Meteorology: Random Listings RSS

In a system of moist air, the dimensionless ratio of the mass of water vapor to the total mass of the system.

Category:Meteorology

A form of data transmission in which the bits of each character are all sent simultaneously, resulting in extremely fast communication but requiring a communication path for each bit. Compare to serial data transmission.

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Same as evaporative power.

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The water portion of the earth as distinguished from the solid part, called the lithosphere, and from the gaseous outer envelope, called the atmosphere.

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An instrument for the measurement of both solar and terrestrial radiation.

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Atmospheric layer throughout which there is no change of temperature with height, i.e. a zero lapse rate.

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A direct-vision nephoscope constructed in the following manner: A grid-work of bars is mounted horizontally on the end of a vertical column and made free to rotate about the vertical axis. The observer rotates the grid and adjusts his or her position unti ...

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The atmospheric pressure at the level of the barometer. May or may not be the same as station pressure.

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Abbreviation for precipitation-evaporation ratio.

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Similar to the spectroheliograph, but used for visual instead of photographic purposes.

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An early and once universal name for the mercury barometer.

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Same as Aeolian.

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Water vapor content of the air. See absolute humidity, dew point, mixing ratio, relative humidity, specific humidity.

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Temperature to which absolutely dry air would have to be brought in order for it to have the same density as moist air, considered at the same pressure.

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A counterclockwise change in wind direction. Backing winds with height are indicative of cold air advection (CAA).

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A hydrometeor consisting of a visible aggregate of minute water and/or ice particles in the atmosphere above the earth's surface. Cloud differs from fog only in that the latter is, by definition, in contact with the earth's surface.

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Sir Napier Shaw's name for the approximate absolute temperature scale,

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The mean difference between the readings of a given instrument and those of a standard instrument.

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A type of climatic diagram whose coordinates are some form of temperature vs. a form of humidity or precipitation.

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Same as atmometer.

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