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A device used by oceanographers to obtain subsurface samples of sea water. The "bottle" is lowered by wire, its valves open at both ends. It is then closed in situ by allowing a weight (called a messenger) to slide down the wire and strike the reversing mechanism. This causes the bottle to turn upside down, closing the valves and reversing the reversing thermometers which are mounted on it in a special thermometer case. If, as is usually the case, a series of bottles are lowered, then the reversal of each bottle releases another messenger to actuate the bottle beneath it.
A series of Nansen-bottle water samples and associated temperature observations resulting from one release of a messenger.
The nautical mile is closely related to the geographical mile which is defined as the length of one minute of arc on the earth's equator. By international agreement, the nautical mile is now defined as 1852 meters.
An instrument which measures the scattering function of particles suspended in a medium in order to determine the visual range through the medium. See visibility meter.
A general term for instruments designed to measure the amount of cloudiness.
An instrument for determining the direction of cloud motion. There are two basic designs of nephoscope, the directvision nephoscope and the mirror nephoscope.
An instrument for measuring the difference of the solar radiation falling on both sides of a horizontal surface from the whole hemisphere.
An instrument for measuring the difference between incoming and outgoing terrestrial radiation.
The difference between downward and upward (total) radiation; net flux of all radiation.
An instrument for the measurement of the net flux of downward and upward total (solar and terrestrial) radiation through a horizontal surface.
The difference between the solar radiation directed downward and upward; net flux of solar radiation.
A reflecting type telescope with a 45° mirror. so that the primary image is observed through a hole in the side of the tube.
A remote indicator for wind speed and direction used in conjunction with a contact anemometer and a wind vane. The indicator consists of a center light, connected to the contact anemometer, surrounded by eight equally spaced lights which are individually connected to a set of similarly spaced electrical contacts on the wind vane. Wind speed is determined by counting the number of flashes of the center light during an interval of time. Direction, indicated by the position of the illuminated outer bulbs, is given to 16 points of the compass.
A conically shaped, copper rain gauge shield.
Not a linear function of the relevant variables.
A rain gauge which indicates but does not record the amount of precipitation captured.
The range of operating conditions within which a device is designed to operate and for which operating influences are stated. See operating conditions, reference operating conditions.
A type of pressure-plate anemometer in which the plate, restrained by a stiff spring, is held perpendicular to the wind. The wind-activated motion of the plate is measured electrically. The natural frequency of this system can be made high enough so that resonance magnification does no occur.
A wind scale adapted by the U.S. Forest Service for use in the forested areas of the northern Rocky Mountains (NRM). It is an adaptation of the Beaufort wind scale. The difference between these two scales lies in the specification of the visual effects of the wind. The force numbers and the corresponding wind speeds are the same in both.
National Weather Service. Administered by the U.S. Department of Commerce.
Acknowledgments
Our thanks to the NovaLynx Corporation for the use of their glossary.