Chapter 353: The Sound of Cannon in the Atlantic (1)
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ββ¦ If it is necessary to filter with activated carbon, the fraction can be passed through an activated carbon filter to remove unwanted volatile odors and aromas, and the activated carbon water filter can also be modified to purify the fraction.
The vodka is diluted to the desired concentration, purified water is added to the fraction to reach the desired alcohol content, and the alcohol percentage is measured with a alcohol detector.
The vodka is bottled, bottled with a gravity filling device and the bottle is corked or capped.
That's the basic process, it's easy! β
After listening to it, Li Yaoyang just wanted to say:
"The brain knows, the hands don't."
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Li Yaoyang, the brewing and production of vodka, can't help, all he can do is to open up sales for new products.
Just for the sake of a Yukon, it's not worth opening a new production line.
Theoretically, the regions with the greatest demand for vodka are those who live in cold regions.
So Li Yaoyang's goal is the Great Lakes region, and Alaska!
Some people wonder, is the Great Lakes region colder than the northeast of the ugly country?
Right!
In fact, in terms of latitude, it is actually about the same, which is equivalent to the northeastern part of China, which is closer to the Arctic Ocean ice field climate zone, and is obviously affected.
The central Great Plains forms an airflow channel, which is unobstructed by both the humid climate in the south and the cold climate in the north, so the ice and snow weather in the winter of the ugly country is exceptionally more and causes more disasters.
The wind in Chicago comes from the wind formed by the temperature difference between cold and hot in the lake area, and the friction on the lake surface is small, and the wind from the lake is strong and the cooling is intensified.
Since the Great Lakes region is a body of water with high specific heat, the temperature is not high.
Coupled with the large lake effect, it is not surprising that the lake area has more water vapor (evaporative heat absorption), cloudy and foggy, more rainy weather, and less sunlight, so the climate is wet and cold.
Let's talk about geography again, there are three major westerly troughs in the northern hemisphere: the Eastern European trough, the East Asian trough, and the North American trough.
Among them, the North American trough is one of the causes of the cold in the central part of the country, with warm and humid air in the south of the westerly wind belt and cold air from Hudson Bay in the north.
Somebody asks, no, sometimes I see as if a westerly jet has passed south of the Rocky Mountains, and there's something called Robespo.
Because the troughs were disobedient, they were also running around, and sometimes when the Zephyr trough was forcibly carried away, the jet had to go around the Rocky Mountains from southern California and then north in West Texas.
At this time, the weather in the middle of the country is relatively warm, and it can even exceed 10 degrees Celsius in January, even all the way to Minnesota!
However, at this time, the jet has just come out of Texas and is heading north, and the positive vorticity southerly wind flow will sweep the warm and humid air from the Gulf of Mexico, and often there will be rain in the Midwest at this time, and even due to the strong convection, there will be tornadoes in Texas.
In fact, the geographical conditions of the ugly country are really good, if the southwest branch of China can only bring some warm and humid air from the Bay of Bengal, through the Hengduan Mountains, the rest of the rain brought to the northern Shaanxi area will be very little.
If the southwest trough could blow directly over the warm sea, and if it did not pass through the Hengduan Mountains, then the precipitation in northern Shaanxi would be considerable.
But why is it called the North American slot?
In fact, most of the time it is still found in central and eastern North America, and most of the time, westerly jets travel north from the west coast, bypassing the Rocky Mountains from the Maple Leaf Country in the north.
At this time, the warm and humid air currents from the eastern Pacific Ocean will be swept in, causing heavy rains on the west coast of the "Pineapple Express", and then it will move south in the central part of the country and north again on the east coast of the country of the country.
The north of the westerly jet is a territory of cold air, so most of the time the central part of the country is under the control of a dry and cold air mass.
In many cases, westerly jets even blow through the maple leaf nation of western Newfoundland, which means that in the winter, the Newfoundland region is even warmer than the Texas coast.
The second reason is that the positive vorticity airflow in front of the trough of the westerly trough tends to produce a divergent effect, and the positive vorticity divergent airflow in front of the trough will generate low pressure on the ground, and the air will rise to a high place and become a high pressure at high altitude, and then run into the trough, sink, and become a cold high pressure.
