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Why Does Light From the Center of the Sun Take Tens of Thousands of Years or More to Reach Its Surface?

Category: Space & Astronomy

Sunlight takes about eight minutes to reach Earth. That is the last, easy part of the trip. The harder part comes first: getting out of the Sun itself.

If light could fly straight from the Sun's center to its surface, it would take only about 2.3 seconds. Instead, the energy made there spends tens of thousands of years or more on the way out, and estimates run from about 30,000 years to millions. This note asks why, and why the sources do not agree on a single number.

The Sun's Light Starts as Mass That Disappears in the Core

The Sun's core reaches about 15 million °C (27 million °F), hot and dense enough for nuclear fusion. There, hydrogen atoms fuse into helium atoms and release a huge amount of energy [1].

The energy comes from a small loss of mass. A helium-4 nucleus has about 99.3 percent of the mass of the four protons that make it, so roughly 0.7 percent goes missing and turns into energy [2]. ESA's teaching material puts the whole Sun at 600 million tons of hydrogen becoming 596 million tons of helium every second, so about 4 million tons are released as energy [2]. Stanford's Solar Center gives about 5 million tons per second [3]. The two sources round differently, so a safe way to say it is “a few million tons every second.”

That energy leaves the fusion reactions as very high-energy light. So what stops it from simply shooting out?

Light Cannot Go Straight Because the Gas Around It Is Crowded

The answer is crowding. The Sun is not solid; it is a ball of hot gas made of charged particles, called plasma. The plasma gets denser toward the center, and the core is about ten times denser than lead, even though it is still a gas [1] [4].

In the layer just outside the core, called the radiative zone, a lecture from Ohio State University says a particle of light (a photon) can travel only about 1 centimeter before it runs into an atom. It then goes off in a random new direction [5]. A path made of many random turns is called a random walk.

Picture crossing a packed school hallway between classes. You aim for the far door, but every few steps someone bumps you and you end up facing another way. You still make progress, but a lot of your steps go sideways or backward. Inside the Sun, the energy meets an almost endless series of bumps. (A real photon is not one traveler: it can be absorbed and re-emitted, so it is better to think of energy being passed along from particle to particle [5].)

One neat comparison comes from the physicists who build neutrino detectors. Neutrinos are made in the same fusion reactions, but they barely interact with matter, so they cross the Sun in seconds. The light from the core takes at least several tens of thousands of years [6]. Same birthplace, very different trips. The delay is not because light is slow; it is because the energy takes a very indirect route.

A Random Walk Needs Far More Steps Than a Straight Walk, and That Is Why the Trip Is So Long

Here is the surprising part. The Ohio State lecture explains that if each step has length l, a random walk needs on average (d/l)² steps to get a distance d away. A straight walk would need only d/l steps [5].

The square matters. If your goal is twice as far away, a straight walk takes twice as many steps, but a random walk takes four times as many. For a goal as distant as the Sun's surface, with steps of only about a centimeter, the count becomes astronomical. The lecture states that it takes a photon about 30,000 years, on average, to random walk from the center to the surface [5], though the short page does not show the assumptions behind that number (more on this below).

Sources Disagree: The Trip Is Said to Take From About 30,000 Years to Millions

Different careful sources give different times:

  • Ohio State University: about 30,000 years from center to surface, under the stated 1 cm step assumption [5].
  • Max Planck Institute for Nuclear Physics: at least several tens of thousands of years [6].
  • NASA and ESA's SOHO classroom page: several hundred thousand years to reach the top of the radiative zone [4].
  • UCAR: it can take millions of years for energy to cross the radiative zone [1].

These are not all measuring the same thing, and none of them is a direct measurement. Nobody can send a marked photon into the Sun and wait. The numbers are estimates, and the answer depends on how far a photon gets between collisions at each depth, which changes as the gas thins toward the surface. A single “1 centimeter” step is a handy round number, not the whole story. A simple calculation of my own, with exactly 1 cm steps and the Sun's radius, gave something nearer 5,000 years than 30,000. I cannot tell from the short lecture page why the two differ, so please treat the 30,000-year figure as one estimate, not a settled value.

So the honest summary is a range, not a single number: from about 30,000 years up to millions, depending on the source and on which part of the trip is counted. It is worth being comfortable with a range here. It tells you which parts science knows well (the trip is extremely slow, and why) and which parts are estimates (exactly how slow).

On the Way Out, the Energy Changes From Invisible Light to Visible Light and Then Hitches a Ride on Moving Gas

The journey changes the energy. Temperatures fall as you go outward: about 15 million °C in the core, about 2 million °C at the top of the radiative zone, and about 5,700 °C at the top of the layer above it [1]. A lecture from UMass Amherst describes how, over many collisions, the high-energy light from the core gives up energy to the gas, so what arrives near the surface is mostly lower-energy visible light [7].

