Author: 一毫秒的永恒

A few decades ago, astronomers could only dream of glimpsing the Moon's other side. This is a NASA visualization. | Credit: NASA's Scientific Visualization Studio

  Look up at the bright Moon and it seems as familiar as ever, no different from the Moon of the past. Indeed, the Moon you admire is the same one our ancestors admired. After sunset, people around the world can see the same familiar shadows and shapes. It is easy to understand why ancient poets used the Moon to express longing for home and family.

  From ancient times until the modern era, people on Earth could see only the Moon’s “near side.” Humanity did not see the “far side” until 1959, when the Soviet Luna 3 spacecraft flew around the Moon and returned photographs.

In 1959, the Soviet Luna 3 probe took the first photograph of the Moon's far side. | Credit: NASA's Scientific Visualization Studio

  This happens because of tidal locking. The Moon is close enough to Earth that Earth’s gravitational pull is not identical across all parts of it, producing a pronounced tidal effect that increases rapidly as the distance decreases. The effect raises tidal bulges on the Moon. Earth’s gravity exerts a torque on those bulges, gradually slowing the Moon’s rotation until its rotation period equals its orbital period around Earth, about 27.3 days. Once the effect of libration is set aside, the same lunar hemisphere therefore always faces Earth. This does not mean that the Moon fails to rotate. On the contrary, it happens precisely because the Moon’s rotation and orbital periods are equal.

Tidal locking makes a satellite's rotation period roughly equal to its orbital period around a planet. Ignoring libration, the Moon behaves as shown on the left, always presenting the same side to Earth. The diagram is a view from above the Moon's rotation axis and is not to scale. If the Moon did not rotate, it would behave as shown on the right, alternately presenting its near and far sides to Earth as it orbited.
If the rotation frequency exceeds the orbital frequency, a small opposing torque arises and eventually produces frequency locking, shown in green.

  The side of the Moon facing Earth has been studied extensively. We can see it; Apollo astronauts landed on the near side so that they could communicate with the National Aeronautics and Space Administration (NASA) on Earth; and every sample returned by the Apollo missions came from the near side.

  Modern satellites, however, have allowed astronomers to map the entire lunar surface. On January 3, 2019, China’s Chang’e 4 probe successfully landed and began exploring the Von Kármán crater in the South Pole–Aitken basin on the far side. It was the first human-made probe to make a soft landing there. Chang’e 4 helps answer questions about the crater’s surface features and has conducted numerous tests on lunar soil, including whether organisms could grow in it.

  What is distinctive about the far side, so distant from human civilization? That distance makes it a genuine radio-quiet zone. The Moon shields it from radio interference produced on Earth, allowing researchers to measure faint signals from the Universe without their being drowned out by electromagnetic noise. Chang’e 4, for example, can observe low-frequency radio signals from the Sun and other celestial objects. Human activity, including television, radio broadcasts, and other communication signals, makes those frequencies impossible to detect from Earth. Low-frequency radio observations can reveal the earliest stars and black holes in the Universe, giving astronomers a deeper understanding of how cosmic structure formed. Chang’e 4 can also conduct lunar-based low-frequency radio astronomy, survey the terrain of its far-side exploration zone, and study its mineral composition, among other investigations of the far side.

  Scientists are now preparing for future space travel. A range of lunar probes have surveyed different aspects of the Moon and searched for resources that could help humans reach Mars. Water found in 2009 by NASA’s LCROSS satellite in permanently shadowed regions at the lunar south pole, for example, could be split into hydrogen and oxygen for fuel and breathing.

  Researchers are also actively exploring polar craters on the Moon. Some of these craters never see daylight and are known as permanently shadowed regions. They are deep and positioned where sunlight never reaches them. The Moon does have places that remain forever dark, but the entire far side is not a “dark side.”

References

  1. https://www.livescience.com/65321-whats-on-far-side-of-moon.html
  2. https://www.knowpia.cn/pages/潮汐锁定
  3. https://www.knowpia.cn/pages/月球背面