Weather: A Popular Exposition of the Nature of Weather Changes from Day to DayD. Appleton, 1887 - 472 стор. |
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Сторінка xiv
... Intensity of type 371 Fluctuation 372 " " Persistence 99 : 372 Recurrence 375 93 Dependence " 9 : 375 Change دو : North - east monsoon : : 377 377 South - west monsoon 381 CHAPTER XIV . FORECASTING FOR SOLITARY OBSERVERS . Nature of the ...
... Intensity of type 371 Fluctuation 372 " " Persistence 99 : 372 Recurrence 375 93 Dependence " 9 : 375 Change دو : North - east monsoon : : 377 377 South - west monsoon 381 CHAPTER XIV . FORECASTING FOR SOLITARY OBSERVERS . Nature of the ...
Сторінка 29
... intensity of the weather . Hence , when we speak of a cyclone as being intense , we mean that it has steep isobars somewhere . The word " intensity " will occur very often in these pages , for when we come to talk about the general ...
... intensity of the weather . Hence , when we speak of a cyclone as being intense , we mean that it has steep isobars somewhere . The word " intensity " will occur very often in these pages , for when we come to talk about the general ...
Сторінка 46
... intensity in any form of atmospheric circulation ; and as simple cloud , moderate , and heavy rain are , as it were , three successive degrees of intensity , the thickness of the bars in the above diagram is proportional to the intensity ...
... intensity in any form of atmospheric circulation ; and as simple cloud , moderate , and heavy rain are , as it were , three successive degrees of intensity , the thickness of the bars in the above diagram is proportional to the intensity ...
Сторінка 125
... weather which are associated with it . The reader will now comprehend . what is meant by the centre , the trough , the front or rear , the intensity , the path , and the velocity of ( 125 ) Pressure over cyclones and anticyclones.
... weather which are associated with it . The reader will now comprehend . what is meant by the centre , the trough , the front or rear , the intensity , the path , and the velocity of ( 125 ) Pressure over cyclones and anticyclones.
Сторінка 126
... intensity in a cyclone . It is not difficult to conceive a cyclone which possessed so little intensity that it could only develop cloud in the centre . Then , if from any cause the intensity of the ascensional current could be increased ...
... intensity in a cyclone . It is not difficult to conceive a cyclone which possessed so little intensity that it could only develop cloud in the centre . Then , if from any cause the intensity of the ascensional current could be increased ...
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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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