Then the cold air mass is maintained, and the low latitudes in front of the westerly trough are the warm air masses from the lower latitudes, which do not need to be maintained, which is a typical extratropical cyclone.
Therefore, under the action of Coriolis force, the air in the center of the low pressure on the ground is all counterclockwise towards it, and the air in the west of the low pressure in the northern hemisphere moves to the south, and the air in the east moves to the north.
Warm air moving north, in fact, can only be north of the westerly wind from the beginning to the end, if the westerly wind belt is not broken.
Before the cold air breaks away from the main force, it appears as a westerly wind belt extending southward.
An extratropical cyclone will cause the westerly trough west of the centre of low pressure to extend further southward, essentially sending cold air southward.
However, the positive vortex air flow in front of the westerly trough is often forced to move north after encountering strong warm and humid air from the Gulf of Mexico, and finally basically rides north from the east coast of the ugly country to Newfoundland.
The center of depression of these extratropical cyclones tends to be very close to the east coast, in other words, the east coast tends to be on the eastern boundary line of the cold air mass/westerly trough, the "flank" of the cold air, where the cold air is weaker.
But when the Central Great Plains is the "front" of the cold air, it is very strong and the cold air flanks force its way over the Appalachian Mountains to Maryland, Virginia, and North Carolina.
Falling from a mountain to a lower altitude will cause a slight foehn effect, and the temperature will rise, weakening the power of the cold air.
The third reason is the topography of the Ugly Country, a small half of the country's land is mountainous, that is, the Rocky Mountains in the west, and the plains in the east can reach half of the country's land, and there are not even decent hills in the middle.
Not to mention the mountains where things go from east to west, the cold air goes along the lowlands, and it is naturally not easy to bully when encountering the tall Rocky Mountains, and the central plain area of the Pingchuan River is a good object to vent.
Coincidentally, the westerly trough has been in the central Great Plains for a long time, which greatly facilitates the cold air to march southward.
In the east, the Appalachian Mountains are encountered, and the only breakthrough that can be used is the St. Lawrence River Valley.
Originally, this was not the direction of the cold air's frontal attack, and now the cold air flank is a bit powerless to climb over the Appalachian mountains.
The fourth reason is the North Atlantic Current, which did not leave the North American coast until near New York and headed straight for Europe, causing the air above to be relatively warm, increasing the temperature difference between the cold and warm air masses.
The greater the difference, the more conducive it is to the strengthening and maintenance of extratropical cyclones, and the more powerful the cold air from the Central Great Plains is to move southward.
This North Atlantic current is also one of the reasons why the westerly winds are forced north on the east coast of North America.
Because the warm air here is too strong, the cold air is already at the end of the crossbow here, and it can't beat the warm air, and the sphere of influence is limited, so the westerly wind belt will step on the "bottom line" of the polar air mass in Hudson Bay and move northward.
It should be noted that the westerly jet will still continue to roll in the warm and humid air flow from the south, and the warm and humid air will encounter the cold air and there will be a significant precipitation process, and the water vapor will condense or even freeze into snow.
This process requires heat to be released, which benefits the East Coast, which is known to feel less cold on a snowy day
In addition, one mistake in the traditional concept must be corrected.
In fact, the average winter temperature in the Rocky Mountains is colder than that of the Central Great Plains, and the average temperature of the plateau must be colder than that of the plains.
However, the reason why I feel that the central Great Plains region is colder is that the extratropical cyclones here on the east coast are very explosive and strengthen quickly, and the cold front often causes the westerly wind belt to move southward quickly and cool down very quickly.
It just so happens that the cold air mainly does not go to the mountains, and people mistakenly think that the central plains are colder than the Rocky Mountains but explosive cyclones, and the cold air is very fast, and it will heat up quickly after it passes, and the temperature in the Rocky Mountains is relatively low after the warming.
This is true in the Great Lakes, and even more so in Alaska, on the edge of the Arctic Circle, where you have to find a way to warm yourself when it's cold, and what better way to warm up than a sip of hard wine on a cold day?
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At the beginning of spring, a movie called "Cannon Sound on the Atlantic" was launched in New Jersey in a low-key manner, and Li Yaoyang came to the scene in person and brought a relatively trendy start-up ceremony - respecting heaven and ghosts.
