The Slingshot Maneuver

For any of you who have seen the movie adaption of, “A Wrinkle In Time” may remember the scene where two of the protagonists hide in a tree stump in order to be thrown over a wall.

Meg, one of these protagonists, has parents who work in quantum theory, so she has picked up knowledge in physics throughout the years at home. She was the one who directed her friend to hide in the tree stump because she knew that the tornado was giving speed to objects that fell into it, calling it, “The Slingshot Maneuver”.

From the very first time I watched this film and learned of this trick, it immediately seemed like a physical conundrum: how something can escape an attractive entity with more speed than it entered with. It actually wasn’t until tonight that I fully grasped the concept with the help of some articles and Neil DeGrasse Tyson.

I found the graphics online of the gravitational slingshot to be rather ambiguous and misleading. The following one, however, is an exception. So as I explain the mechanics operating behind the curtains of the “slingshot maneuver “or “gravity assists” as I’ll be referring to them from this point foward, reference the diagram I’ve embedded below:

So gravity assists have actually been somewhat of a popular yet unsung hero of space travel and research. In this article from NASA, you can read about how space probes have historically made use of multiple during their treks to the exterior solar system for their practically free acceleration.

But how does a body falling into a planet gain speed? Even if said object is later able to escape the heart of the planet’s gravitational pull, all of that energy gained while advancing toward it will be stripped from the body upon departure.

The conservation of energy does still hold during this process, so it is very correct to assert that there is no net change in speed of the probe. But you’re forgetting that this is not the only motion at play in these conditions— planets revolve around the sun.

In order for the planet to have its gravitational influence, the probe has to catch up to its speed, relative to the sun (we use the Sun as a rest frame, since compared it doesn’t have motion like the satellites of our solar system). If the probe weren’t able to match the planet’s speed, it would gain too much distance from the planet for a gravity assist to take place.

So in approaching the planet from behind (remember this detail) the probe gains the velocity of the planet. And through doing this, it saps some of the planet’s angular momentum, although the effects of this are negligible since the planet is immense in mass.

And while the planet will continue in its elliptical path of orbit, the probe will not; it will continue in the same direction it was moving with the planet when it matched its speed. If you look at the diagram above, the path of the prove moves in an overall hyperbolic fashion with the eccentricity increasing or decreasing contingent on the angle in which the probe enters in reference to the planet’s direction of motion.

And it is through this minor purloin of momentum that our exploratory satellites reach speeds and distances in space that were never even thinkable prior.

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Roche Limit

In science fiction novels and movies, we occasionally see a planet or a moon being teared into pieces due to it being to close to a star or a larger planet. In the newly premiered Chinese sci-fi movie The Wandering Earth II, our moon potentially gets torn into chunks as it moves closer to the Earth and passes its Roche limit. You might wonder, what exactly is this limit and why would it tear objects apart?

We know that tidal forces exist due to the differences in gravity on the near and far sides of a planet or a satellite. We also know that tidal forces become more extreme as an object gets closer to the source of the tidal effect (due to the object’s radius occupying a larger portion of the distance between the object and the source). The Roche limit, first calculated by French astronomer Édouard Roche, is the distance to a (larger) celestial body when an approaching (smaller) celestial body disintegrates due to extreme tidal effects that exceed the self-gravity that holds the smaller object together.

Visual demonstration of the Roche limit

A completely rigid object would maintain its shape up to the point of the Roche limit, while a more fluid object will tend to get elongated due to tidal forces as it approaches its Roche limit, and this elongation further increases the tidal effects and rips the object apart. The Roche limit depends on the ratio of the density (or mass) of the two objects, and the calculation of this limit for rigid bodies is shown below.

One example of a celestial body being torn apart in the Solar System is the comet Shoemaker-Levy 9, which unfortunately traveled too close to Jupiter, got past its Roche limit, and was broken into over 20 pieces and eventually bombarded the cloudy surface of Jupiter (See figure below).

