Meteorology: Random Listings RSS

A definite portion of a stream channel, commonly taken between two gauging stations, but may be taken between any two specified points.

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A hygrometer based upon the diffusion of water vapor through a porous membrane.

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A temperature scale on which the freezing point of water equals 32

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An instrument used for measuring the specific gravity of a liquid.

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bucket rain gauge-A rain gauge where the precipitation collected by the receiver empties into one side of a chamber which is partioned transversely at its center and is balanced bistably upon a horizontal axis. When a predetermined amount of water has bee ...

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A coating of ice, generally clear and smooth. formed by the freezing of supercooled water on a surface.

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A rainbow formed by light rays which have been reflected from an extended water surface. Not to be confused with a reflected rainbow whose image may be seen in a still body of water. The center of a reflection rainbow is at the same elevation as the sun b ...

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The older name for the Celsius temperature scale. Officially abandoned by international agreement in 1948, but still in common use.

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See constant-level balloon.

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FAA

Federal Aviation Administration.

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Same as ombrometer.

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An ion counter of the aspiration condenser type, used for the measurement of the concentration and mobility of small ions in the atmosphere.

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See stage.

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The level at which ice crystals and snowflakes melt as they descend through the atmosphere.

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Liquid water at temperatures colder than freezing.

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

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A numbering system using a base number of 16 and including the ten decimal digits (0 to 9) along with six alpha digits (A to F). Thus. a digit is available to represent each of the possible values of a 4-bit binary digit.

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A numbering system using a base number of 2 and having only two digits: 0 and 1. The fundamental system of representing information with electrical pulses.

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Of or pertaining to rain.

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The difference between the input quantity applied to a measuring instrument and the output quantity indicated by the instrument. The inaccuracy of an instrument is equal to the sum of its instrument error and its uncertainty.

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