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Wheelspins are a real masterstroke in the Forza Horizon formula. Where the racing games of old would simply give you a fixed number of credits after each event, wheelspins turn the whole endeavour into an automotive gameshow where every chequered flag is a chance to either win big or curse the gods as the needle lands agonising inches away from giving you a Koenigsegg.
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This is the simplest method: a straightforward transaction in the Forzathon Shop. This would allow scientists to study the far-side of a black hole and actually see its shadow in space.
Since the size and shape of this shadow depends on the mass and spin of black hole, these observations could tell us much about how space and time are warped in this extreme environment.
Calculations indicate a resolution of 50 micro-arcseconds approximately 2, times finer than the Hubble Space Telescope is needed to image the shadow effect.
This amazing high-resolution imaging is within the reach of the ALMA-enabled Event Horizon Telescope. Obtaining an image of a black hole is not as easy as snapping a photo with an ordinary camera.
To capture its image, amazingly high resolution is needed. By combining the data collected by antennas thousands of kilometers apart, VLBI achieves a resolution equivalent to a radio telescope several thousands of kilometers in diameter.
However, VLBI also has a lot of large blank areas that are not covered by any of the antennas. These missing parts make it difficult for VLBI to reproduce a high-fidelity image of a target object from the synthesized data.
This is a common problem for all radio interferometers, including ALMA, but it can be more serious in VLBI where the antennas are located very far apart.
It might be natural to think that a higher resolution means a higher image quality, as is the case with an ordinary digital camera, but in radio observations the resolution and image quality are quite different things.
The resolution of a telescope determines how close two objects can be to each other and yet still be resolved as separate objects, while the image quality defines the fidelity in reproducing the image of the structure of the observed object.
For example, imagine a leaf, which has a variety of veins. The resolution is the ability to see thinner vein patterns, while the image quality is the ability to capture the overall spread of the leaf.
Researchers have been studying data processing methods to improve image quality for almost as long as the history of the radio interferometer itself, so there are some established methods that are already widely used, while others are still in an experimental phase.
The observations with the EHT and the GMVA were completed in April The data collected by the antennas around the world has been sent to the United States and Germany, where data processing will be conducted with dedicated data-processing computers called correlators.
The data from the South Pole Telescope, one of the participating telescopes in the EHT, will arrive at the end of , and then data calibration and data synthesis will begin in order to produce an image, if possible.
This process might take several months to achieve the goal of obtaining the first image of a black hole, which is eagerly awaited by black hole researchers and the general astronomical community worldwide.
This lengthy time span between observations and results is normal in astronomy, as the reduction and analysis of the data is a careful, time-consuming process.
Right now, all we can do is wait patiently for success to come — for a long-held dream of astronomers to be transformed into a reality.
ALMA was designed to work as an interferometer — a telescope made up of many individual elements. This common acceleration on the surface of the Earth is the acceleration due to gravity, which is 9.
Isaac Newton realized that there was a force acting to keep objects against the surface of the Earth, and it was directly related to the mass of the Earth.
The larger the mass an object had, the more its gravitational force would be. Using this mathematically relationship, Newton proposed that the 9.
Density is the how compact a substance is and is measured relative to another substance, such as water. In other words, density is how well a substance or object floats or sinks.
Volume is the cubic dimensions or space that an object takes up. Isaac Newton did not know the value of Big G the gravitational constant , but knew that it was a tiny number, since the mass and radius of the Earth were very large numbers, and the result of the equation had to equal 9.
One way to determine Big G was to determine the density, volume and radius of the Earth. We can solve for Big G using this formula,.
However, he is less well known for his hypothesis that the Earth was hollow on the inside. During the late s and early s, scientists debated what the density of Earth was.
Newton suggested an average density about 5 times more than water , while Halley suggested an average density less than water for the interior of the Earth.
The problem was no one knew the value of Big G. During the next century there was much discussion on the density of the Earth the value for D.
Expeditions into caverns and dark caves around the world were trying to find an entrance to the hollow center of the Earth.
This debate captured the interest of a little short man named John Michell , who was the head of a church in Yorkshire, England , but dabbled in science in his spare time, and often wrote to fellow scientists of the day, including Benjamin Franklin.
In his spare time, he thought of an experiment to measure Big G, by using a set of big very dense lead balls placed in close proximity to a set of smaller, but also very dense lead balls suspended from a string tied to a balancing rod.
When the large lead balls are placed next to the smaller lead balls, the force of gravity will attract the two balls to each other. This attraction causes the balancing rod to shift slightly.
To measure this movement or change in the balancing rods angle, a light was reflected off a mirror set on top of the balancing rod. Henry suffered from what would be called autism today, as he was incredible shy, and struggled to carry on conversations with anyone not his close friend.
Then at the age of 68, John Michell died, and left his experiment to Henry Cavendish to complete. In a large building, Henry reconstructed the experiment with the lead balls near his home, and calculated an accurate measure of Big G, the gravitational constant, which is 6.
As well as the gravitational forces acting to hold astrological objects in orbit with each other. Furthermore, it explains why large objects in the universe take on spherical shapes around the center of mass.
They are held against the Earth by its gravitational force. The length of the day is the time the Earth rotates once, with each longitude facing the sun once and only once during this daily rotation.
Today the Earth takes 23 hours, 56 minutes and 4. Of course, the amount of daylight and night varies depending on your location and time of year, because the Earth rotates around a polar axis that is tilted at This is why people in Alaska at a higher latitude experience longer daylight during the month of July, and longer darkness during the month of December, than someone living near the Equator.
Measuring the length of each rotation of the Earth requires clicking a very accurate stopwatch each day, and recording the time it takes for Earth to make one rotation.
For the most part it says pretty close to 23 hours, 56 minutes and 4. However, the length does fluctuate by about 4 to 5 milliseconds.
In other words, 0. These fluctuations appear to be on a decadal cycle, so the days in the s were shorter by 0.
Weaker fluctuations occur over a yearly cycle, with days in June, July and August shorter by 0. In fact, the Earth is not just a solid mass of rock, we have a liquid ocean and a gaseous atmosphere that impacts the length of each day.
It is like you are on a washing machine spinning around with wet clothes, and depending on where those clothes are in each spin cycle, there will be some variation in the speed of the spin itself.
Climate change also can have a rather important impact on the length of the day. If we were to compare the average day length during the last glacial period 25, years ago to today, the day would be shorter.
This change in inertia is the same phenomenon you observe when an ice skater brings his or hers arms out during a spin.
The speed of the spin slows down. While these fluctuations are interesting, they are small several milliseconds , but we are interested in finding out when the Earth will stop spinning, and for that question we need a much longer record of day lengths, going back millions of years.
Fossil corals that live in the inter-tidal zone of the ocean are subjected to twice daily tides caused by the rotation of the Earth and gravitational pull of the moon, and amplified by the relative location of the sun.
These changes in water depth result in a record in the growth rings, as well as cyclic sediments such as tidal rhythmites and banded iron formations.
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