends to zero, the density diverges. Thus a radiation fluid has no regular free surface: a finite radiation-filled cavity needs a material wall supporting nonzero pressure, rather than an unsupported radiation-vacuum interface.
Introduce the characteristic scales
Then , and . The gas-only equation of state gives the important dimensionless identity . The PDF's CNO cycle approximation has temperature power 13; the converted TeX's power 1.3 is an OCR error.
Since , the mass and hydrostatic pressure support equation immediately become
Thus and . The stellar structure equations for nuclear heating give
so
For radiative diffusion in a star, , and therefore
This gives the radiative gradient coefficient
In an efficiently convective region, the monatomic adiabatic temperature gradient is . Hence . If the radiative gradient is shallower, radiation suffices; if it is steeper than the adiabatic gradient, the Schwarzschild criterion selects convection and the shallower adiabatic profile. Thus
The regular central conditions are with finite positive . In particular and , so the pressure and temperature derivatives tend to zero at the centre. The normalized surface has . In the idealized zero-pressure, zero-temperature surface used for stellar homology, ; a physical photosphere supplies small nonzero surface values that are neglected in these bulk homology relations.
The common dimensionless profiles and boundary conditions keep constant. With fixed , constant yields . Substitution into the nuclear coefficient then gives . Consequently the CNO homology with density-dependent inverse-cubic opacity is
The Stefan–Boltzmann law gives . Eliminating mass, rather than dropping composition dependence, gives the Hertzsprung-Russell diagram relation
The additive constant depends on the fixed physical and structural coefficients; logarithms refer to fixed choices of units.
For physical evolution time , distinct from the dimensionless temperature , hold stellar mass fixed and put , . The mean molecular weight approximation and the homology relation give . Converting hydrogen mass to helium releases energy at rate , so fuel conservation is . Therefore
Integration with the initial composition proves the homogeneous fuel-depletion luminosity feedback law
It is valid while hydrogen remains and the homology assumptions hold. Fuel exhaustion occurs when , before the formal denominator vanishes; the apparent infinite luminosity is not a physical endpoint of this stellar model.
Let be the gravitational energy. Multiply the stellar hydrostatic equation by and integrate through the star. Integration by parts and zero surface pressure give
while its hydrostatic right-hand side is . Hence the stellar virial theorem is
There is a genuine reference-sheet error to resolve. A monatomic ideal gas with adiabatic exponent has specific internal energy of an ideal gas , not the printed on PDF page 2. The latter would give total internal energy and zero total energy, inconsistent with radiating contraction. The following derivation uses the consistent monatomic value.
A fully convective star is approximately isentropic and has an adiabatic stellar polytrope with index . The given polytropic gravitational-energy formula yields . The virial relation gives total internal energy , so total energy is . At constant mass with no nuclear heating, Kelvin-Helmholtz contraction obeys , whence
Here denotes physical time.
In the plane-parallel atmosphere, the inward optical depth satisfies , so hydrostatic equilibrium in optical depth gives . Neglecting radiation pressure, and the specified opacity becomes . Therefore
The grey atmosphere relation and the boundary integrate to
To apply the Schwarzschild criterion, put . Logarithmic differentiation gives
This increases inward, starting from zero. Marginal convection has , so . Since , the grey-atmosphere convection onset with seventeenth-power opacity is
The purely radiative atmosphere is used only up to this boundary.
The convective relation is spatially uniform in its entropy coefficient at each instant; can change as the star radiates and contracts. At the convection boundary is a fixed number, so at fixed composition and opacity normalization. Thus
On the other hand, the central scalings for the stellar polytrope give and . Hence, at fixed composition,
Equating the interior and atmosphere expressions yields . Applying the Stefan–Boltzmann law then proves the Hayashi contraction with seventeenth-power opacity relation
At fixed mass write , with constant and . The contraction equation is , where . Direct integration gives
Multiplying through by and substituting the current luminosity gives
For the stated very large initial radius, or after that initial-radius term becomes negligible,
This is the luminosity-age relation within the contraction model, rather than an assertion that a physical star begins at literally infinite radius.
