# ent

id: 36457
type: PRODUCT
entity:
  | | 64 | 88 | 77 | 67 | 59 | 51 | 45 | | 66 | 88 | 78 | 68 | 60 | 52 | 45 | | 68 | 88 | 78 | 68 | 60 | 52 | 46 | | 70 | 88 | 78 | 69 | 61 | 53 | 47 | | 72 | 89 | 79 | 69 | 61 | 54 | 48 | | 74 | 89 | 79 | 70 | 62 | 55 | 48 | | 76 | 89 | 79 | 71 | 63 | 55 | 49 | | 78 | 89 | 79 | 71 | 63 | 56 | 50 | | 80 | 90 | 80 | 71 | 63 | 56 | 50 | | 82 | 90 | 80 | 72 | 64 | 57 | 51 | | 84 | 90 | 80 | 72 | 64 | 57 | 51 | | 86 | 90 | 80 | 72 | 64


id: 36457
type: PRODUCT
entity:
  | | | | | | +------------------------------| | | | | | |Mean Temperature of Dew-point.| | | | | | | +-------------------------| | | | | | | |Mean Degree of Humidity


id: 36457
type: LAW
entity:
  | | | In.| | | ---------+-------+----+----+----+----+----+--+---+----+---+---------+ January | 29·932|1·44|43·2|33·7|38·3|35·4|89| 11| 1·8|7·7|W.


# bib

id: 22472
title: The Book of the Damned
author: Fort, Charles
txt: ./txt/22472.txt
cache: ./cache/22472.txt
extension: .txt
mime: text/plain
summary:
  instances of similar objects or substances said to have fallen from the later, another object, like the one said to have fallen in 1819, had The substance that looked like beef that fell from the sky. of a substance that looked like beef fell from the sky--"from a clear lived near said he had seen it fall like flakes with the snow." tentatively and provisionally, we accept the Super-Sargasso Sea. Before we take up an especial expression upon the fall of immature and it--think that carved stone objects have fallen from the sky, because they think they have seen such objects fall from the sky. an object the size of a baseball--but I think a thing could fall from wheel-like objects in the sky, see _Nature_, 22-617; London _Times_, luminous object, had been seen to fall from the sky--or from a As to our data of gelatinous substance said to have fallen to this earth


id: 36457
author: Zambra, Joseph
txt: ./txt/36457.txt
cache: ./cache/36457.txt
extension: .txt
mime: text/plain
summary:
  barometers, thermometers, anemometers, and in every class of instruments. mercury in the barometer at the sea-level generally stood above 30 inches; When the mercury in a barometer tube rises or falls, the level of the the instrument, in order to correct the observed height of the barometer. cistern, filled with mercury, the brass tube, with its divided scale and up the frame; on one side of the tube is placed a scale of inches; a small instrument has a large syphon barometer tube, in which the mercurial surface of the mercury in a syphon barometer is read, as in the instrument the instrument, from which the barometer scale of inches is divided. mercurial barometer were corrected for index-error and temperature. into extensive use thermometer and barometer scale-plates made of tube is arrested, _and indicates the exact temperature_ of the bulb or air The _dry_ bulb thermometer indicates the temperature of the air itself;

title:
  A Treatise on Meteorological Instruments Explanatory of Their Scientific Principles, Method of Construction, and Practical Utility


id: 38928
title: Meteorology; or, Weather Explained
author: M''Pherson, J. G. (John Gordon)
txt: ./txt/38928.txt
cache: ./cache/38928.txt
extension: .txt
mime: text/plain
summary:
  dust in the air and little water-vapour present, there is an brine-particles, driven into the air as fog forms above the ocean surface, burnt in filtered air, intense fog is produced when water-vapour is words, a cubic inch of the air contained 200,000 dust-particles--nearly a 12,000 dust-particles in a cubic inch of the air: whereas in the following and 60,000 dust-particles to the cubic inch of air were registered; but in wind the dust-particles reached the low number of 300 per cubic inch, the The number of dust-particles in the air which become centres of of condensation of the water-vapour so as to form a cloud-particle; and a a fog, the dust-particles in the air have been fully clothed with July afternoon, counted 4000 dust-particles in a cubic inch of the air; number of dust-particles in the air of large towns. determines the number of dust-particles in the air.


id: 36344
title: The Mentor: The Weather Serial Number 110; 1 July, 1916
author: Talman, Charles Fitzhugh
txt: ./txt/36344.txt
cache: ./cache/36344.txt
extension: .txt
mime: text/plain
summary:
  Of The United States Weather Bureau Chief of the United States Weather Bureau when the department was first hence the study of weather--meteorology--is one of the most important [Illustration: STATIONS OF THE UNITED STATES WEATHER BUREAU the phenomena of the atmosphere,--rain and snow, cloud and fog, wind and The layer of the atmosphere lying between sea-level and the upper cloud upward in the air shows under average conditions a fall of temperature [Illustration: THE NEW IDEA IN WEATHER OBSERVATORIES At about 200 stations of the Weather Bureau, distributed over the United days after we had made announcement of a "Weather" number of The Mentor. TALMAN, of the United States Weather Bureau, Washington. [Illustration: CENTRAL OFFICE OF THE UNITED STATES WEATHER BUREAU, [Illustration: A SIMPLE WEATHER STATION] The United States Signal Service (now the Weather Bureau) For a number of years the United States Weather Bureau maintained a


id: 38072
title: Wind and Weather
author: McAdie, Alexander
txt: ./txt/38072.txt
cache: ./cache/38072.txt
extension: .txt
mime: text/plain
summary:
  continued north, close to the shore, and the prevailing winds were _from the prevalence of the north, northwest and west winds. map on which are plotted pressure, temperature, wind direction, velocity Moreover, the weather map does not indicate the true flow of the air, The paths vary widely; from the Gulf storms moving northeast and West PATHS OF HIGH AND LOW, GREAT SNOW STORM OF JANUARY 27-28, 1922] Unlike most storms, there was no strong cold northwest wind blowing into the rule in that hemisphere is to face the wind, and the storm centre When a stream of warm air with a high absolute humidity flows north on the east side of a LOW, and a cold northwest wind follows quickly after northwest and west winds during winter months, the decrease in north In summer, southeast and east winds bring fog and cooler weather; while day a moderate wind from the east, known as the sea-breeze.


id: 63122
title: Geography of the Air
author: Greely, A. W. (Adolphus Washington)
txt: ./txt/63122.txt
cache: ./cache/63122.txt
extension: .txt
mime: text/plain
summary:
  resulting mean diminution of pressure, and the movement of the air from places of high to places of low pressure, the lower air ascending believes that air flowing into the cyclone from a "high" at the ground through a difference of temperature of the air from the equator to the largely the result of greater density due to low temperature, as is atmospheric pressure, temperature, and wind direction over the whole Marvin, whose successful experiments on wind pressures and velocities the square of the velocity of the wind, expressed in miles per hour; wind in pounds per square foot and of the velocity in miles per hour. hour too high, and for an indicated velocity of 90 miles the lower temperatures, the observations of Regnault as to the pressure of The work of Professor Hazen in charting tornadoes and in determining Geography of the Air. Great attention had previously been given to this subject by