Comet Shoemaker-Levy 9 in July 1994

Within the Roche limit of a planet, chunks of rock and ice will not tend to coalesce to form moons, which is why rings of planets generally lie within this radius, as asteroids and moons that enter this radius disintegrate into small pieces. In contrast, larger moons of planets generally orbit beyond this radius to stay in one piece.

There are several exceptions, though. Saturn’s moon Pan, a ring shepherd in Saturn’s Encke division, and Jupiter’s moons Metis and Adrastea all lie within their Roche limits, since forces other than their self-gravity holds themselves together. Another exception is the minor planet 50000 Quaoar in the Kuiper Belt which has a ring far beyond its Roche limit. Astronomers are still investigating why Quaoar’s ring did not amalgamate into a satellite.

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Celestial Navigation Techniques Blog #2

Before any GPS or easy to use maps, explorers were completely reliant on the stars and their hunches to determine their location during their travels. In the Northern Hemisphere, it was much easier to determine latitude because of the conveniently located star Polaris just above the northern celestial pole. Using the Sun is also a possibility for navigation, but more precise measurements of dates and the path of the ecliptic are required for an accurate determination. Navigators have used tools like the sextant featured above since at least the 1700s in order to measure precisely their position in the oceans. The Ancient Greeks created similar items like the astrolabe which was very important and useful with hundreds of different astronomical uses varying from navigation to timekeeping. In modern times, global positioning systems have satellites orbiting the Earth act as “artificial stars” which are able to accurately send radio signals to travelers below.

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Blog2: Telescopes of all kinds

picture from iStock

There are many different types of telescopes, each designed for a specific purpose. Here are some of the most common types:

  1. Refracting Telescope: This type of telescope uses lenses to refract (bend) light and form an image. They are often called “refractors” and are easily recognized by their long, narrow tubes.
  2. Reflecting Telescope: This type of telescope uses mirrors to reflect light and form an image. They are often called “reflectors” and are usually shorter and wider than refractors.
  3. Catadioptric Telescope: This type of telescope combines elements of both refracting and reflecting telescopes, using lenses and mirrors to form an image. They are often more compact than other types of telescopes and are popular for both amateur and professional astronomers.
  4. Radio Telescope: This type of telescope is specifically designed to detect radio waves from space. They are often much larger than optical telescopes and come in a variety of shapes and sizes, including dish-shaped and cylindrical.
  5. Space Telescope: This type of telescope is placed in orbit around the Earth and is used to observe the universe in different parts of the electromagnetic spectrum. The Hubble Space Telescope is one of the most well-known space telescopes.
  6. Solar Telescope: This type of telescope is specifically designed to observe the Sun. They typically use special filters to block out the Sun’s bright light and allow safe observation.
  7. Interferometric Telescope: This type of telescope uses multiple smaller telescopes working together as an array to simulate a larger telescope. They can provide high-resolution images and are commonly used in radio astronomy.

Conclusion

Each type of telescope has its own strengths and weaknesses, and the choice of which one to use depends on the specific observing goals and requirements of the astronomer.

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Blog 2: Retrograde Motion

Due to Earth’s counterclockwise rotation, many objects in the sky like the Sun rise in the east and set in the west. However, planets such as Mars exhibit apparent retrograde motion, where they appear to reverse direction in the sky and move from west to east. This is a result of planets orbitting at different speeds than Earth and thus, Earth passes or is passed by these planets during its orbit. The ancient Greeks noticed this retrograde motion but rejected the possibility of Eart rotating the Sun since they didn’t believe the stars could be far enough to not detect stellar paralax. Instead, figures such as Aristotle developed complex motions for planets that involve an extra loop accounting for retrograde motion. After the Copernician model of the solar system, retrograd motion no longer remained a mystery.

Retrograde Motion

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Retrograde motion

Retrograde motion is one of the apparent motions of planets relative to the background of the stars. If we continue to track a certain planet for a period of time, we will find that it sometimes moves to the east, sometimes stops for a short time, sometimes moves to the west, then makes a short stay, and then moves to the east as it did at the beginning. In order to explain this phenomenon, the epicycle-deferent model was born. This geocentric model dominated for two thousand years until Kepler’s three laws were proposed.