Write the photon energy density as , where by the Stefan–Boltzmann law. The photon gas has pressure and zero photon chemical potential. The first law of thermodynamics therefore gives
Dividing by and integrating gives the entropy density of a photon gas:
The integration constant is fixed to zero at zero temperature, consistently with the Third law of thermodynamics.
The inequality says interactions act much faster than the expansion time, maintaining local thermal equilibrium. For adiabatic reversible expansion with no additional source of entropy, cosmological entropy conservation fixes the entropy in a comoving volume. Since that volume scales as , and the relativistic degrees of freedom are fixed here, is constant. Thus
During radiation domination, the Friedmann equation gives , and hence . Fast interactions alone would not exclude an additional entropy-producing process; changing relativistic species likewise changes the simple temperature scaling.
Use stellar homology: dimensionless density, temperature and luminosity profiles are taken to have the same shape, so the dimensional scale relations follow from the structure equations. Mass conservation and hydrostatic support give
The ideal gas equation then gives , with the dimensional constants held fixed. The specific stellar energy-generation rate has the prescribed hydrogen factor and temperature exponent, so
Independently, radiative diffusion in a star gives , hence
Equating the nuclear supply and radiative transport establishes composition-dependent CNO homology:
At one fixed composition, these reduce to and as required.
The Stefan–Boltzmann law gives , so . Thus the logarithmic Hertzsprung-Russell diagram slope along this zero-age main sequence is
Increasing mass moves upward and leftward on the conventional diagram, whose temperature axis is reversed.
For composition changes, neglect the small heavy-element contribution to the mean molecular weight and set . Then . The fixed trace catalyst abundance is absorbed into ; this is not an assertion that an exactly metal-free star can undergo CNO burning. Substitution into the homology laws gives
For a retained, nonnegligible fixed metallicity , the corresponding mean-molecular-weight factor is instead. The displayed requested formula uses the trace-metal approximation.
At fixed mass, differentiating with respect to at the formal reference gives
Consequently
and the initial fully mixed hydrogen-burning evolutionary track has slope
Hydrogen depletion has , so both luminosity and effective temperature initially increase. The star therefore moves upward and leftward, on a shallower logarithmic track than the mass sequence. The figure uses dimensionless luminosity and temperature relative to its initial reference star; the track is computed for declining at constant mass.
Figure 1.
Zero-age radiative homology sequence and the fixed-mass fully mixed hydrogen-burning track
. Details.
Ordinary cluster main-sequence turn-offs instead evolve toward brighter, cooler, more extended configurations and eventually the giant region. Normal stars are therefore not mixed throughout their entire mass during hydrogen burning: the core composition changes while the envelope retains hydrogen, and composition and entropy gradients develop. Core exhaustion and subsequent shell burning then produce very different structural evolution. Complete mixing is a special evolutionary scenario, not the standard explanation of ordinary giant formation.
These hydrogen-burning scalings must not be extrapolated literally to . Their vanishing nuclear coefficient would make the inferred radius tend to zero and the effective temperature singular; in reality hydrogen exhaustion requires a different structural and energy-generation model. A homogeneous remnant may be helium-rich, but its later structure is not described by the same CNO law. Also, the cover-sheet radiation-pressure expression has a temperature-power typo: the physical term is . Radiation pressure was neglected in this derivation, so that typo does not enter the calculation.
A passive disk is heated predominantly by intercepted stellar radiation, rather than by its own viscous dissipation. A rough luminosity criterion, ignoring geometric factors, is
The intrinsic accretion disk luminosity is of order , with additional accretion energy potentially released at the stellar surface. The local test is more precise: absorbed irradiation must dominate the viscous flux at the radius being considered. For an ordinary steady Keplerian accretion disk, sufficiently far outside its inner edge,
where is the irradiation grazing angle of a disk. Reflection, very small incidence angles and shadowing can invalidate a simple total-luminosity comparison. The following calculation assumes an illuminated, absorbing surface.
