Chapter two hundred and eighty-seventh fog lost the tower
The white cloth bag was pierced through with a blink of an eye, and thousands of poisonous bees flocked out, and it turned out to be honeycombs!
As soon as the buzzing sound appeared, the most poisonous bee in the three realms came.
This is a tiger head bee!
The tiger-headed bee is huge and extremely violent. It is generally called a bumblebee, also known as a tiger-headed bee.
This type of bee is the largest and most toxic bee species.
The body color of the tiger-headed bees is bright and usually yellow and black, that is, they have tiger-like marks. The two large jaws on the head are well developed and powerful, and there is a stinger on the tip of the abdomen that connects to the poison glands in the body.
Unlike ordinary bees who feed on pollen, the food of tiger-headed bees is not these small powdery particles, but insects and plants. They even cannibalize each other when the climate is harsh and food is poor.
Bee venom is a poisonous protein composed of many amino acids, which can cause poisoning, such as redness, swelling, strange itching, and tingling, which can cause shock and death in severe cases.
Insects stung by tiger-headed bees will die in minutes, even if large animals are not treated in time, they will die within a few quarters of an hour, and even if trees, flowers and plants are sucked by it, they will dry up locally.
Tigerhead bees belong to a social insect tribe, with members including a female worm that lays eggs, namely the queen, and a large number of worker bees, most of which are female worms, and drones account for only a small number.
"Is it the end of my journey? I started to be clever, and the immortals are really shameless."
Huang Tian despised him, and then he reminded the demon gods: "Be careful, there is Qinyuan recorded in the Book of Changes."
Qin was very similar to bees in its original shape, but it was as big as a mandarin duck. Any bird, beast, human and animal that was stung by it would die immediately, and even the plants would wither and die.
It should be the largest bee known in the Three Realms, so the author classified it as a bird. But its nature has not changed. Poison needles and venom are its most powerful weapons.
The largest body length of ordinary bees is no more than three centimeters, while ordinary mandarin ducks are at least thirty centimeters long, which is more than ten times the length of bees.
The weight is even more different. The venom secreted by ordinary bees is only 30 mg at a time, but if it is Qinyuan, the venom may be as high as dozens of grams at a time. With such a dose, even an elephant will probably be poisoned to death.
Although the demons were a little afraid of the use of the tiger-headed bee and Qin Yuan by the blind immortal, they were not as scared as they were.
Instead of panicing, they stood like stone sculptures and clay sculptures, motionless, and even their breath gradually disappeared.
"Hmph, Qin Yuan, Tigerhead Bee, this method is too unfair and open!"
The voice of the Demon Emperor in the Daytime sounded from all directions, and then he snorted coldly: "The mist lost the tower!"
After the sounds disappeared during the day, gradually, the entire ice cone world began to become hazy and became more and more intense. Within a few breaths, I could no longer see my five fingers.
The fog comes!
When the water vapor is sufficient, breeze and atmosphere are stable, when the relative humidity reaches a certain state, the water vapor in the air will condense into tiny drops and slung in the air, causing the visibility of the ground level to decrease. This weather phenomenon is called fog. More fog occurs between February and April in spring.
The conditions for its formation are: one is cooling, the other is humidification, and increase the water vapor content.
Types of fog include radiation fog, advection fog, mixed fog, evaporation fog, etc.
Fog is a weather phenomenon composed of tiny water droplets or ice crystals suspended in the air near the ground. It is a product of water vapor condensation in the air near the ground. It is a liquid state.
When the water vapor contained in the air reaches its maximum, it reaches saturation.
The higher the temperature of the air, the more water vapor it can hold in the air.
If the water vapor contained in the air is more than the saturated water vapor under a certain temperature condition, the excess water vapor will condense. When enough water molecules bind to the tiny dust particles in the air, the water molecules themselves will also bond to each other, and become small water droplets or ice crystals.
The water vapor in the air exceeds the saturation and condenses into water droplets, which is mainly caused by the decrease in temperature. This is also the reason for the foggy morning in autumn and winter.
If the ground heat is lost, the temperature drops, and the air is quite humid, then when it cools to a certain extent, part of the water vapor in the air will condense and turn into many small water droplets, suspended in the air layer near the ground, forming fog.
It and the cloud are both caused by temperature drops, and the fog can actually be said to be clouds close to the ground.
The temperature is relatively high during the day and the air can accommodate more water vapor.
However, at night, the temperature drops and the ability of the water vapor in the air can be reduced. Therefore, part of the water vapor will condense into fog.
Especially in autumn and winter, due to the long night and the chances of cloudless winds, the ground heat dissipation is faster than in summer, resulting in a sharp drop in the ground temperature. This makes the water vapor in the near-ground air easily reach saturation in the second half of the night to the morning and condense into small water droplets, forming fog.
The temperature is the lowest in the morning of autumn, winter and spring, which is the most fog.
The conditions for fog formation are cooling, humidification, and condensation nuclei, increasing the water vapor content.
