Handy Book of MeteorologyW. Blackwood and Sons, 1868 - 371 sider |
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Side 32
... feet where great accuracy is not required , or where it is not possible to be attained . But in reducing to sea ... feet . Observed mean height , Correction required at 61 ° .7 ( Table I. ) , Reduced to 32 ° , 29.820 inches . -.088 22 ...
... feet where great accuracy is not required , or where it is not possible to be attained . But in reducing to sea ... feet . Observed mean height , Correction required at 61 ° .7 ( Table I. ) , Reduced to 32 ° , 29.820 inches . -.088 22 ...
Side 33
... feet : the height is therefore 450 feet above the sea . In cases where simultaneous observations cannot be had at the sea- level , the height may be determined from observations made at some known height above the sea , with which ...
... feet : the height is therefore 450 feet above the sea . In cases where simultaneous observations cannot be had at the sea- level , the height may be determined from observations made at some known height above the sea , with which ...
Side 41
... feet above the sea , the pressure in summer is 22.364 inches , while in winter it is only 22.044 inches . At Padua , there is scarcely any difference in the pressure between summer and winter . The increase in the summer pressure at the ...
... feet above the sea , the pressure in summer is 22.364 inches , while in winter it is only 22.044 inches . At Padua , there is scarcely any difference in the pressure between summer and winter . The increase in the summer pressure at the ...
Side 45
... feet in height . For higher situations the reduction was made by means of Dippe's me- thod , as detailed in Guyot's Mathematical and Physical Tables , ' D , p . 60 . 89. In the charts the isobarometric lines are drawn for every tenth of ...
... feet in height . For higher situations the reduction was made by means of Dippe's me- thod , as detailed in Guyot's Mathematical and Physical Tables , ' D , p . 60 . 89. In the charts the isobarometric lines are drawn for every tenth of ...
Side 51
... feet above the sea . The highest atmospheric pressure does not occur at this point , but at a considerable distance westward , near the sources of the Obi and Yenisei . The non - coincidence of the areas of greatest cold and greatest ...
... feet above the sea . The highest atmospheric pressure does not occur at this point , but at a considerable distance westward , near the sources of the Obi and Yenisei . The non - coincidence of the areas of greatest cold and greatest ...
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America antisolar point ascending Asia Atlantic atmospheric pressure average barometer blow Britain calm causes centre charts cirrus cirrus cloud cistern climate cloud coast cold colder column condensed continent Crown 8vo daily dew-point diminished direction dry air earth earth's surface east Edition electricity equator equatorial current Europe evaporation falls Fcap feet flow globe greater heat height hemisphere Hence high pressure higher hour humidity hygrometer Iceland inch of mercury inches increase Indian Ocean isobarometric lines January John Herschel July latitudes low pressure lower Mauritius maximum mean temperature mercury Meteorological meter miles minimum moisture monsoon months northern northern hemisphere Norway observations occur ocean Orkney perature Plate polar current polarisation prevail Professor rain rainfall regions rises round Scotland season snow soil south-west St Petersburg storms summer temperature terrestrial radiation thermometers tion tropics tube upper currents vols weather wind winter Yakutsk
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