Weather Charts and Storm WarningsHenry S. King & Company, 1876 - 158 pagini |
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Pagina 24
... small in comparison with the superficial extent of the area over which the storm is felt . Everyone knows that it is a common occurrence to see clouds at a moderate elevation either moving rapidly while calm 24 Weather Charts and Storm ...
... small in comparison with the superficial extent of the area over which the storm is felt . Everyone knows that it is a common occurrence to see clouds at a moderate elevation either moving rapidly while calm 24 Weather Charts and Storm ...
Pagina 25
... small waves , each with its own eddies and circulations , which are carried on with the stream . If we could look at the upper surface of the atmosphere , we should see much the same sort of conditions , except that what corresponds to ...
... small waves , each with its own eddies and circulations , which are carried on with the stream . If we could look at the upper surface of the atmosphere , we should see much the same sort of conditions , except that what corresponds to ...
Pagina 44
... difference between the extreme readings is less than half an inch , although the gradients for a short distance may be high . The small trace of truth which the scale lettering in 44 Weather Charts and Storm Warnings .
... difference between the extreme readings is less than half an inch , although the gradients for a short distance may be high . The small trace of truth which the scale lettering in 44 Weather Charts and Storm Warnings .
Pagina 45
Robert Henry Scott. The small trace of truth which the scale lettering in question contains is accounted for in the following way . On the average of a great many readings of the barome- ter , taken under various circumstances as regards ...
Robert Henry Scott. The small trace of truth which the scale lettering in question contains is accounted for in the following way . On the average of a great many readings of the barome- ter , taken under various circumstances as regards ...
Pagina 46
... smaller than anticyclonic , so that when the barometer is low there is a greater probability of a steep gradient , from adjacent higher readings , existing in the neighbourhood and causing high winds , than when the barometer is high ...
... smaller than anticyclonic , so that when the barometer is low there is a greater probability of a steep gradient , from adjacent higher readings , existing in the neighbourhood and causing high winds , than when the barometer is high ...
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Termeni și expresii frecvente
Aberdeen anticyclonic area of low Atlantic atmosphere barometer Beaufort scale Brest Cape Gris Nez centre changes Cheaper Edition Cloth clouds coast Crown 8vo cyclonic cyclonic area cyclonic disturbances cyclonic systems Daily Weather Report Demy 8vo depression direction Donaghadee east Easterly fact fall Fcap force Frontispiece gradients Henry hoisted Holyhead inch indication instance International Scientific Series Ireland islands isobars LL.D low pressure Meteorological Office motion of storms Noon North-west northern side northward Novel November 29 observations Observatory passing POEMS Portrait Post 8vo price 58 Prof Professor rain region Rochefort scale Scilly Scotland Second Edition SERMONS shown signal Skudesnaes Small crown 8vo Square crown 8vo stations storm warnings Stornoway Sumburgh Head telegraphic temperature thermometer Third Edition tion Translated University of Erlangen Valencia vapour tension veering velocity vols Volume WEATHER CHARTS Westerly ΙΟ ΟΙΟ
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