One type of fog is formed by radiation cooling, most of which appear in nights and mornings where the water vapor near the ground is abundant and stable or has inversion, and is called radiation fog in meteorologically; the other type is warm and humid air moving horizontally. After passing through the cold ground or water surface, the water vapor in the air is gradually liquefied by cooling, which is called advection fog in meteorologically; sometimes the fog formed by two reasons is called mixed fog.
It can be seen that the one who can meet these conditions is late autumn and early winter, especially in late autumn and early winter mornings.
Smoke in towns is another reason, that is, people's activities.
Morning and evening are the time when a large amount of smoke is discharged. When pollutants are under low air pressure and low wind conditions, they do not easily spread. Combined with water vapor in the lower air, it is easier to form smoke. This smoke often lasts for a long time, resulting in long-term foggy days.
The reasons for the dissipation of fog are, first, due to the increase in the lower surface, the fog droplets evaporate; second, the wind speed increases, blowing away or lifting the fog into clouds; second, there is turbulent mixing, water vapor is uploaded, heat is transferred, and fog droplets evaporate near formation.
The duration of fog is mainly related to the local climate wet and dry climate: Generally speaking, arid areas have shorter fog and mostly dissipate within half an hour, while in humid areas have long fog, which can last for about three hours.
When white light shines on a transparent object, the light it passes through is mainly light of the same color as the transparent object, and other colors are absorbed by the transparent object.
If a transparent object can pass through all colors of light, then this transparent object is colorless, like ice.
However, after the water turns into fog, many reflective surfaces are formed. At this time, the light cannot pass through and is reflected, which means that all kinds of colors of light are reflected off, so the fog becomes white.
There are many types of fog classification methods. According to the weather conditions of fog, it can be divided into two categories: air mass fog and frontal fog:
Air fog has:
A radiating fog: After sunset, hot air on the ground radiates into the sky, and the cooled ground condenses nearby air. The humid air will therefore drop below the dew point and form countless small water points suspended in the air, which is the radiating fog.
It mainly appears in the early morning of autumn or winter, when the weather is clear and the wind is weak, and will naturally dissipate shortly after sunrise or after the wind speed accelerates. It often occurs at night and early mornings where water vapor near the ground is abundant and stable or with inversion.
2 Advection fog: The fog formed by warm and humid air moving horizontally, passing through the cold ground or water surface, gradually cooling, is called advection fog in the meteorological condition. This fog is often accompanied by drizzle weather.
Three evaporation fog: that is, cold air flows through the warm water surface. If the temperature is very different from the water temperature, a large amount of water vapor will evaporate on the water surface and the cold air near the water surface will condense into fog.
At this time, there is often an inverted layer on the fog layer, otherwise the convection will cause the fog to dissipate. Therefore, the evaporation fog range is small and the intensity is weak, which generally occurs around the pond in the second half of the year.
Four uphill fog: This is the fog generated by humid air rising along the hillside and adiabatic cooling to make the air reach supersaturation.
This humid air must be stable and the slope of the hillside must be small, otherwise convection will form and fog will be difficult to form.
Five advection radiation fog: advection radiation fog is caused by the combined action of two factors: advection and radiation.
Frontal fog: It often occurs near the front at the junction of cold and warm air. Generally, after the fog, there is continuous rainfall. Both frontal fronts are present, but most of them are near the warm front.
The front fog is formed by the raindrops in the warm air clouds above the front falling into the cold air on the ground, evaporating, causing the air to reach supersaturation and condensed; while the front fog is moved from warm and humid air to the area occupied by the cold air in front of the front, and is formed by cooling to reach supersaturation.
Because the fog near the front often moves along with the front, military uses this frontal fog to cover the troops and launch sudden attacks on the enemy.
Mixed fog: Sometimes the fog formed by two reasons above is called mixed fog.
Smoke: The commonly referred to as smoke is a solid and liquid mixed aerosol, etc. formed by smoke and mist at the same time.
Valley fog: This usually occurs in winter valleys.
When the heavier cold air moves into the valley, the warm air also passes through the top of the mountain, the temperature increases in the temperature, resulting in a valley fog, which can last for several days.
Ice mist: Ice mist will be generated when the water points in any type of mist are condensed into borneol.
Usually, it will also be generated when the temperature is lower than the coolant point, so it is commonly found in extremely cold places. It can be divided into dispersed aerosols and condensed aerosols. Liquids at normal temperatures are atomized due to splashing, spraying and other reasons, and are dispersed in the atmosphere, forming a dispersed aerosol.
The liquid becomes steam and escapes into the atmosphere due to heating. After cooling, it condenses into tiny droplets to form a condensed aerosol.
Now the Demon Emperor of the Day used these principles to create a "fog loss" that spreads everything and hides everything, making Qin Yuan and the tiger-headed bee suddenly lost their direction and become waste that cannot capture the target.
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Chapter completed!