Weather: A Popular Exposition of the Nature of Weather Changes from Day to DayD. Appleton, 1887 - 472 стор. |
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Сторінка 8
... position of the nearest area of low pressure . 3. That the velocity of the wind was always nearly proportional to the closeness of the isobars . 4. That the weather - that is to say , the kind of cloud , rain , fog , etc. — at any ...
... position of the nearest area of low pressure . 3. That the velocity of the wind was always nearly proportional to the closeness of the isobars . 4. That the weather - that is to say , the kind of cloud , rain , fog , etc. — at any ...
Сторінка 22
... position of the areas of high and low pressure have considerably changed , and with them the positions of those areas where the weather is good or bad . For instance , suppose that at 8 a.m. on one morning we find pressure low over ...
... position of the areas of high and low pressure have considerably changed , and with them the positions of those areas where the weather is good or bad . For instance , suppose that at 8 a.m. on one morning we find pressure low over ...
Сторінка 23
... position of the nearest area if low pressure . 3. That the velocity of the wind is always nearly pro- portional to the closeness of the isobars . 4. That the weather - that is to say , the kind of cloud , rain , fog , etc. — at any ...
... position of the nearest area if low pressure . 3. That the velocity of the wind is always nearly pro- portional to the closeness of the isobars . 4. That the weather - that is to say , the kind of cloud , rain , fog , etc. — at any ...
Сторінка 24
... position , so that changes of weather were caused by the drifting past of these areas of good or bad weather , just as on a small scale rain falls as a squall drives by . The motion of these areas was found to follow certain laws , so ...
... position , so that changes of weather were caused by the drifting past of these areas of good or bad weather , just as on a small scale rain falls as a squall drives by . The motion of these areas was found to follow certain laws , so ...
Сторінка 31
... characteristic features depend on the position of the trough , and have nothing to do with the centre . For instance , the weather and sky over the whole front of the cyclone — that is , all that lies in front WEATHER - PROGNOSTICS . 31.
... characteristic features depend on the position of the trough , and have nothing to do with the centre . For instance , the weather and sky over the whole front of the cyclone — that is , all that lies in front WEATHER - PROGNOSTICS . 31.
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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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