So, what causes the retrograde motion of the planets? Actually, they are not really retrograde. The earth is closer to the sun than many planets, so the earth moves faster. Whenever Earth overtakes a planet, the outer planets appear to start receding in the sky. From Earth, Mercury and Venus appear to oscillate on either side of the Sun. These planets all do circular motion around the sun, it’s just that here on Earth, it looks like the planets are going backwards.

source

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Nuances of Thermal Energy

A picture of a hot scary oven

Today I learned about the nuances of thermal energy that answered a forgotten question from my childhood. When I was little I was always afraid to stick my hand inside a hot oven because I knew how badly my tongue gets burned whenever I drink something hot. However, when I finally did stick my hand inside a hot oven for a few seconds, it turns out that it didn’t burn me as much as I thought, and I briefly wondered why. Now, ten years later, I know that even though the temperature looks really high (about 450 degrees Fahrenheit), what really determines whether something is hot or cold is thermal energy. Thermal energy depends not only on temperature, but also the number and density of particles. So the reason why the air didn’t burn as much as the water did is because air is less dense than water, drinking the water meant many more molecules struck my tongue each second, and more thermal energy was transferred.

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The polarization of light

Light waves travel through electric and magnetic fields that vibrate perpendicular from each other. As an electromagnetic wave, like all waves, light’s vibration has a direction along with its frequency and wavelength. We often imagine waves moving up and down vertically, like a wave on the shore, but this is not always the case. Specifically, the polarization of an electromagnetic wave is the orientation of vibration of the electric field.

You may own sunglasses that mitigate glare, which is often caused by light with a horizontal polarization reflected off of a horizontal surface. This type of sunglasses contains a polarizer, which absorbs incoming light that vibrates horizontally and transmits vertical light.

In 2019, the Event Horizon Telescope captured the first ever photo of a black hole. The same black hole, centered in the Messier 87 galaxy some 50 million light-years away, was captured again in 2021 with polarimetric imaging tools that recovered and visualized the light’s polarization. This new perspective allows astronomers to measure how magnetic fields influence matter near the event horizon of the black hole. While the original photo depicts the brightness of the surrounding light, the second depicts its direction.

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Post 2

Astronomy is a science. This means that in astronomy we make predictions, test hypotheses, and use findings to continuously build and refine our theories. Interestingly, astronomy was very likely the first science. Humans, ever since the ancient civilizations, have looked to the sky and pondered its mysteries.

What use would such people have in astronomical science? Consider the importance of keeping time. Keeping time has a broader goal than being able to tell what hour of the day it is. Time is important for farmers and their crops—the changing of the seasons dictates what can grow. Time is also important for religious holidays that must fall at the same time each year. Time is also important for further astronomical observations, and we see it as a variable in many relevant equations.

Here is a photo of an ancient Egyptian sundial, used to keep time. It is taken from Wikipedia.

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” Exploring the Wacky World of Ocean Tides”

Tides are definitely one of the most mesmerizing phenomena in the world. The tides are the rise and fall of the sea level caused by the gravitational pull of the Moon and the Sun. The Moon has a strong gravitational pull that causes tidal ocean currents while the sun’s pull is way weaker because it is farther away.

An interesting fact about tides is that they can affect and play a role in the movement of some objects in our solar system. For example, a recent study showed that the tides on Jupiter’s largest moon, Ganymede, generate a good amount of heat, which contributes to its overall internal warmth. Tide could show us that there might be life outside Earth. For example, the observed tides on the Saturnian moon, Enceladus, shows that hat geyser-like jets spew water vapor and ice particles from an underground ocean beneath the icy crust of Enceladus. So this made it a promising object to study creating hope for a possibility of extraterrestrial life.

Enceladus: Ocean Moon

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