Answer to Question 1
Answer: Relative humidity: relates the amount of water vapor in the air to the maximum possible at the current temperature. The World Meteorological Organization defines the relative humidity as
RH = (mixing ratio/saturation mixing ratio) x 100. Because of its dependence on temperature, the relative humidity will change throughout the course of the day even if the amount of moisture in the air is unchanged. Dew point: the temperature at which saturation occurs. It is a simple index to use and easy to interpret. And it is dependent almost exclusively on the amount of water vapor present.
Answer to Question 2
Answer: Specific humidity expresses the mass of water vapor existing in a given mass of air. Specific humidity has the advantage of not changing as air expands or contracts. When a kilogram of air expands, its mass is unchanged (it is still 1 kg), and the proportion that is water vapor is unchanged. As a result, the specific humidity is unaffected. Likewise, specific humidity is not temperature dependent. If a kilogram of air contains 1 g of water vapor, it still contains 1 g after heating. For this reason, specific humidity is a good indicator for comparing water vapor in the air at different locations whose air temperatures might be different from each other.
Major moons of Uranus in order of increasing distance (left to right), at their proper relative size
Relative energies of covalent bonds and noncovalent interactions
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One way to think about the different phases or stages of adulthood is in terms of the relative ...
Finger pressure to a trigger point.
Point Mutations