Rebirth of the Godly Prodigal - Chapter 719

[Chapter 649: A powerful sneeze]

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When Lucifer was bored this morning, he touched his chin and thought: “By the way, this thing is really magical. Where did the storm curse I sent go? Why? No one is alive but no corpse… No, I searched all the people in the kingdom who may be enemies of Hong Dali and found no one who was hit by the storm. Or is this curse invalid? The power of the curse has lost its effect? It doesn’t seem like it… Could it be that something strange happened to Hong Dali? Well, it’s possible. This Hong Dali is really magical…”

… …

“Sneeze,” Hong Dali, who was on the deck of the Big Fish, sneezed fiercely and touched his nose: “Who is talking about me?” He said and sneezed again: “Sneeze, a hundred Years old! Grandma, the weather is quite warm, why do you keep sneezing…”

…

The butterfly effect, also called topological chain reaction, refers to the small changes in the initial conditions in a dynamic system. A huge long-term chain reaction for the entire system. This is a chaotic phenomenon. There are fixed numbers and variables in the development of anything. There are rules to follow in the development trajectory of things. At the same time, there are also unpredictable “variables”. A small change can affect the development of things, which shows that the development of things is complex.

And this is the magic of nature…

After Hong Dali finished sneezing twice, he entered the Big Fish’s island to sleep with Li Nianwei without a care (don’t think wrongly, he was looking for his thighs…), but His two sneezes were extraordinary…

At this time, the Big Fish was traveling on the route to the Bermuda Triangle, which was already in the tropical ocean. On the sea surface, there are often many weak tropical vortices. In professional terms, these are the “embryos” of typhoons. Because typhoons always develop from this weak tropical vortex.

Actually, it was nothing. But the problem is, Hong Dali sneezed twice…

right on the sea around his Big Fish. It is vast enough here, and it is a tropical ocean. The surface temperature of the sea water is higher than 26.5C, and it is in a layer of sea water 60 meters deep. The water temperature has exceeded this value. The vast ocean surface is a necessary natural environment for the formation of typhoons. Because of the friction between air molecules inside the typhoon, an average of 3100-4000 calories/cm**2 of energy is consumed every day. This huge energy can only be released by the vast tropical ocean. Only latent heat can be supplied. In addition, the strong winds swirling around a tropical cyclone can cause the sea water near the center to churn. In the typhoon center where the air pressure drops very low, it can even cause the ocean surface to surge upward. Then it spread out in all directions, so the sea water billowed from the center of the typhoon to the surrounding areas.

Originally, such an environment was only likely to form a typhoon, but not necessarily a typhoon.

before the typhoon forms. It requires an initial disturbance, just like a spring oscillator. It will not vibrate without a disturbance.

And Hong Dali’s two sneezes were exactly this initial disturbance!

First, there is a very weak tropical vortex around the Big Fish.

We know that the operation of any machine consumes energy, which requires an energy source. A typhoon is also a “heat engine”. It rotates at such a huge scale and speed and consumes a lot of energy, so it needs an energy source.

The air blown out by Hong Dali’s two sneezes merged with the very weak tropical vortex, making the very weak tropical vortex a little bit stronger, and began to move very, very slowly.

In this tropical vortex, the air pressure itself is lower than the surroundings. After Hong Dali’s two sneezes merged in, the vortex moved and the air pressure gradually became lower. The surrounding air carried a large amount of water vapor and flowed to the center of the vortex, and An upward movement occurs in the vortex area; the moist air rises and the water vapor condenses, releasing huge latent heat of condensation, which begins to make the big machine of the typhoon run.

When the Big Fish aircraft carrier advanced more than ten nautical miles, the tropical vortex affected by Hong Dali’s two sneezes had initially formed a certain size – about twenty centimeters in diameter.

To say that the diameter of more than 20 centimeters is actually smaller than a hair on the top of a person’s head on the vast sea, but we know that things are developing – this happens to be a tropical ocean, The water temperature is very, very suitable. The high temperature and high humidity of the tropical ocean supplies water vapor. The air rises strongly, causing condensation and releasing latent heat. A typhoon has begun to form.

But just like this, this small vortex is not enough to cause any harm. It is likely that if it encounters the slightest interference, it will disappear into the sea forever.

But the real problem is that at this time, coincidentally, a gust of sea breeze happened to blow by, which caused a more violent reaction – the sea breeze merged into the vortex, and the low temperature brought by the sea breeze increased even more Due to the temperature difference in the vortex, this small tropical vortex became more and more spectacular – from a diameter of about twenty centimeters to about one meter in a short time.