The method of carrying energy changes too. In the outer layer, the convective zone, the gas is cooler and gets in the way of light more. Ohio State's astronomy notes explain that convection works well in a fluid that is hard for light to get through: hot fluid rises, cooler fluid sinks, and this circulation carries the energy [8]. Think of a pot of soup on the stove with hot soup rising from the bottom. NASA's SOHO page says energy travels quickly through this outer layer [4]. So the slowest part of the trip is the crowded radiative zone.

You can see the top of this circulation on the Sun's surface. Telescope images show bright patches called granules, each about 1,000 kilometers across, with darker lanes between them. Hot plasma rises in the bright patches and cooler plasma sinks in the lanes [9].

Past the Surface, the Sun's Outer Atmosphere Is Even Hotter

The visible surface, where light finally escapes into space, is at about 5,800 K (roughly 5,500 °C or 10,000 °F) [4]. You might expect it to get cooler as you move away, like walking away from a campfire. Instead, the corona, the Sun's thin outer atmosphere, is about 2 million K [4]. This note does not go into why, but it is a good question to take to the original sources.

Try It at Home: Flip a Coin to See How Far a Random Walk Goes

You can test the “square” idea with a coin and a pencil. No Sun involved.

  1. Draw a number line on paper from −30 to 30 and put a marker on 0.
  2. Flip the coin. Heads, move one step right. Tails, move one step left.
  3. Do this 100 times, then note how far you ended up from 0.
  4. Repeat a few times. Walking straight, you would be 100 steps away. Most random walks of 100 steps end up around 10 steps away. To get 20 steps away, you would typically need about 400 flips.

That is the square at work: twice as far means about four times as many steps. Now imagine the Sun's photons making an unimaginably larger number of steps.

Never look at the Sun to explore this topic. Use these pages, pictures from space telescopes, and your own paper-and-coin game instead. If you want to read the originals, start with the SOHO classroom page and the UCAR page on the Sun's interior; both are written for general readers.

Sources

I read these pages through a fetch tool that returns the passages matching my questions, so I quote only figures and wordings it returned, and I did not read the full text of every page. The Ohio State lecture and the SOHO, UCAR and Max Planck pages gave the different trip times; I list the range rather than choosing one. The UMass Amherst lecture and the photosphere details were taken from material checked for the Japanese edition of this note, not re-fetched for this version. The comparison with a school hallway, the soup pot, my own 5,000-year check, and the coin game are mine, not from the sources.

  1. UCAR Center for Science Education, “Inside the Sun.” https://scied.ucar.edu/learning-zone/sun-space-weather/inside-sun (core temperature and density, fusion, radiative zone, “millions of years,” temperatures at layer tops)
  2. ESA Science Portal, “Stellar Processes and Evolution - Educational Support.” https://sci.esa.int/web/education/-/36828-stellar-processes-and-evolution (99.3 percent mass, 600 to 596 million tons per second)
  3. Stanford SOLAR Center, “Ask A Solar Physicist.” https://solar-center.stanford.edu/FAQ/Qfusion.html (about 5 million tons per second)
  4. NASA/ESA SOHO, “Our Star the Sun.” https://soho.nascom.nasa.gov/classroom/sun101.html (plasma density, several hundred thousand years, fast convective zone, surface 5,800 K, corona 2 million K)
  5. Ohio State University, A162 Lecture 7. https://www.astronomy.ohio-state.edu/weinberg.21/Intro/lec7.html (2.3 seconds, 1 cm steps, (d/l)², 30,000 years)
  6. Max Planck Institute for Nuclear Physics, “Research: BOREXINO.” https://www.mpi-hd.mpg.de/lin/research_bx.en.html (neutrinos cross in seconds, photons at least several 10,000 years)
  7. UMass Amherst, “The Sun and Stellar Structure.” https://people.umass.edu/wqd/strobel/starsun/strsunb.htm (gamma rays to visible light; summary only, not re-read for this version)
  8. Ohio State University, “Lecture 3: Inside the Sun.” https://www.astronomy.ohio-state.edu/ryden.1/ast162_1/notes3.html (convection works well in fluids opaque to light; summary only, not re-read for this version)
  9. NCAR High Altitude Observatory, “Solar Convection and Mean Flows.” https://www2.hao.ucar.edu/hao-science/science-topic/solar-convection-and-mean-flows-lsv (granules about 1,000 km, rising and sinking plasma)

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