Meteorology: Random Listings 

Companion to the wet-bulb thermometer in a psychrometer. Used to measure ambient air temperature.

A general name for instruments which detect the presence of (but do not necessarily measure) small electrical charges by electrostatic means. Compare to electrometer.

A line drawn through geographical points having the same duration of sunshine (or other function of solar radiation) during a given interval of time.

A faintly-colored circular arc similar to a rainbow but formed on fog layers containing drops whose diameters are 100 microns or less. Also called mistbow, white rainbow.

A device that combines several separate communications signals into one and outputs them on a single line.

A type of cooling-power anemometer based upon the principle that the time constant of a thermometer is a function of its ventilation.

An instrument which automatically determines the size distribution of raindrops.

Anemometer which generates an electrical contact output with a frequency proportional to wind speed.

Ragged low clouds, usually stratus fractus. Most often applied when such clouds are moving rapidly beneath a layer of nimbostratus.

Thermometer in which the difference in the rates of expansion with temperature of a liquid and its receptacle is used as a measure of the temperature. The liquid used may be ethyl alcohol, toluene, petroleum, or mercury.

A reversing thermometer (for seawater temperature) which is not protected against hydrostatic pressure. The mercury bulb is therefore squeezed, and the amount of mercury broken off on reversal is a function of both temperature and of hydrostatic pressure.

Name applied to a class of instruments which measure the liquid content of the atmosphere.

The unit of speed in the nautical system; one nautical mile per hour. It is equal to 1.1508 statute miles per hour or 0.5144 meters per second.

The difference between downward and upward (total) radiation; net flux of all radiation.

The wind speed and direction at various levels in the atmosphere above the level reached by surface weather observations.