Weather: A Popular Exposition of the Nature of Weather Changes from Day to DayD. Appleton, 1887 - 472 стор. |
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Сторінка 5
... developed the science of statistics . By this method the average readings of meteorological instruments , such as the height of the barometer or thermometer , or the mean direction and force of the wind , at any number of places were ...
... developed the science of statistics . By this method the average readings of meteorological instruments , such as the height of the barometer or thermometer , or the mean direction and force of the wind , at any number of places were ...
Сторінка 6
... developed by Dové and Kaemtz . When the attempt was made to apply statistics to weather - changes from day to day , it was found that average results were useless . The mean temperature for any particular day of the year might be 50 ...
... developed by Dové and Kaemtz . When the attempt was made to apply statistics to weather - changes from day to day , it was found that average results were useless . The mean temperature for any particular day of the year might be 50 ...
Сторінка 10
... develops all that was known before . On the one hand , the new method not only explains why certain prognostics are usually signs of good or bad weather , and the reason why the indications sometimes fail ; but also the reason why rain ...
... develops all that was known before . On the one hand , the new method not only explains why certain prognostics are usually signs of good or bad weather , and the reason why the indications sometimes fail ; but also the reason why rain ...
Сторінка 13
... develop- ment which has recently been made in the interpretation of their indications . So far , we shall confine our atten- tion to weather of the northern temperate zone only . This will take up about one - third of the work , and ...
... develop- ment which has recently been made in the interpretation of their indications . So far , we shall confine our atten- tion to weather of the northern temperate zone only . This will take up about one - third of the work , and ...
Сторінка 31
... developed till we come to our chapter on wind and calms . The weather in a cyclone is somewhat complicated . Some characteristic features depend on the position of the trough , and have nothing to do with the centre . For instance , the ...
... developed till we come to our chapter on wind and calms . The weather in a cyclone is somewhat complicated . Some characteristic features depend on the position of the trough , and have nothing to do with the centre . For instance , the ...
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Загальні терміни та фрази
appearance ascensional associated Atlantic atmosphere atmospheric circulation bad weather barogram barographic blow blue sky Britain called calm centre changes chapter circulation cirro-cumulus cirro-stratus cirrus cirrus-stripes cold cumulo-nimbus cumulus curve cyclones and anticyclones depression develop diagram direction diurnal variation east eddies England Europe explain Fahr fall festooned forecasting front gale give gradients gusts halo heat inch influence instance intensity isotherms latitude low pressure marked mercury meteogram meteorology millimetres monsoon motion moving nature nearly north-east north-west northern hemisphere observer pampero portion prognostics radiation rear reason rotation round secondary sequence of weather shapes of isobars showers sometimes south-east south-west squall station storm straight isobars strato-cumulus stratus striæ stripe suppose surface synoptic charts synoptic meteorology temperature thermal slope thermogram thunderstorms tion trace tropical cyclone tropics trough type of weather upper currents usually V-depression vapour veer velocity wedge Weilbach whole wind
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