The ghost guy thought it was novel, and the Chinese people who participated in the production were not surprised.
But for Lai, it's all amazing.
He has been involved in countless filmmakings, but this is the first time he has made a film in this era.
Looking at the old photographic equipment and the retro costumes in his eyes, he always felt like he was in a dream.
But if you pinch your thighs hard, you know that all this is not a dream, and it really can't be real!
Anyone who knows cinema knows that the first real movie cameras and projectors were made in Edison's lab in New Jersey.
Human vision is temporary, for example, a cigarette butt that is lit at night will see a complete circle, and the principle of cinema is here.
Around the 30s of the 19th century, there was an entertainment game in Europe, a device called the magic disk, which was often placed in the living room.
Turning one of the discs and looking through the gap between the other fixed discs, you will feel that the small paintings on the edges of the movable discs seem to move.
After improvement, the original use of reflectors and light changers, a special light box, to project the drawn image onto the screen.
In this way, in the past ten years, everyone has done a lot of experiments.
For example, stick a few photos on the wheels of a wheel, which are segments of the action before and after.
Start spinning the wheels, and as a result, one will see a continuous movement come to life.
Since Edison invented the light bulb and the phonograph, he wanted to increase sales, so he decided to link image and sound, which would surely increase the sales of his audiovisual equipment.
However, after Edison's large investment, it was still difficult to achieve the synchronization of sound and image.
Driven by curiosity, people began to imitate each other, and began to make and produce.
That's how the animation studio was born.
Pedestrians used to spend a few coins to watch a 15-second lively action show through a small hole, and such a game spread to the Chinese people called the Western Scene, and until the 80s of the 20th century, it could still be seen on the streets.
What was the film of this so-called early cinema?
The train coming into the station, the female worker who eats after work, the baby who feeds, etc., and it is very short.
But this novelty has fascinated countless citizens in an instant, and they are rushing to watch the anime.
The animation has no sound, and because Edison's research was unsuccessful, there has been no sound and shadow synchronization.
Because this kind of movie, after all, is too simple, it quickly loses its magic, and the movie gradually falls into the cold.
In 1896, a magician, MΓ©rieux, also got a projector in fashion to set it up for his own use.
One day he was watching one of his recent works with self-appreciation, and suddenly saw a shocking picture.
The carriage pulls the coffin, what's going on?
The magician jumped up from his chair, and he was terrified.
I suddenly remembered that there was a carriage pulling a coffin passing by during the shooting, but it was just after the machine did not turn, which means that this suddenly inserted picture was caused by the reshoot after the machine stopped.
This new discovery is that the magician experimented with a series of shooting methods, he stopped, then shot again, stopped and shot some movements, and the combination of pictures was amazing.
The dying film was brought back to life at the hands of this magician, who successfully founded a studio and a star film company.
In 1899, he made the newsreel "The Dreyfus Affair", which was based on the realism of real French society and created a precedent for the film industry to reproduce history.
Film art has a history of more than 100 years, and film has had a close relationship with the world since its birth.
In the mid-90s of the 19th century, the Lumière brothers' filmmaking focused on documenting the events of everyday life in the world.
Giotto Canudou, the proposer of the "Seventh Art Manifesto", as a pioneer of film theory, "admitted in the early 20th century that the idea of nature adding characters was right."
Nature's refusal to decorate and dress it up is certainly suitable for intensifying the storyline, and at the same time becoming an important factor in the integration of the storyline and the actors".
Kanudu believes that cinema is an expression of mental activity, and tries to extract this meaning from the whole work, but the integration of the character's spirit with nature is essential.
Louis de Lucke, the first heir to Canudou's theoretical activities, did not forget to pay attention to the special situation of French history after the First World War in his films, and his concern for reality was the background of filmmaking.
"Visualism" was criticized by De Luc for his mistakes in his work, and developed to the limit in the hands of Sherman Dulac.
The avant-garde cinema of pure form, pure style and pure decoration, Jacopo ComΓn calls it "curiosity", and perhaps not creation.
However, Dulac founded both The State of France and Cinema in the Service of History.
It is not difficult to see that this avant-garde figure is also concerned with real issues, and Dulac believes that it is faster to report the news in film, and the masses are closer to the news.