At a point on the upper surface, the outward unit normal in the meridional plane is proportional to , and a light ray from the point source is directed along . Its flux through the upper face is the incident inverse-square flux times minus their scalar product:
For a thin disk with small surface slope this becomes
The tangent slope and ray slope differ by . Positive incidence requires disk flaring, , and an unobstructed ray from the star. A negative value of the formula would mean that direct illumination of this face is absent, not that it receives a negative heating flux. The hierarchy makes the finite angular size of the star negligible here.
Let , so the ideal gas equation of state gives the isothermal sound speed . In the stellar vertical gravitational potential, hydrostatic equilibrium has vertical acceleration , where . Integration of gives a Gaussian atmosphere with disk scale height
Consequently satisfies . Substitute this into the stipulated Stefan–Boltzmann law and the irradiation flux:
Here specifies surface height in units of disk scale height and is unrelated to the wind-energy fraction in the preceding solution. This separable differential equation integrates exactly to
If the thin-disc solution is formally matched to , then , giving
It follows that the flaring passive disk asymptotic is
This applies in the thin intermediate region , in addition to the point-source and stellar-gravity assumptions. The corrections are of relative order . In particular, the printed hierarchy must still be accompanied by the initial thin-disc condition : if , radii larger than cannot satisfy that approximation. The matching at is an extrapolation used to set an integration constant; the derivation is not a valid treatment of a thick surface at itself.
Identify the stellar surface temperature with its effective radiating temperature, so that luminosity of a spherical blackbody gives . The given stellar surface scale height has , hence . Substituting into yields
Thus a small stellar surface scale height leaves a wide interval above and below in which the thin disk flaring law can apply. The point-source approximation imposes the stronger lower cutoff obtained from :
This cutoff is still much smaller than when . The full interval is therefore , whenever these bounds overlap. An assumed thickening radius must lie above the lower cutoff for all of the original approximations to hold simultaneously. The stellar luminosity-temperature relation is essential to the final comparison; independent arbitrary values of and would not imply it.
The solar constant measures the incident power per area normal to the sunlight. A spherical Earth of radius intercepts sunlight over the disc , but radiates over its surface . For uniform surface albedo in the global energy-budget approximation, absorbed power is . Treat the surface as a blackbody, assume efficient heat redistribution and neglect internal heating. The Stefan–Boltzmann law and the planetary surface energy balance then give
For a nonuniform surface the same power balance instead defines an effective planetary equilibrium temperature, ; its fourth root is not generally the arithmetic mean of the local temperatures. Also, area-averaging the surface albedo is an approximation to the properly insolation-weighted averaging. These are the simplifications implicit in the naked-planet calculation.
Take , so . The changed area is , giving
The initial planetary equilibrium temperature is . Thus
The differential estimate gives the same result. This is the global equilibrium response of the specified model, not the immediate local Arctic warming or the full atmospheric response.
The exceptional 2007 Arctic sea ice decline is best understood as a weather event acting on an already vulnerable ice cover, with several reinforcing pathways. Warmer air increases downward long-wave heating, lengthens the melt season and delays autumn freezing. Changes in snowfall and the development of melt ponds also change the surface energy balance. Air temperature alone, however, does not identify the source of the observed bottom melt: heat must reach the underside through the ocean.
Warmer Atlantic-origin water supplies a larger subsurface ocean heat content after entering through Fram Strait and the Barents Sea. Its influence on sea ice depends on vertical exchange, because a cold, relatively fresh halocline normally separates it from the ice. Erosion of that halocline, through altered freshwater distributions, wind-driven mixing or changes in circulation, weakens stable density stratification and can increase upward ocean heat flux. A warmer Atlantic layer without this exchange need not produce immediate extra bottom melt. Conversely, warmer Pacific inflow through Bering Strait introduces heat into the shallower western Arctic; advection through the Chukchi Sea provides another route to ice retreat and ocean heat storage.