At this time, this small tropical vortex moved faster and faster. About an hour later, it happened to move to a latitude that was very suitable for the formation of typhoons. The formation of typhoons requires certain conditions. If the earth’s rotational deflection force is large enough, the geostrophic deflection force at the equator is zero and gradually increases toward the poles. Therefore, the location of the typhoon is approximately 5 or more latitudes away from the equator. This tropical vortex is just at this latitude.

Due to the rotation of the Earth, a force is produced that changes the direction of the air flow, which is called the “Earth’s rotation deflection force.” When the tropical vortex moves here, the earth’s rotation makes it difficult for the surrounding air to flow directly into the low pressure, but instead rotates counterclockwise along the center of the low pressure.

At this time, this small tropical cyclone had grown a little bigger, reaching a diameter of more than two meters.

At this time, it still looks so small, just like a small seed that is slowly sprouting and growing.

Inside this small tropical vortex, just above the weak low pressure, the difference in wind direction and speed between high and low altitudes gradually decreases, and soon the upper and lower air columns act in unison, causing rapid accumulation of heat in the upper air, thereby increasing the temperature.

As the ambient airflow above the friction layer flows along the isobars, the upper-level warming effect is further completed. This small tropical vortex grows rapidly and becomes larger, and soon the diameter increases to three, four, or five meters. Meters…

If it is only on this scale, it is obvious that it is not enough.

But the problem is that after a day of sunshine, strong cumulonimbus clouds have formed on the sea surface here.

That small tropical cyclone passed by and brought a lot of cold air due to the wind speed. At this time, the hot air in these cumulonimbus clouds on the sea surface rises, and the surrounding cooler air continuously replenishes it. When it is heated, it rises again. This cycle quickly makes the air above hot, the air below cold, and the air above hot. The evaporation of water vapor in the air expands the range of cloud bands.

At this time, this small tropical cyclone already had a diameter of nearly fifteen meters. The expansion of the cloud belt made this hot and cold motion more intense. Then, the expanding cloud group was affected by the geostrophic deflection force and began to gradually Spin quickly.

The centrifugal force generated by the rotating air throws the air outwards. The air in the center becomes thinner and thinner, and the air pressure continues to decrease. Finally, this small tropical vortex completely sprouts, grows up, and becomes more and more mature. Finally, , reaching a diameter of nearly thirty meters, and entered the initial stage of the typhoon.

…

U.S. Weather Bureau.

The staff were yawning out of boredom and discussing various events that had happened in the world in the past two days.

“Hey, Jobs, have you seen the news in the past two days? Our country’s three aircraft carrier formations have conducted naval exercises. This is a rare large-scale action.” A Meteorological Bureau employee glanced at the screen in boredom, and then rushed to his side. colleagues said.

“Of course, how could you not know about such a big thing,” the colleague smiled and said, “It’s a miracle that such a big battle was fought for a prodigal. To be honest, I feel like it’s a bit of a fuss.”

” No matter what, he is just a prodigal. This is really too much.” The man from before shook his head: “These people have nothing to do and waste military money. There is really no place to spend the aircraft carrier. One sea trip and tens of millions of dollars are gone.” “Don’t worry about high-level affairs.” My colleague sat on the sofa and looked at the satellite cloud image again, and suddenly said in surprise: “Look, what is

this

?”

“What’s wrong?” The first person hurried over and said with a smile: “It’s just a small typhoon, you are so panicked.”

“Haha, you are a little nervous.” On the satellite cloud map, the diameter of the wave is only about thirty. The typhoon weighing 1.3 meters is moving towards the United States, but for everyone at the Meteorological Bureau, such a small typhoon naturally does not need to worry them. Normally, such a small typhoon disappears before it even makes landfall.

“Okay, okay, don’t do useless things.” At this time, the director of the US Meteorological Bureau came in: “Everyone works quickly!”

…

No one in the US Meteorological Bureau was aware of this small tropical vortex. No one cares about it, after all, it is so small that no one even bothers to mention it.

But this small tropical vortex is still working hard to move and grow…

Because the central air pressure of the tropical depression is lower than that of the outside world, the surrounding air rushes into the tropical depression and rises when heated, supplying the tropical depression with more energy. Exceeding the output energy, at this time, the air in the tropical low pressure rotates more fiercely, the maximum wind force in the center increases, and the central air pressure further decreases.

Finally, the maximum wind force near the center reached about 60 kilometers per hour. At this time, this small tropical vortex finally successfully upgraded to a level. It was upgraded from the seed-like tropical depression at the beginning to the intensity of a tropical cyclone. The weakest level of a small typhoon.