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The mass of a hurricane will deform space in the directions at both its periphery, as well as its inner core. Towards the centre of a mass (or a extended mass) the magnitude of acceleration due to gravity (ADG) is misunderstood. ADG is much stronger than previously believed.
Gravity is the cause of a cloud system weakly begins to rotate. Fast rising heat and varm air reinforces this process.
This also applies to weak low pressure systems, such as tornado breeding grounds, because these are also extended masses.
We know that huge low pressure systems, such as hurricanes, twist weaker low pressure systems around themselves, strengthening the hurricane. This is a unification process that works exactly the same way when it comes to much weaker low pressure systems.
Small weak low pressure systems will unite with each other, but the aforementioned effect complicates the process. The unification is only possible if a small low pressure system twists itself around a greater one. |
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The illustration shows two low pressure systems colliding together. |
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Many small low pressure systems, like heavy clouds, will aggregate. As this occurs weak winds will begin to form. Rising winds inside weak low pressure systems will slowly begin to rotate and rise similarly to winds in large low pressure systems. It is the combination between slowly upwards rising winds and strong winds at higher altitudes that dramatically begin to speed up the naturally rotating process of small low pressure system collisions. This is the birth of a tornado. Such a process can start a series of weak low pressure system collisions. This can transpire very quickly. |
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The turbulence of a tornado can cause several weak low pressure systems to collide simultaneously. This is why multiple funnels may form, and then suddenly disappear after the unification process is complete. |
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How could the Monticello tornado travel 160 km further than usual? Well it’s basically not that strange. As long as a low pressure system travels on a path rich in heavy clouds, and the area has strong upper winds, a tornado can continue. |
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Let’s consider what happens at higher altitudes. The basic cause of the vortex (horizontally rotating air in higher altitude) is therefore not the cause of a tornado but the result of vertically rotating air pushed being forced into a horizontal position. The overturned, horizontally rotating airstreams reinforce the already rotating air in the horizontal upper altitudes, but this itself is not enough to start a tornado. What happens in addition is, the upwards moving air from a tornado contributes to the upper air stream. The upper air stream delivers wind for the distant high pressure. This stream has a different "requirement" day by day with regard to how fast the wind, which is delivered, must be moving. When the requirement one day is huge, the upward weak rotating winds from a potential tornado area can be a very "welcome guest" to enter into the upper airstreams, and be nearly sucked upwards by the strong "delivery requirement" in the upper flowing air stream. A tornado is therefore a combination of more than one factor. This new theory implies that a better understanding of the force of gravity could be important for also better understanding of how and why small low pressure systems really act when air is moving upwards or when low pressures collides, - that is the point of this theory. |
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Like a Hurricane it seems that tornados also can have a 'sunny eye' - just very much smaller. |
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But gravity also play a role when how much smaller low pressures is created.
Many places in the world "hole in the sky" have been observer. The prevailing theory is; - those heavy ice crystals are falling down into the hole, - this part is probably correct. But the heavy ice crystals are not created by airplanes (if so the hole would not be round), these are also not created by sky's in higher altitude, (that also does not explain the round shape). The reel cause is slow upwards rotating air moving both upwards and towards centre of small weak low pressures, which mean towards the centre of a low pressure (most often towards a the centre of a big cloud) and at the same time rotating upwards. When slowly moving upwards air (in the centre of the low pressure) rises, the vapour (as the upwards rotating wind carries) crystallizes, and fall down (after a while), - the same way it came from (in the centre of the hole). The size of a low pressure determinate how strong role gravity plays. Gravity plays a weak but important role. More holes in the clouds : http://weathervortex.com/sky-holes.htm http://www.youtube.com/watch?v=9XvBYBOFKaM&feature=related http://www.youtube.com/watch?v=FXF9HSB627U&feature=fvw http://www.youtube.com/watch?v=91DngoT5Hi8&feature=related
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