The Arctic Oscillation changes winds, ice motion and export. Positive phases during earlier years helped remove old, thick ice through Fram Strait and left a younger, thinner pack. Summer 2007 also had a pronounced pressure contrast between the Beaufort region and the Eurasian Arctic, associated with the Arctic dipole anomaly. Its winds promoted ice displacement and warm-air transport. The summer circulation should not be described merely as a particular Arctic Oscillation index: the spatial pattern and the preconditioning from earlier years both matter.
Long-term thinning reduces the latent heat of fusion needed to remove the remaining ice. Replacement of multi-year sea ice by first-year sea ice therefore makes a given summer heat input more effective, while mobile thin ice is more readily redistributed or exported. These dynamical changes can expose open water early enough for substantial solar absorption. Water and melt ponds have lower surface albedo than snow-covered ice, so absorbed short-wave energy rises, increasing upper-ocean heat storage and bottom melt. This ice-ocean albedo feedback also delays refreezing. In the Beaufort Sea in 2007, enhanced solar heating of the newly exposed upper ocean was an especially important explanation of extreme bottom melt. Thus thinning and wind-driven opening can initiate retreat, while solar heating amplifies it; changes in Atlantic or Pacific heat supply can further reinforce the process where circulation permits.
A further positive climate feedback involves terrestrial carbon. Loss of the insulating ice cover permits greater autumn and winter transfer of stored ocean heat to the atmosphere. The resulting regional warming can increase thaw of coastal and inland permafrost. Microbial decomposition of previously frozen organic material then releases carbon dioxide, and oxygen-poor wet environments also release methane. These greenhouse gases strengthen the greenhouse effect, increasing global warming and further thaw. The permafrost carbon feedback provides the causal chain from summer ice retreat to an additional global influence. An Arctic methane feedback involving subsea sources is also possible, but the amount actually reaching the atmosphere depends on oxidation and transport; an abrupt, wholesale release is not a necessary consequence of summer ice loss.
For the bottom-melt estimate, use and the given . Assume the ice at the melting interface is already at its local freezing temperature; there is then no separate sensible-heating term. Per square metre the latent heat requirement is
July through September has days, so the mean ocean heat flux to the ice is
Using instead gives about , within the intended accuracy. Around the date of this examination, the estimated net anthropogenic radiative forcing since preindustrial times was about ; doubling carbon dioxide gives about . The calculated bottom flux is tens of times larger. There is no energy-budget contradiction: it is a local, summer ocean-to-ice heat transfer, supplied by absorbed sunshine, stored heat and transport, whereas radiative forcing is a global perturbation to the radiation budget. Redistribution and local absorption can produce much larger regional fluxes than the global forcing.
For an already ice-free water column, take and liquid-water specific heat capacity . Assuming all the same energy remains in that uniformly mixed column,
If the water initially lies near the seawater freezing point, about , its final temperature is approximately . An absolute final temperature requires that additional initial condition; the energy calculation itself determines only the temperature increase. The given ice specific heat capacity is not the appropriate value for heating liquid seawater.
Efficient convection makes the interior follow a nearly adiabatic process and maintains uniform specific entropy. For the fully ionized monatomic ideal gas, the specific-heat ratio is , so the adiabatic temperature gradient gives . Integrating at a fixed time gives
The coefficient is spatially constant because the composition and specific entropy are uniform. It can change as the star loses energy. Equivalently the gas is an adiabatic stellar polytrope with and polytropic index ; and the pressure-temperature coefficient are different quantities.
This fixes the dimensionless Lane-Emden equation profile throughout a stellar homology sequence. Writing in the mass integral gives , with a fixed positive shape constant . Integrating the stellar hydrostatic equation through the same profile, with negligible surface pressure compared with central pressure, gives . Hence
These are homology scalings of central stellar pressure. Substituting the central quantities into yields
Thus is constant for the fixed stellar polytrope family.
