Barometric sentence example

barometric
  • As a result of their isolation, the proportion of endemic plants is greater here than in any other region, and the great elevation of the mountains, with the consequent variation in temperature, moisture and barometric pressure, has multiplied the number of species.
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  • The regular tides are hardly perceptible, but, under the influence of barometric pressure and wind, the sea-level occasionally varies as much as ft.
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  • (9) The velocity then should be independent of the barometric pressure, a result confirmed by observation.
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  • The theoretical investigation given above shows that if U is the velocity in air at 1° C. then the velocity U ° at o° C. in the same air is independent of the barometric pressure and that Uo = U /(1 +o o01841), whence U 0 =332 met./sec.
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  • The average barometric pressure over England is about 2 9.94 in., and normally diminishes from south-west to north-east at all seasons, the mean pressure on the south coast being 29.97 and that on the northern border 29.88.
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  • The results obtained as to the relation between dissipation and barometric pressure are conflicting.
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  • The mean annual barometric height is 29.93 in.; the mean annual moisture, 81%; the mean annual rainfall, 27.99 in.
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  • the great range of the diurnal variation of barometric pressure during the afternoon hours, - which is the more striking, since at Rurki, Lahore, and other stations near the foot of the Western Himalayas this range is less than in the open plains.
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  • Or early climatologists who made their own daily observations of precipitation and barometric pressure, interpreting as well as collecting readings.
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  • In addition, the Edge 305 incorporates a barometric altimeter for extremely accurate elevation and vertical profile data.
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  • The barometric altimeters that are used in some of our most popular heart rate monitors are very accurate, pressure sensing devices.
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  • In reality, the Davis Vantage Pro Plus measures atmospheric pressure, but then translates this to barometric pressure.
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  • Barometric pressure also changes with local weather conditions, making barometric pressure also changes with local weather conditions, making barometric pressure an extremely important and useful weather forecasting tool.
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  • barometric pressureesults will vary depending on part number, vehicle application and barometric air pressure.
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  • .110 Eiffel 100 Tower Summer 110 100 Bureau Central Winter Bureau Central 110 Summer 100 110 Kew Barometric 100 Pressure 90 night its hour of maximum).
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  • On the Sonnblick, Conrad (22) found dissipation increase decidedly as the absolute barometric pressure was larger, and he found no difference between days of rising and falling barometer.
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  • At Trieste, Mazelle (47) found no certain connexion with absolute barometric pressure.
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  • von Schweidler (46) found no connexion between absolute barometric pressure and dissipation, also days of rising and falling pressure gave the same mean.
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  • of mercury it boils at 170° C. In an atmosphere of steam it distils without decomposition under ordinary barometric pressure.
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  • The result is calculated by means of the formula: _ W0 +at) X 7,980,000 D (p +pI - s) [m { 1 + a (t - to) } - m l { 1 + y (t - to) } 1(I + yt)' in which W=weight of substance taken; t= temperature of vapour bath; a =0.00366 = temperature coefficient of gases; p= barometric pressure; p i = height of mercury column in vessel; s= vapour tension of mercury at t°; m= weight of mercury contained in the vessel; =weight of mercury left in vessel after heating; R = coefficient of expansion of glass = 0000303; y = coefficient of expansion of mercury =o 00018 (0.00019 above 240°) (see Ber.
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  • The theoretical investigation given above shows that if U is the velocity in air at 1° C. then the velocity U ° at o° C. in the same air is independent of the barometric pressure and that Uo = U /(1 +o o01841), whence U 0 =332 met./sec.
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  • The middle region, to 14°-16° N., has variable winds in an area of low barometric pres- sure, while in the southern Red Sea south-east and east winds prevail.
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  • The watch checked the barometric pressure at intervals of 15 seconds in order to track elevation and any weather changes.
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  • This watch also measures altitude and barometric pressure and is water resistant to 330 feet.
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  • The two last curves in the diagram contrast the diurnal variation at Kew in potential gradient and in barometric pressure for the year as a whole.
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  • At barometric pressures such as exist between 18 and 36 kilometres above the ground the mobility of the ions varies inversely as the pressure, whilst the coefficient of recombination a varies approximately as the pressure.
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  • A Log Book is a marine or sea journal, containing, in the British navy, the speed, course, leeway, direction and force of the wind, state of the weather, and barometric and thermometric observations.
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  • causes an accumulation of air over the cold area, The diminution of barometric pressure which takes place all over Asia during the summer months, and the increase in the winter, are hence, no doubt, the results of the alternate heating and cooling of the air over the continent.
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  • of mercury it boils at 170° C. In an atmosphere of steam it distils without decomposition under ordinary barometric pressure.
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  • It has been found that variations in barometric pressure affect the flash-point and accordingly corrections have to be made in obtaining strictly comparative results at different pressures.
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  • The height of Zahr el-Kazib, by barometric measurement, is 10,018 ft.; that of the others does not reach io,000 ft.
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  • His dissertation on the "barometric light," first observed by Jean Picard, and discussed by Jean Bernoulli under the name of mercurial phosphorus, or mercury shining in vacuo (Diss.
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  • the height of the mercury in the wide tube and the top of f he narrow tube represents the pressure due to the mercury column, and this must be added to the barometric pressure in order to deduce the total pressure on the vapour.
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  • While the majority of his researches bear on one or other of the subjects just mentioned, others deal with such widely different topics as the birds of Greenland, ocean temperatures, the Gulf Stream, barometric measurement of heights, arcs of meridian, glacier transport of rocks, the volcanoes of the Hawaiian Islands, and various points of meteorology.
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  • The middle region, to 14°-16° N., has variable winds in an area of low barometric pres- sure, while in the southern Red Sea south-east and east winds prevail.
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  • While these are tracks frequently followed by the centres of barometric depressions, individual cyclones may and do cross the country in all directions, though very rarely indeed from east to west or from north to south.
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  • There were indications that monsoon influences extended as far north at least as the Great Pamir, and a definite analogy was established between the record of barometric pressure on the Pamirs and that of the outer ranges of the Himalaya.
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  • by means of the formula Vo=V(P - p)/(z-}- o0366t)760, in which V is the observed volume, P the barometric pressure, p the vapour tension of water at the temperature t of the experiment.
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  • The barometric pressure at sea-level in the south-west of Iceland during the period 1878-1900 varied between 30.8 and 27.1 in.
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  • of the Platte, and are evidently sensitive to barometric conditions; alternately " blowing " or sucking " as these vary; so that, in cold weather water-pipes may be frozen too or more feet below the surface of the ground.
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  • and a barometric height of 30 in.
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  • This diminution of pressure, which continues as the heat increases till it reaches its maximum in July soon after the solstice, is followed by the corresponding development of the south-west monsoon; and as the barometric pressure is gradually restored, and becomes equalized within the tropics soon after the equinox in October, with the general fall of temperature north of the equator, the south-west winds fall off, and are succeeded by a north-east monsoon, which is developed during the winter months by the relatively greater atmospheric pressure which then occurs over Asia, as compared with the equatorial region.
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  • The prevailing winds in this region, which the sea traverses longitudinally, are westerly, but the sea itself causes the formation of bands of low barometric pressure during the winter season, within which cyclonic disturbances frequently develop, while in summer the region comes under the influence of the polar margin of the tropical high pressure belt.
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