Handy Book of MeteorologyWilliam Blackwood, 1868 - 371 sider |
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Side 34
... consequently evaporation , which depends on the temperature . The hemisphere exposed to the sun is warm , and the hemisphere turned in the other direc- tion is cold . Owing to the short time of each revolution , the period of greatest ...
... consequently evaporation , which depends on the temperature . The hemisphere exposed to the sun is warm , and the hemisphere turned in the other direc- tion is cold . Owing to the short time of each revolution , the period of greatest ...
Side 41
... consequently , the difference be- tween the temperature in July and January is very small , the difference in the pressures of the same months is also very small , being only 0.018 inch . At Guatemala , 4856 feet high , the mean ...
... consequently , the difference be- tween the temperature in July and January is very small , the difference in the pressures of the same months is also very small , being only 0.018 inch . At Guatemala , 4856 feet high , the mean ...
Side 45
... consequently , the lines are hypothetical , they are made . dotted lines . 90. MEAN ATMOSPHERIC PRESSURE FOR JULY . - It will be seen from Plate I. , representing the mean pressure for July , * The following are a few of the places ...
... consequently , the lines are hypothetical , they are made . dotted lines . 90. MEAN ATMOSPHERIC PRESSURE FOR JULY . - It will be seen from Plate I. , representing the mean pressure for July , * The following are a few of the places ...
Side 47
... consequently its temperature rises higher than that of the sea . From the above causes the summer temperature of continents greatly exceeds that of the ocean in the same latitudes . An ex- amination of Plate IV . will show the ...
... consequently its temperature rises higher than that of the sea . From the above causes the summer temperature of continents greatly exceeds that of the ocean in the same latitudes . An ex- amination of Plate IV . will show the ...
Side 49
... Consequently this ocean shows the great- est excess of atmospheric pressure as compared with other parts of the earth's surface in the same latitudes . The South Atlantic shows also a pressure as high ; but this pressure is due both to ...
... Consequently this ocean shows the great- est excess of atmospheric pressure as compared with other parts of the earth's surface in the same latitudes . The South Atlantic shows also a pressure as high ; but this pressure is due both to ...
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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