At the approximate photosphere, take and use the ideal gas relation . The prescribed opacity gives
The stellar surface boundary condition and surface gravity of a star therefore imply
This is the temperature-four special case of convective contraction with power-law opacity.
Using the Stefan–Boltzmann law, the luminosity is
For , the supplied gravitational-energy formula is . The stellar virial theorem for a monatomic gas gives , so the total energy is . During Kelvin-Helmholtz contraction, with constant mass and no significant nuclear source, . Thus
Multiplying by and integrating gives
The sign makes the radius decrease as time increases.
When the accumulated contraction term dominates the initial-radius term, this yields . Combining it with the central ideal gas temperature gives the late-time central-temperature scaling
Replacing by gives the stated late-time form. The asymptotic step also requires a time long enough to forget the initial radius, not merely a choice of zero for the age.
The Maykut-Untersteiner model solves a seasonally forced, one-dimensional sea ice thermodynamics problem with a snow layer above saline ice. Let increase downward from the upper surface, with snow–ice interface and ice bottom . Write for conductive heat flux, positive downward, and for downward shortwave radiation penetrating the material. Local energy conservation gives
For , the radiation term is : absorption heats the interior. Here is the derivative of specific enthalpy with temperature at prescribed ice salinity, and includes the latent heat of changing brine fraction. Using only pure-ice specific heat capacity would omit this storage. A usual approximation has and , with in degrees Celsius and positive, unit-dependent constants . Thus warmer saline ice has larger effective heat capacity and lower thermal conductivity. Layerwise constant gives the usual finite-layer heat equation; full differentiation retains its spatial variation. Snow uses its own density and thermal conductivity, and its stronger extinction can make shortwave penetration negligible beneath it.
Define the net atmospheric input to the upper surface by
where is albedo, is turbulent sensible heat loss and is turbulent latent heat loss. Their signs can reverse. The outgoing longwave term uses the Stefan–Boltzmann law. Subtract the penetrating shortwave , because it heats the interior rather than the infinitesimal surface. If is surface ablation speed and the density of the material currently exposed, the upper boundary obeys
Below the melting point, and the flux balance determines . Once it reaches , the positive excess produces surface ablation; snow melts first, and only afterwards does that ablation remove ice. At the snow–ice interface, absent interfacial phase change,
At the base, and the Stefan condition is
Here is signed bottom growth speed, and is ocean heat flux toward the ice. An upward conductive loss freezes ice; an excess melts it. For a prescribed upward turbulent ocean heat flux, the model needs no separate ocean temperature solution. A water-side closure could write at the boundary in this downward coordinate. Snowfall is an independent mass input: with snowfall mass flux , in a constant-density approximation. The ice thickness obeys . Compaction or refreezing, if added, requires corresponding mass and energy terms rather than counting snowfall directly as ice growth. These boundary conditions and interior equations determine temperature, surface melt and basal growth together.
Under periodically repeated annual forcing, annual sea-ice thermodynamic equilibrium is a periodic annual state, not constant thickness:
Winter accretion then balances net annual ablation. “Equilibrium thickness” normally denotes a mean or a specified point in this annual cycle. Different forcing can instead eliminate a perennial-ice solution.
Increasing ocean heat flux reduces bottom growth directly in the Stefan condition, lowering equilibrium thickness and eventually removing perennial ice. The stabilizing winter response is visible in the approximate conductive flux
when ice thins, conductive loss and winter regrowth increase. More snow lowers this flux and inhibits winter growth. However, snow also raises albedo and delays summer exposure of dark ice. The competing snow insulation and summer ice protection effects mean an annual snow sensitivity cannot be deduced from winter insulation alone. Under the original forcing, the Maykut-Untersteiner model gives an almost flat annual-thickness response below about annual snow depth, followed by strong thickening as snow persists into summer. This particular transition is not a universal threshold for other forcing or snowfall timing. Increasing summer albedo reduces absorbed solar energy, reduces surface and internal melting, and increases equilibrium thickness; sufficiently low albedo removes perennial ice. The original thermodynamic sensitivity calculations establish these three responses.
