what do you mean by humidity Latitude
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Answer:
Humidity latitude is equal to the mass of water vapor divided by the total volume of air, or water vapor density. Absolute humidity changes as the volume of an air parcel changes. Changes in the volume of an air parcel occur normally as air rises or sinks.
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Answer:
Humidity
The amount of water vapor in the air is referred to as humidity. Humidity may be usefully defined in any of several ways:
* Absolute humidity is equal to the mass of water vapor divided by the total volume of air, or water vapor density. Absolute humidity changes as the volume of an air parcel changes. Changes in the volume of an air parcel occur normally as air rises or sinks.
* Specific humidity is equal to the mass of water vapor in the air divided by the total mass of the air parcel (including the water vapor). Since this is a unitless number, it is expressed as a percentage.
* Mixing ratio is the mass of the water vapor divided by the mass of the air parcel without the mass of the water vapor included (dry air). Again this is a unitless quantity that is expressed as a percentage. Specific humidity and mixing ratio remain constant as long as water vapor is not added to or removed from a parcel of air.
Specific humidity is at a maximum in the Tropics and declines as one moves poleward reaching minimum values in each polar region. This implies that the air in the most "arid" desert regions of the planet (30 degrees N or S latitude) actually contains more water vapor than temperate regions much farther north, and certainly more than the polar regions.
Explanation:
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