Handy Book of MeteorologyWilliam Blackwood, 1868 - 371 sider |
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Side 12
... Eastern , and South - Eastern Europe , will furnish the required materials . This admirable publication , which must be regarded as the latest important step taken in the progress of meteorology , shows graphically the atmospheric ...
... Eastern , and South - Eastern Europe , will furnish the required materials . This admirable publication , which must be regarded as the latest important step taken in the progress of meteorology , shows graphically the atmospheric ...
Side 34
... east to west in twenty - four hours . Hence these two hemispheres are in direct contrast to each other in respect of heat , and consequently evaporation , which depends on the temperature . The hemisphere exposed to the sun is warm ...
... east to west in twenty - four hours . Hence these two hemispheres are in direct contrast to each other in respect of heat , and consequently evaporation , which depends on the temperature . The hemisphere exposed to the sun is warm ...
Side 50
... east of Asia is caused by the vapour which the summer monsoon brings to these regions , and which is there precipitated in a copious rainfall . The low pressures which prevail during all seasons in the Antarctic Ocean are no doubt due ...
... east of Asia is caused by the vapour which the summer monsoon brings to these regions , and which is there precipitated in a copious rainfall . The low pressures which prevail during all seasons in the Antarctic Ocean are no doubt due ...
Side 51
... Eastern Asia . The effect of the mountain - systems of Asia , in particular the Yablonoi or Stanovoi Mountains , in ... east , and the west . 106. This area of high barometer is continued westward through Europe south of the North Sea ...
... Eastern Asia . The effect of the mountain - systems of Asia , in particular the Yablonoi or Stanovoi Mountains , in ... east , and the west . 106. This area of high barometer is continued westward through Europe south of the North Sea ...
Side 52
... east and west across the continent damming up the dense cold air and preventing it from flowing over the United States . The effect of the Mediterranean and neighbouring seas , which are at this season warmer than the land surround- ing ...
... east and west across the continent damming up the dense cold air and preventing it from flowing over the United States . The effect of the Mediterranean and neighbouring seas , which are at this season warmer than the land surround- ing ...
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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 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 St Petersburg storm summer temperature terrestrial radiation thermometers tion tropics tube upper currents vapour vols weather wind winter Yakutsk