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Thundershowers are produced in the presence of strong convective movements in moist air, and their occurrence is closely related to the stability of the atmosphere.
In summer, on sunny days with little wind, the ground is exposed to strong sunlight, heating the air near the ground, and the closer to the ground, the higher the air temperature rises, and the afternoon is the time when the ground temperature rises the highest, and it is also the most unstable period of the day when the atmosphere is in the sky, so the development of strong convective movement is the most rapid at this time. If the air is very humid and moisture is abundant, thundershowers can occur in the afternoon and evening. This type of thundershower, which is formed by the intense heat of the ground, is called a hot thunderstorm.
From midnight to morning, the ground temperature drops at its lowest and the atmosphere tends to stabilize, so hot thunderstorms are not easy to form.
Thundershowers occur differently in spring than in summer. In summer, hot thunderstorms are mostly produced under the same warm air mass, and the weather before the thunderstorm is clear, while spring thunderstorms mostly occur in the area where cold and warm air masses collide. When the two cold and warm air masses in the north and south clash with each other, the warm and humid air climbs on the back of the cold air, and a large amount of water vapor is condensed, so that the sky is cloudy, it rains for days, and there is no sunlight on the ground all day long, so that the temperature can not rise very high during the day, and the temperature cannot drop very low at night, and the diurnal change of temperature is very small.
However, at the top of the high-altitude clouds, the daytime is still illuminated by the sun, where the diurnal variation in temperature is relatively large.
During the day, the clouds are very hot by the sun, the temperature is easy to rise, the head of the atmosphere becomes lighter, the stability increases, and the possibility of thundershowers becomes smaller; At night, the cloud top dissipates heat into space, and the temperature in the upper part of the cloud drops, especially from midnight to morning, which is the lowest time of the day, and the head of the atmosphere becomes heavier and tends to be unstable. This is the reason why Chunredo appears from midnight to morning.
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Rain is short, has an abrupt start and end, and varies greatly in precipitation intensity. Sometimes accompanied by lightning and thunder, it mostly occurs in the summer.
Rainfall with a significant change in intensity in a short period of time knows no
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Sudden showers. Unexpected showers. Showers without warning.
Showers, which fall from cumulonimbus clouds, are rains that are short, start and end suddenly, and vary greatly in intensity. Sometimes accompanied by lightning and thunder, it mostly occurs in the summer. Showers are discontinuous, generally small in scope, with rain streaks, and often accompanied by high winds.
Introduction
Showers, which generally occur in the sunny weather of summer, without any warning, are sudden rain that makes people unexpected and unprepared. Thundershowers are much more intense than showers, and are accompanied by electrical discharges, which are often preceded by strong winds and thunderstorms.
When the wind comes, the sand and rocks are scattered, and the roof is blown down and the wall is blown down. In the wind and rain, things in the street dance in the wind, fly everywhere, and even uproot large trees. Thundershowers:
Also known as a thunderstorm. A rain shower accompanied by thunder and lightning. China's thundershowers are the most abundant in summer, mainly in spring and autumn in the south of the Yangtze River, and the least in winter, and after October, the thundershowers north of the Yangtze River are basically extinct.
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Thundershower means generally refers to a kind of shower accompanied by thunder and lightning, manifested as a large-scale cloud movement, much more intense than showers, but also accompanied by electrical discharge, commonly found in summer, when thundershowers come, there are often strong winds, thunderstorms combined with weather phenomena, continuous and strong thunderstorms, often up to the level of heavy rain.
The phenomenon of thundershowers is described as a weather phenomenon of strong winds and thunderstorms when thundershowers come, and continuous and intense thunderstorms can often reach the level of heavy rain.
Distribution characteristics of thundershowers: from the time of day, thundershowers mostly occur in the afternoon and evening, the most thunderstorms in the world are Bogor City, Indonesia, with an average of 322 thunderstorm days per year, so it is known as the "thunderstorm capital of the world", the area with the most thunderstorms in China is the Nanling Mountains, with an average of 50 thunderstorm days per year.
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Showers mean: rain that is short, starts and ends suddenly, and varies greatly in the intensity of precipitation, with variable rainfall. Showers have the characteristics of discontinuity, the scope is generally not large, with rain streaks, from the "Atmospheric Science Terminology".
Example sentences: 1. My father has always been introverted and rarely spoken, and he looks gloomy all day long, as if there will be thundershowers at any time.
2. When the thunderstorm comes, it is like a thousand knights roaring in the sky, and it is like a thousand drunken poets chanting in the clouds.
3. The continuous drizzle in spring gradually turned into big drops of showers, and the wind was as cool as in early spring.
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Summary. Local showers: That is, a part of the whole, that is, some places, will rain in bursts, that is, it will not rain continuously.
Local showers: That is, a part of the whole, that is, some places, will rain in bursts, that is, it will not rain continuously.
Local showers are not in the same place, it rains on the left and it does not rain on the right.
Partial: It is a part of the whole of the city, such as a city is not all the city is rainy, but there are places that are part of the city and the place will rain.
Oh. The kind of situation you said is called mountain rain, and some places are called the next stall side road rain, which is a phenomenon of sunrise in the east and rain in the west, and every rain is regional under normal circumstances, showers: It means that the thundershowers we usually talk about will not be continuous, and they will suddenly bury a rough burst of fiber, and it will stop after a while, or the rock erection will rain again after a period of time, so it is called a shower.
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