
In the air, the amount of water vapor is classified as ______.
A. Wind
B. Precipitation
C. Humidity
D. Temperature
Answer
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Hint: The amount of water vapor in the air is measured as the maximum percentage of water it can hold.
-It is measured using a hydrometer or psychrometer.
-If it increases, the atmosphere becomes sticky and moist.
Complete Answer:
Let us look at the options and discuss the solution.
Option A. Wind is the development of air, brought about by the different warming of the Earth by the sun and the Earth's rotation. Winds range from light breezes to regular dangers, for example, typhoons and tornadoes. Thus, it is an incorrect option.
Option B. Temperature is a proportion of the hotness or frigidity of an article or substance concerning some standard worth. Thus, it is an incorrect option.
Option C. The measure of water vapor noticeable all around is known as humidity. It can make hot temperatures significantly more insufferable. It influences both climates just as the atmosphere. It additionally influences worldwide environmental change. Both low and high humidity is unbearable. Thus, it is the correct option.
Option D. Precipitation is any fluid or frozen water that structures in the climate and falls back to the Earth. It comes in numerous structures, similar to rain, hail, and day off. Alongside vanishing and buildup, precipitation is one of the three significant pieces of the worldwide water cycle. Thus, it is an incorrect option.
Hence the correct answer is Option C.
Additional Information:
Absolute dampness (units are grams of water fume per cubic meter volume of air) is a proportion of the real measure of water vapor noticeable all around, paying little mind to the air's temperature. The higher the measure of water fume, the higher the absolute moistness.
Note: Humidity can influence human wellbeing since it influences our warm solace - as such, regardless of whether we feel excessively hot or excessively cold.
-At the point when the climate is warm and stickiness is high, the body thinks that it's hard to keep cool since it's harder to eliminate heat using vanishing sweat into the air. This can prompt perilous degrees of overheating.
-It is measured using a hydrometer or psychrometer.
-If it increases, the atmosphere becomes sticky and moist.
Complete Answer:
Let us look at the options and discuss the solution.
Option A. Wind is the development of air, brought about by the different warming of the Earth by the sun and the Earth's rotation. Winds range from light breezes to regular dangers, for example, typhoons and tornadoes. Thus, it is an incorrect option.
Option B. Temperature is a proportion of the hotness or frigidity of an article or substance concerning some standard worth. Thus, it is an incorrect option.
Option C. The measure of water vapor noticeable all around is known as humidity. It can make hot temperatures significantly more insufferable. It influences both climates just as the atmosphere. It additionally influences worldwide environmental change. Both low and high humidity is unbearable. Thus, it is the correct option.
Option D. Precipitation is any fluid or frozen water that structures in the climate and falls back to the Earth. It comes in numerous structures, similar to rain, hail, and day off. Alongside vanishing and buildup, precipitation is one of the three significant pieces of the worldwide water cycle. Thus, it is an incorrect option.
Hence the correct answer is Option C.
Additional Information:
Absolute dampness (units are grams of water fume per cubic meter volume of air) is a proportion of the real measure of water vapor noticeable all around, paying little mind to the air's temperature. The higher the measure of water fume, the higher the absolute moistness.
Note: Humidity can influence human wellbeing since it influences our warm solace - as such, regardless of whether we feel excessively hot or excessively cold.
-At the point when the climate is warm and stickiness is high, the body thinks that it's hard to keep cool since it's harder to eliminate heat using vanishing sweat into the air. This can prompt perilous degrees of overheating.
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