Weather: A Popular Exposition of the Nature of Weather Changes from Day to DayD. Appleton, 1887 - 472 стор. |
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Сторінка
... 107 Illustrations . 5s . LVIII . GEOGRAPHICAL and GEOLOGICAL DISTRIBU- TION of ANIMALS . By Prof. A. HEILPRIN . 58 . London : KEGAN PAUL , TRENCH , & CO . , 1 Paternoster Square . THE INTERNATIONAL SCIENTIFIC SERIES . VOL . LIX . α.
... 107 Illustrations . 5s . LVIII . GEOGRAPHICAL and GEOLOGICAL DISTRIBU- TION of ANIMALS . By Prof. A. HEILPRIN . 58 . London : KEGAN PAUL , TRENCH , & CO . , 1 Paternoster Square . THE INTERNATIONAL SCIENTIFIC SERIES . VOL . LIX . α.
Сторінка 4
... tion could be suggested why they did so ; neither could any reason be given why the same weather was not always preceded by the same signs . A halo sometimes precedes a storm ; why does it not always do so ? Why is rain sometimes ...
... tion could be suggested why they did so ; neither could any reason be given why the same weather was not always preceded by the same signs . A halo sometimes precedes a storm ; why does it not always do so ? Why is rain sometimes ...
Сторінка 13
... tion to weather of the northern temperate zone only . This will take up about one - third of the work , and exhaust the more popular portions of the subject . We shall then have to plunge more deeply into the details of isobars , and ...
... tion to weather of the northern temperate zone only . This will take up about one - third of the work , and exhaust the more popular portions of the subject . We shall then have to plunge more deeply into the details of isobars , and ...
Сторінка 29
... tion in front of the centre facing the direction towards which it moves is called its front , and the whole of this portion may obviously be divided into a right and left front . The other side of the centre is , of course , the rear of ...
... tion in front of the centre facing the direction towards which it moves is called its front , and the whole of this portion may obviously be divided into a right and left front . The other side of the centre is , of course , the rear of ...
Сторінка 70
... tion of the air in the different shapes of isobars . In the course of our remarks , we shall explain incidentally both the meaning and value of the older cloud - lore , and also the great development in the science of forecasting . 70 ...
... tion of the air in the different shapes of isobars . In the course of our remarks , we shall explain incidentally both the meaning and value of the older cloud - lore , and also the great development in the science of forecasting . 70 ...
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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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