Figure 1.
Three schematic equilibrium-thickness sensitivities: ocean heat flux, annual snow depth and summer albedo
. Details.
The three curves are original qualitative sketches, not a new numerical integration or digitization. The snow marker refers to that historical forcing; the unnumbered loss boundaries and ordinate indicate trends rather than calibrated universal thresholds.
For the summer retreat discussed around the time of this examination, the proposed mechanisms act as follows.
These processes overlap: circulation causes export, export changes thickness and open-water fraction, and those changes alter solar absorption. Without specified regional budgets there is no defensible unique percentage partition. For enhanced Beaufort summer basal melt, upper-ocean solar heating and western-Arctic heat pathways are more directly relevant than invoking unmodified heat from a deep, isolated Atlantic layer. ice-mass-balance observations of extreme Beaufort melt identify increased solar absorption in open water as an important source.
Take as an explicit ice-density approximation and use the supplied . The latent heat for basal ablation is
June–September contains about days, so
Using would give . This is the net flux used for melting: the gross ocean heat flux can also supply conductive losses and changes in cold content. It greatly exceeds an annual central-pack background of a few , but is compatible with a summer upper ocean absorbing solar radiation at tens to hundreds of . For scale, an added open-water fraction , a shortwave input and an ice–water albedo contrast produce additional area-mean absorption before losses. This is an illustrative budget, not a measurement. Wind mixing and circulation can deliver stored solar or advected heat to the underside.
The ice-albedo feedback closes the warming loop: retreat exposes darker water; extra solar absorption warms the upper ocean; basal and lateral melt increase retreat. The stored heat also delays autumn freeze-up, exposing water to atmospheric heat transfer for longer. Its later release warms the atmosphere, but must not be counted as a second source in addition to the solar energy that originally entered the ocean. In winter, greater heat loss from open water and rapid growth of thin ice partly oppose the summer positive feedback.
In stellar homology, the dimensionless radial profiles are the same after scaling radius, enclosed mass, pressure, temperature and luminosity. At corresponding radii let , , , and . The printed is understood as this local radial scaling, with surface radius .
Let and keep composition, opacity coefficient and nuclear coefficient fixed first. Mass conservation gives , and hydrostatic equilibrium gives . The ideal gas law then gives . Scaling the stellar energy-generation rate equation and the stellar radiative temperature gradient gives respectively
The second follows from , not from energy production. Equating the two luminosity scalings gives
This assumes the denominator is nonzero and a consistent homologous family exists. If the mean molecular weight differs by , then and
Ratios of the opacity and energy-generation coefficients multiply the right-hand side. Thus fixed composition is a real restriction, not an automatic property of every stellar sequence.
Use the Stefan–Boltzmann law to locate the family on a Hertzsprung-Russell diagram. It implies and
For proton–proton chain burning take the usual local approximation , with Kramers' opacity law , . Then
For the CNO cycle with electron-scattering opacity, , so
A conventional local choice gives and slope . Choosing instead gives slope . The source specifies no numerical nuclear exponents, and the effective exponent changes with temperature; the general expression is the unambiguous answer.
Figure 1.
Idealized radiative homology branches on a Hertzsprung-Russell diagram, with pp exponent 4 and CNO exponent 16
. Details.
The Hertzsprung-Russell diagram places hotter stars to the left. Its branches rise toward higher luminosity and mass, and the CNO cycle/electron-scattering opacity branch has the steeper logarithmic slope. Their illustrative joining point and normalization are arbitrary because the proportional opacity and reaction laws do not specify absolute stellar scales. These are the fully radiative ideal-gas homology predictions, not exact observed main sequence relations: convection and increasing radiation support limit those assumptions in real stars.
