Handy Book of MeteorologyWilliam Blackwood, 1868 - 371 sider |
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Side 13
... wind from its ordinary direction , indicate the presence of a storm at no great distance . By closely watching the wind and the barometer , the course the storm is taking can be readily known . 26. In the schools of the United States of ...
... wind from its ordinary direction , indicate the presence of a storm at no great distance . By closely watching the wind and the barometer , the course the storm is taking can be readily known . 26. In the schools of the United States of ...
Side 75
... winds , and being guided by the figures in the table given above , the mean tempera- ture was probably 54 ° .4 ... wind passes over it at a reduced rate and force , and there being consequently less evaporation , our bodies are de ...
... winds , and being guided by the figures in the table given above , the mean tempera- ture was probably 54 ° .4 ... wind passes over it at a reduced rate and force , and there being consequently less evaporation , our bodies are de ...
Side 123
... wind . Also , since the temperature of the ocean is more uniform than that of the land , winds coming from the ocean ... wind ; whereas the polar current , gaining heat in its progress towards the equator , becomes a drier wind . Hence ...
... wind . Also , since the temperature of the ocean is more uniform than that of the land , winds coming from the ocean ... wind ; whereas the polar current , gaining heat in its progress towards the equator , becomes a drier wind . Hence ...
Side 124
... winds on climate . If the mountain - chains lie perpendicular to the course of the wind , and are at the same time of great height , the effect will be to some extent to divert the winds from their course . But the chief effect mountain ...
... winds on climate . If the mountain - chains lie perpendicular to the course of the wind , and are at the same time of great height , the effect will be to some extent to divert the winds from their course . But the chief effect mountain ...
Side 142
... wind . Nothing could present this in a clearer light than the winds which are found to occur dur- ing the November and December periods . Thus , during the cold period of November , winds from the N.E. , N. , and N.W. were in the ...
... wind . Nothing could present this in a clearer light than the winds which are found to occur dur- ing the November and December periods . Thus , during the cold period of November , winds from the N.E. , N. , and N.W. were in the ...
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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