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Showing 1–30 of 324 reference entries

Physics · Earth & cosmosNewtonian gravitation

An inverse-square force models attraction between point masses.

Model
Earth & cosmosRock cycle and geological transformation

Rock materials can change through multiple geological pathways.

Model
Earth & cosmosPlate tectonics

Moving lithospheric plates organize many large-scale geological processes.

Model
Earth & cosmosEarth's water cycle

Water moves among reservoirs above, on and below Earth's surface.

Model
Earth & cosmos · Biology · ChemistryEarth's carbon cycle

Carbon moves through biological, oceanic, atmospheric and geological reservoirs.

Model
Earth & cosmosPlanetary radiative energy balance

Earth's energy storage changes when incoming and outgoing energy differ.

Model
Earth & cosmosAtmospheric greenhouse effect

Infrared absorption and emission affect how Earth loses heat to space.

Model
Earth & cosmosWeather, climate and their time scales

Weather describes short-term conditions; climate describes their longer-term patterns.

Definition
Earth & cosmosOrbits as gravitational motion

An orbiting body can remain in continuous gravitational free fall.

Model
Earth & cosmosStellar fusion and evolution

Main-sequence stars release energy by fusing hydrogen into helium.

Model
Earth & cosmosHot Big Bang and the cosmic microwave background

Expansion and relic radiation support an earlier hot, dense Universe.

Model
Physics · Earth & cosmosFriedmann cosmological evolution

Homogeneity and isotropy reduce gravitational expansion to two balances.

Model
Physics · Earth & cosmosNuclear binding energy

A bound nucleus has less rest mass than its separated nucleons.

Model
Physics · Earth & cosmosExponential radioactive decay

A fixed decay probability per time gives a population timescale.

Model
Physics · Earth & cosmosFission, fusion and reaction energy

Nuclear rearrangement can release or require energy.

Model
Earth & cosmosMinerals, structure and diagnostic properties

Mineral identification combines structural and physical evidence.

Method
Earth & cosmosRadiometric ages and sample history

Isotopic measurements estimate an age only with a suitable geological model.

Method
Earth & cosmosSeismic constraints on Earth's interior

Wave travel, refraction and transmission constrain an interior model.

Method
Earth & cosmosThe geodynamo model

Fluid motion in the outer core maintains much of Earth's magnetic field.

Model
Earth & cosmosWater budgets and storage change

A defined area's water storage changes with total inflow and outflow.

Model
Earth & cosmosDarcy flux and hydraulic conductivity

Groundwater flow is often approximately linear in hydraulic-head gradient.

Approximation
Earth & cosmosOcean circulation and overturning

Wind, buoyancy changes and mixing contribute to ocean transport.

Model
Earth & cosmosGlobal atmospheric circulation

Unequal heating and rotation organize broad circulation patterns.

Model
Earth & cosmosClimate forcing and energy-budget perturbations

External changes can disturb climate's radiation budget.

Definition
Earth & cosmosClimate feedback mechanisms

Climate responses can amplify or damp a change.

Model
Earth & cosmosClimate detection and attribution methods

Attribution compares observed changes with plausible drivers and variability.

Method
Earth & cosmosStellar evolution and fuel stages

Stellar structure changes as core fuel and conditions change.

Model
Earth & cosmosWhite dwarfs, neutron stars and stellar black holes

Different evolutionary outcomes leave different compact remnants.

Model
Earth & cosmosAnnual stellar parallax and distance

Changing observing position permits geometric distance inference.

Method
Earth & cosmosCosmological redshift and distance inference

Spectral stretching carries expansion information but is not one universal distance ruler.

Method
ModelSource checked

Friedmann cosmological evolution

PhysicsEarth & cosmos

Homogeneity and isotropy reduce gravitational expansion to two balances.

Key knowledge

For a homogeneous isotropic perfect-fluid universe, H = ȧ/a, H² = 8πGρ_tot/3 − kc²/a² and ä/a = −4πG(ρ_tot + 3p_tot/c²)/3, with ρ_tot a mass-equivalent density.

Values and equations

H = ȧ/a; H² = 8πGρ_tot/3 − kc²/a²; ä/a = −4πG(ρ_tot + 3p_tot/c²)/3

H
Hubble expansion rate s⁻¹
a
Length-valued scale factor m
ρ_tot
Total mass-equivalent energy density kg m⁻³
p_tot
Total pressure Pa
k
Normalized spatial curvature sign
G
Gravitational constant m³ kg⁻¹ s⁻²
c
Vacuum light speed m s⁻¹
t
Cosmic proper time used for dots s

Conditions and scope

  • Cosmic proper time, scale factor a > 0 in length units and normalized k = −1,0,+1.
  • Total density and pressure include any vacuum component; no additional Λ term is added here. Local inhomogeneity and quantum regimes require other treatment.
Sources · 1

References

Sources retain their recorded scope. A source link alone does not establish verification of every statement.

  1. Lecture Notes on General Relativity (1997): CosmologySean M. CarrollCourse notes · PDFpreposterousuniverse.comRead source

Evidence and review

Equations 8.30–8.37: vacuum fluid, acceleration, expansion and H; source c = 1 restored with mass-equivalent density.

2026-10-10 · Classical FLRW background relations only; historical observational values in the 1997 notes are excluded.

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physics-friedmann-equations
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