Weather: A Popular Exposition of the Nature of Weather Changes from Day to DayD. Appleton, 1887 - 472 стор. |
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Сторінка 10
... trace the circulation and eddies of the atmosphere . By carrying the general laws of physics into the conception of a circulating gas , we find that a cold mixed atmosphere of air and vapour descending into a warmer soil would remain ...
... trace the circulation and eddies of the atmosphere . By carrying the general laws of physics into the conception of a circulating gas , we find that a cold mixed atmosphere of air and vapour descending into a warmer soil would remain ...
Сторінка 22
... tracing actual cases . It is so different looking at the " ups " and " downs " of the barometer when they are marked ... traces are called - and deductions from synoptic charts are 22 WEATHER .
... tracing actual cases . It is so different looking at the " ups " and " downs " of the barometer when they are marked ... traces are called - and deductions from synoptic charts are 22 WEATHER .
Сторінка 23
... traces are called - and deductions from synoptic charts are so apparently unconnected that they have hitherto been almost treated as different branches of meteorology . One main feature of this book will be our endeavour to collate ...
... traces are called - and deductions from synoptic charts are so apparently unconnected that they have hitherto been almost treated as different branches of meteorology . One main feature of this book will be our endeavour to collate ...
Сторінка 30
... trace at any one place , the ups " and " downs suggest the analogy of waves , so that the lowest part of a trace may be called a " trough . " Or we may look at the cyclone as a circular eddy , moving in a given direction , and so far ...
... trace at any one place , the ups " and " downs suggest the analogy of waves , so that the lowest part of a trace may be called a " trough . " Or we may look at the cyclone as a circular eddy , moving in a given direction , and so far ...
Сторінка 40
... manner from left to right . This inversion is obviously necessary , because the cyclone is moving from right to left . The upper line gives the trace which a self - recording barometer would have marked . In front 40 WEATHER .
... manner from left to right . This inversion is obviously necessary , because the cyclone is moving from right to left . The upper line gives the trace which a self - recording barometer would have marked . In front 40 WEATHER .
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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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