Weather: A Popular Exposition of the Nature of Weather Changes from Day to DayD. Appleton, 1887 - 472 стор. |
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Сторінка 53
... practice by far the most frequently to the north . We have therefore selected such a one for the diagram of the wind and weather in an ideal wedge , which we give in Fig . 7. There the highest pressure is at the bottom of the diagram ...
... practice by far the most frequently to the north . We have therefore selected such a one for the diagram of the wind and weather in an ideal wedge , which we give in Fig . 7. There the highest pressure is at the bottom of the diagram ...
Сторінка 54
... practice the gradients are never steep , so the force of the wind rarely rises to above that of a pleasant breeze . The broad features of the cloud and weather in a wedge are written across the diagram ( Fig . 7 ) . In front we find ...
... practice the gradients are never steep , so the force of the wind rarely rises to above that of a pleasant breeze . The broad features of the cloud and weather in a wedge are written across the diagram ( Fig . 7 ) . In front we find ...
Сторінка 72
... practice stratus and cumulus are usually the lowest , the composites the middle , and cirrus the highest layer of cloud ; but no absolute level can be assigned to each stratum at any season , or in any country . For instance , cumulus ...
... practice stratus and cumulus are usually the lowest , the composites the middle , and cirrus the highest layer of cloud ; but no absolute level can be assigned to each stratum at any season , or in any country . For instance , cumulus ...
Сторінка 81
... practice this cloud is almost invariably produced in front of thunderstorms , and it is difficult to see how it can be formed otherwise than G by assuming the air to rise in a thin vertical CLOUDS AND CLOUD - PROGNOSTICS . 81 Minor ...
... practice this cloud is almost invariably produced in front of thunderstorms , and it is difficult to see how it can be formed otherwise than G by assuming the air to rise in a thin vertical CLOUDS AND CLOUD - PROGNOSTICS . 81 Minor ...
Сторінка 106
... of anticyclones in fine weather , and the same cloud which precedes a dangerous storm . In practice the surroundings are so different that the apparent similarity of names rarely misleads the most ordinary observer 106 WEATHER .
... of anticyclones in fine weather , and the same cloud which precedes a dangerous storm . In practice the surroundings are so different that the apparent similarity of names rarely misleads the most ordinary observer 106 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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