The standard thin-disk dissipation flux, summed over both faces, follows by substituting the Keplerian accretion disk profile into the viscous heating rate:
The Stefan–Boltzmann law gives because there are two emitting faces. Local radiative equilibrium consequently gives the effective-temperature profile of a zero-torque disk
Here is the Stefan-Boltzmann constant. The scale is not the temperature exactly at the inner boundary: the zero-torque inner boundary condition makes that formal temperature zero. Maximizing shows that the maximum effective temperature of a zero-torque disk occurs at , with .
At equal central mass and accretion rate, characteristic effective temperatures scale as . Thus, comparing corresponding values of ,
The neutron-star disk is about 180 times hotter. The Planck law and Wien displacement law move its characteristic emission to about 180 times higher frequency, or 180 times shorter wavelength. A white dwarf disk commonly emits in optical and ultraviolet bands, while the hotter neutron star disk can emit in X-rays. Absolute bands require an actual accretion rate; the relative shift follows directly from the stated scaling.
For a slowly rotating central star, the accretion-disk boundary layer radiates a luminosity . A layer of thickness comparable to the disk scale height has emitting area times a geometric constant. Applying the Stefan–Boltzmann law to this blackbody area gives
Comparing with gives the boundary-layer temperature scaling
Only the scaling is fixed: for a two-faced annulus of area , for example, . A surface belt gives a different order-one coefficient.
For a thin disk, , so a comparable luminosity emerges from a smaller emitting area at a higher effective temperature. The boundary-layer emission is harder than the disk emission, with its Planck law peak shifted to higher frequency. It is also closer to a single-temperature component than the broad multitemperature blackbody disk spectrum, under the adopted uniform-temperature approximation. Rapid stellar rotation weakens the heating and this conclusion's temperature contrast.
For PP chain burning and the Kramers' opacity law, insert , , and into the homology relations for radiative stars:
Thus the radiative homology with proton-proton burning and Kramers opacity is
To obtain the Hertzsprung-Russell diagram slope, apply the Stefan–Boltzmann law :
Equivalently . The Hertzsprung-Russell slope of a stellar homology sequence refers here to logarithmic luminosity versus logarithmic effective temperature; a conventional diagram reverses its horizontal axis, so the line descends toward the right.
For fixed composition, electron-scattering opacity is effectively independent of mass density and temperature, so . With the specified CNO cycle exponent , the homology relations for radiative stars give
The radiative homology with CNO burning and electron scattering is therefore
The Stefan–Boltzmann law now gives
Equivalently . These slopes are illustrated with arbitrary separate reference-model normalizations:
Figure 1.
Logarithmic Hertzsprung-Russell slopes for the two idealized radiative homology sequences, with temperature increasing to the left
. Details.
The proton–proton/Kramers model applies to the lower-mass regime; the CNO/electron-scattering model applies to the higher-mass regime. Higher-mass cores are hotter, making the more temperature-sensitive CNO cycle efficient, and highly ionized material favors electron-scattering opacity. These are the stated idealized radiative, gas-pressure-supported sequences: a fully convective low-mass star or a radiation-pressure-dominated massive star needs a different structural model. The intersection of independently normalized lines in the figure does not specify a physical crossover mass.
Take an unresolved spherical planet at Euclidean distance , with uniform surface temperature , stationary isotropic emission, and no intervening extinction. Isothermality does not by itself imply blackbody radiation; first derive the geometric result for a uniform emergent specific intensity .
The observer sees the projected disc with apparent solid angle . Integrating its specific intensity over that angle gives the observed spectral radiative flux
where is the small angle to the detector normal. For a blackbody, , and the Stefan–Boltzmann law gives . Hence
Equivalently, the surface radiative flux is and the luminosity of a spherical blackbody is , leading to the same result by inverse-square dilution. A uniform wavelength-dependent emissivity multiplies the spectral formula; an atmospheric spectrum can require a full angular radiative transfer integral rather than a single Planck function.