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courses:ast100:4 [2024/12/14 02:21] – [4. Detecting Planets] asad | courses:ast100:4 [2024/12/14 09:41] (current) – [4. Detecting Planets] asad | ||
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+ | ==== Saturn' | ||
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+ | **Hermes:** Galileo first observed these rings with a telescope, but it was Huygens from the Netherlands who first understood that they were indeed rings. From here, it’s clear that these rings are not continuous disks but rather a collection of countless ice particles ranging from a few centimeters to several meters in size. Besides water, many of these particles also contain various carbon compounds. These rings extend from about 30,000 km above Saturn’s surface to nearly 150,000 km. Despite a diameter of 300,000 km, the thickness of these massive rings ranges from about 10 meters to a maximum of a few hundred meters. The A, B, C, D, and F rings can be seen here, and the gaps between the rings are named after different scientists. For instance, the gap between the A and B rings is called the Cassini Division and the Huygens Gap; between the B and C rings is the Coulomb Gap, and between the C and D rings is the Maxwell Gap. Maxwell, the founder of electromagnetic theory, was the first to understand that Saturn’s rings are not a single disk but rather a collection of countless small objects. | ||
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+ | **Hermes:** If a moon or asteroid comes too close to a planet, the planet’s gravitational force pulls the near side of the object more strongly than the far side, as gravity decreases with distance. This results in the object being stretched and eventually torn apart into fragments due to the gravitational pull. These fragments then form a ring around the planet. Saturn’s rings were formed in this way. Moreover, if you observe closely, you will see small rocky fragments, about 10–20 km in size, scattered in certain places within the rings. These are called moonlets. Due to these moonlets, spiral structures, similar to spiral galaxies, form within Saturn’s rings. Saturn’s rings and its 62 moons can be compared on one hand to an entire solar system and on the other hand to a spiral galaxy like the Milky Way, with the spiral patterns of the rings resembling those of a galaxy. | ||
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+ | **Hermes:** Why not? Because of the gravity of these moonlets in Saturn’s rings, small waves sometimes form in the ocean of the rings. Waves spread evenly outward from a moonlet. However, since the inner rings of Saturn rotate faster than the outer rings, the inward-moving waves outpace the outward-moving waves. The perfectly circular wave (technically called a __density wave__) becomes spiral due to this uneven velocity, just as a circular ring can be twisted into a spiral pattern. In the case of galaxies, replace the moonlets with nebulas and stars, and replace the ocean of rings with the gases and stars of a galaxy. Since the velocity of stars and gas in galaxies also decreases with distance, the density waves created within galaxies similarly give them their spiral shape. | ||
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===== - Earth ===== | ===== - Earth ===== | ||
**Hermes:** If you understand how auroras form on Earth, you’ll understand Saturn’s as well. The solar system is now about 1 billion years old. If we travel from Saturn to Earth, we can see how auroras formed near Earth’s poles even 3.6 billion years before the emergence of humans. | **Hermes:** If you understand how auroras form on Earth, you’ll understand Saturn’s as well. The solar system is now about 1 billion years old. If we travel from Saturn to Earth, we can see how auroras formed near Earth’s poles even 3.6 billion years before the emergence of humans. | ||
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- | ===== - Classification of Planets ===== | + | ===== - Classification of Planets ===== |
- | {{: | + | **Hermes:** Exactly. From size, we can derive volume, and dividing mass by volume gives density. This figure shows the radius of all discovered planets plotted against their mass. The x-axis represents planetary mass relative to Earth, while the y-axis represents planetary radius relative to Earth. Each bubble represents a planet, and the color of the bubble indicates the discovery method. |
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+ | **Hermes:** Yes. A planet on the lower diagonal line has the same density as Earth, meaning its mass per cubic centimeter is 5 grams. Planets on the upper diagonal line have the same density as Saturn, about 0.7 grams per cubic centimeter. Planets between these lines have densities between Earth and Saturn. Planets below the lower line are denser than Earth, and those above the upper line are less dense than Saturn. The discovery methods are also shown here. | ||
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+ | **Hermes:** Not all methods need to be discussed for now. | ||
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+ | **Hermes:** Life is short, and watching rhinos in the Kaziranga National Park along the banks of the Brahmaputra is much more enjoyable than endless study. Look, two rhinos bathing over there. | ||
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+ | **Hermes:** Since we’ve already discussed the classification of galaxies and stars, it’s only fair to talk about planetary classification too. In this scatter plot, the y-axis again shows planetary radius, but the x-axis now shows orbital period instead of mass, meaning the time a planet takes to orbit its star. | ||
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+ | **Hermes:** A planet’s equilibrium temperature is the temperature it would have if it emitted as much energy as it receives from its star. This may differ from its actual surface temperature. For example, Earth’s average surface temperature is 15°C, but its equilibrium temperature is -18°C. The actual temperature is higher because some reflected energy is retained in Earth’s atmosphere due to the greenhouse effect. In this plot, you can see that planets with shorter orbital periods are closer to their stars and thus have higher temperatures (more red-colored bubbles). Those with longer periods are farther from their stars and cooler (more blue-colored bubbles). Kepler discovered the relationship between period and distance 400 years ago, and we met him during the Stellar Age. | ||
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+ | **Hermes:** The black diamond icon represents Earth, with a period of 365 days. Planets with very short periods (1–10 days) are extremely hot, potentially lava worlds (if rocky like Earth), ocean worlds (covered in water), or hot Jupiters (gaseous like Jupiter). On the other hand, planets with very low temperatures are cold gas giants or ice giants. | ||
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+ | **Hermes:** Planets at least twice the size of Earth but smaller than Neptune are commonly called super-Earths. These range from molten-hot to ice-cold worlds. One well-known super-Earth, | ||
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courses/ast100/4.1734168087.txt.gz · Last modified: 2024/12/14 02:21 by asad