CYCLONE

On the night of November 12, 1970, a typhoon ravaged the Bay of Bengal. There were continuous winds of up to 150 miles per hour [240 km / hr] and a hurricane, or floods that raised the sea level to a depth of more than 40 feet [10.4 m] - up to 34 feet! Hurricane and floods were wreaking havoc, and by 2021 Hurricane Football was the deadliest hurricane in history, killing an estimated 300,000 to 500,000 people. And the shocking response of the then government of Western Pakistan contributed to the liberation struggle that led to the formation of Bangladesh. Just think, the weather system was powerful, helping to create a completely new world. Extreme weather systems can cause damage in a moment like a hurricane. But they can also come in slowly and make gradual changes in our climate for days, such as the warm spring rains or the unusual hailstorm of the year.

Understanding the timing of various weather systems, how they are formed, and their effects is an important part of the physical universe. Especially because all weather conditions, from heavy thunderstorms to small fog eruptions, drive energy exchanges within the atmosphere. [INTRO] Weather includes all weather conditions at a specific time. And if you live in the middle, or everything between 35 and 55 degrees north and south, you can expect the weather to be predictable. A bright day in southern South Dakota or on the South Island of New Zealand or Scotland can suddenly turn cloudy and gray and suddenly emerge. Every day we may not see what is happening in space, unless there is a natural disaster we are headed for or we are stuck in a lot of small talk. "Good weather still exists today, Brandon. That's right ... sometime! Don't you think?" But there are too many patterns of land distribution in space and in the oceans.

As we have learned, because the Earth is curved and tilted, the amount of sunlight entering, or closing the body, is not the same everywhere. Each year, the tropics receive twice as much energy as poles, which must be released with the help of atmospheric radiation. The unequal amount of insolation also creates variations in temperatures that drive some of the major re-measurement efforts: medium-sized storms, also called tidal storms or external storms. These giant weather systems travel 1,000 miles or more. Although they coincide with the term "storm," the mid-latitude cyclone is a relatively round climate - in contrast to Hurricane Ball, a tropical storm with very little wind. We will talk more about tropical storms later. Moderate storms can last a week or more, bringing with them many changes in daily weather or severe storms as they move from west to east and west winds. These weather systems can be formed in the middle of the width of both hemispheres.

 But closer to where I live for example, in the Northern Hemisphere, we see mid-latitude storms forming eastward, which is a low-pressure band just below the poles that live between two major high-pressure areas: high tropical pressure to the south and high polar to the north. War breaks out in the sky between warm, wet air from tropical areas and cold air from poles. In fact, the term "front polar" was first coined by Norwegian meteorologists Jacob Bjerknes and Halvor Solberg while studying moderate storms. World War I was raging, and the frontier between warm and cold air seemed to be at war with the allied forces. Generally, we can call these two opposers, which are wind bodies with the same temperature and humidity that make up a region. Such as when the air pressure rises above the tropical oceans it will be warmer and more humid than the formation inside the cold northern part of Canada, which will be cold and very dry.

And as they travel, they bring their own temperatures and humidity with them. Intermediate latitudes find a lot of friction between air masses. And that's where a lot of storms and rain come from because when different air masses come together like water and oil or Godzilla and Gothra - they don't like to mix. Instead they meet at the sloping borders called the front. For example, when cold air feels foggy and gets into hot air, we get a cold front. A cold front nose like an ice plow, which you can wrap around because it is big and heavy, pushes warm air out of the way, and then throws it up. And with the cold front comes alternating winds, lower temperatures, and lower pressure. If the tropical heat is unstable and demanding high and humidity, we will receive heavy rainfall from thunderstorms and a continuous wall of cumulus and cumulonimbus clouds. But when the air is cold

the weight recedes, the size of the warm air sees their opportunity and they go in and out, making a warm place. Warm air cannot remove the thick, cold area near the ground, so the warm front slides over it like a thick blanket.

Overall, the warmer climate is abrupt and more violent than before and is usually longer, with a warm, moist air behind it. The first sign of one is higher cirrus clouds, followed by lower and more altostratus clouds, and then lower and thick stratus clouds bring lonely rain. So different air masses bring a different climate to their awakening and influence the local climate as they pass. Warm and cold limits are relatively small stumbling blocks. But wars - or hurricanes in the middle of nowhere - can start when cold air and warm air meet ahead. While these masses of winds are blowing closer and closer to the surface of the earth, another war loom is about three miles [5 km] above them: the western wind blows. These winds blow very fast because there is a small amount of high impact. And within the western hemisphere, about six miles [10 km] above the Earth's surface, the wind blows very fast. He is a jet front jet radio and travels up to 450 kilometers per hour, threatening every place in the world. Even if it has risen sharply in space, a slight change in jet stream direction can cause a forward polar curve leading to a low-pressure area where the pre-heated front moves and the cold front moves towards the equator.

As the air condenses and rises making the low-pressure area turn into a full-blown central storm, the cold air of the massis shrinks and travels faster, passing the explosion, the warm front of the cyclonic and merging beneath it. And it will not end until the storm is completely cut off from the warm air of the air that was its source of energy and moisture. In this war, both the colder parts of the world and the jet stream in the front can also travel at certain times of the year. They can direct cyclonic systems and their masses of wind across the continent as they follow the Sun north to the Arctic in the summer, and then turn south to the south in winter. And no two hurricanes are the same because no two winds are the same. Now, big weather systems don't end up in the middle, even if the warmer and cooler layers happen when a lot happens. In oceans and tropical seas, we can also find hurricanes, low winds, which are some of the biggest hurricanes on Earth. A tropical storm, between the Tropic of Cancer and the Tropic of Capricorn, can grow with incredible winds of over 110 miles [118 km] an hour. They go by many names: storms in the Atlantic, hurricanes in the Pacific, and hurricanes in the Indian Ocean. (So   now we're talking about tropical cyclones now. But we do this by recording this in Florida, near the Atlantic, so I'll call them hurricanes from here on.) Tropical storms come from the same warm air. Without a cold air opponent, there is no precedent.

Warm air in the sea means that there is a lot of water vapor. So as this warm air rises and cools, more energy releases its transition from a weak, low-pressure area to a strong, strong storm - rising up to 12 to 14 miles and taking full altitude of the troposphere. The chimney effect draws more moisture into the system. The air is blown down by low pressure in the eye of the storm, and then sends a whirlwind due to the effect of Cororiolis. The air then rises rapidly to the surface, and is filled with water vapor, which condenses and releases hidden heat energy, producing thunderstorms and heavy rainfall. A lot of time, effort and money is spent on learning storms, so there is something we know. As in the Atlantic, the official hurricane season lasts from the first of June until the 30th of November. But storms are most prevalent in late summer and early fall, when the ocean temperature is 60 degrees Fahrenheit [26 ° C] or higher, and the sea breeze is extremely humid.