Moisture is added to air by

7.3 Moisture, Fog and Frost - Practice Questions

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11th Grade
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1.
FLASHCARD QUESTION
Front
Back
evaporation and sublimation.
Answer explanation
As water changes from one state to another, an exchange of heat takes place. These changes occur through the processes of evaporation, sublimation, condensation, deposition, melting, and freezing. However, evaporation and sublimation are the only ways water vapor is added into the atmosphere.
2.
FLASHCARD QUESTION
Front
Why is frost considered hazardous to sUAS operations?
Back
Frost decreases lift capacity by spoiling the smooth flow of air over the propellers.
Answer explanation
Frost is considered hazardous to sUAS operations because it spoils the smooth flow of air over the propellers or wings and makes it harder for the aircraft to generate lift. Frost decreases the lift capacity of the aircraft.
Frost does not change the basic aerodynamic shape of the wing, but the roughness that even a very thin layer of frost creates on an aircraft’s propellers or wings will drastically impact your aircraft’s performance.
3.
FLASHCARD QUESTION
Front
If the temperature is 64°F (and if the temperature/dewpoint spread is too small and decreasing), what type of weather is most likely to develop?
Back
Fog or low clouds
Answer explanation
Fog typically occurs when the temperature of air near the ground is cooled to the air’s dew point. Remember, the dew point is the temperature at which the air will have 100% humidity -- it’s fully saturated with water vapor. At this point, the water vapor in the air condenses and becomes visible in the form of fog.
4.
FLASHCARD QUESTION
Front
What is "dew point"?
Back
The temperature to which air must be cooled to become saturated.
Answer explanation
The dew point, given in degrees, is the temperature at which the air can hold no more moisture, so it’s at 100% humidity. As moist, unstable air rises, clouds often form at the altitude where temperature and dew point reach the same value. At this point, the air is completely saturated, and moisture begins to condense out of the air in the form of fog, dew, frost, clouds, rain, hail, or snow.
The dew point is the temperature air needs to be cooled to become saturated or achieve a relative humidity of 100%. Once the air is saturated, it cannot hold any more water in the gas form. Further lowering of the temp increases saturation and the water vapor starts to condense and appears typically in the form of fog, rain, or frost
5.
FLASHCARD QUESTION
Front
The amount of water vapor which air can hold depends on the
Back
air temperature.
Answer explanation
The dew point, given in degrees, is the temperature at which the air can hold no more moisture, so it’s at 100% humidity.
But the actual variable that affects the dew point is air temperature!
6.
FLASHCARD QUESTION
Front
Clouds, fog, or dew will always form when
Back
water vapor condenses.
Answer explanation
Fog typically occurs when the temperature of air near the ground is cooled to the air’s dew point. Remember, the dew point is the temperature at which the air will have 100% humidity -- it’s fully saturated with water vapor. At this point, the water vapor in the air condenses and becomes visible in the form of fog.
7.
FLASHCARD QUESTION
Front
Low-level turbulence can occur (and icing can become hazardous) in which type of fog?
Back
Steam fog
Answer explanation
Steam fog is common over bodies of water during the coldest times of the year, and because of that, it’s also known as sea smoke. Steam fog forms when cold, dry air moves over warm water. As the water evaporates, it rises and resembles smoke. Low-level turbulence can occur (and icing can become hazardous) with the presence of steam fog.
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