Handy Book of MeteorologyBlackwood and Sons, 1867 - 204 sider |
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Side 10
... Scotland Edinburgh Normal School , systematically trained the students to regular habits of meteorological observation . When the law of storms begins to be generally understood , and , as a consequence , the value of observations of ...
... Scotland Edinburgh Normal School , systematically trained the students to regular habits of meteorological observation . When the law of storms begins to be generally understood , and , as a consequence , the value of observations of ...
Side 28
... Scotland , and the south of Sweden , whence it proceeds in a north - easterly direction to Spitzbergen . The following mean annual pressures will show the nature of the depression : -Paris , 29.988 ; London , 29.956 ; Glasgow , 29.863 ...
... Scotland , and the south of Sweden , whence it proceeds in a north - easterly direction to Spitzbergen . The following mean annual pressures will show the nature of the depression : -Paris , 29.988 ; London , 29.956 ; Glasgow , 29.863 ...
Side 41
... Scotland in August 1860 was 549.4 , and in the same month of 1864 it was also 54o.4 ; but in 1860 the mean of the highest day temperatures was 60 ° .8 , whilst in 1864 it was 62 ° .5 . This higher day temperature in 1864 was the chief ...
... Scotland in August 1860 was 549.4 , and in the same month of 1864 it was also 54o.4 ; but in 1860 the mean of the highest day temperatures was 60 ° .8 , whilst in 1864 it was 62 ° .5 . This higher day temperature in 1864 was the chief ...
Side 43
... Scotland , whose temperature but barely exceeds the minimum heat required for the proper ripening of the staple objects of agriculture , the inquiry becomes invested with a peculiar interest , especially in examining places and ...
... Scotland , whose temperature but barely exceeds the minimum heat required for the proper ripening of the staple objects of agriculture , the inquiry becomes invested with a peculiar interest , especially in examining places and ...
Side 45
... Scotland , during the past nine years the temperature at three inches below the surface has fallen to 26 ° .5 in loose sandy soils , and at a depth of twelve inches the freezing point has only once been observed . But in clay soils , at ...
... Scotland , during the past nine years the temperature at three inches below the surface has fallen to 26 ° .5 in loose sandy soils , and at a depth of twelve inches the freezing point has only once been observed . But in clay soils , at ...
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America amount appear ascending atmosphere barometer becomes begins blow calm cause centre changes charts climate cloud coast cold column compared considerable continued countries course covered currents daily diminished direction earth east effect electricity equator Europe evaporation falls feet flow fogs follows force formed frequently give greater greatest heat height Hence higher hour humidity important inches increased indicate influence land latitudes least less light lines lower mass maximum mean mercury meteorological miles mist months mountains night observations occur ocean owing passed perature position pressure prevail produced quantity radiation rain rainfall range regarded regions rises round scale season seen side snow soil sometimes south-west space storm summer surface takes temperate temperature theory thermometers tion tube upwards vapour warm weather whole wind winter
Populære avsnitt
Side 149 - The Fatherhood of God, Considered in its General and Special Aspects, and particularly in relation to the Atonement, with a Review of Recent Speculations on the Subject.
Side 83 - That rises upward always higher, And onward drags a labouring breast, And topples round the dreary west, A looming bastion fringed with fire.
Side 150 - Atlas,' &c. &c. — There is no work of the kind in this or any other language, known to me, which comes so near my ideal of perfection in a school-book, on the important subject of which it treats. In arrangement, style, selection of matter, clearness, and thorough accuracy of statement, it is without a rival ; and knowing, as I do, the vast amount of labour and research you bestowed on its production. I trust it will be so appreciated as to insure, by an extensive sale, a well-merited reward. G....
Side 104 - N. NNE. NE. ENE. E. ESE. SE. SSE. S. SSW. SW. WSW. W. WNW. NW. NNW.
Side 70 - Are brought ; and feel by turns the bitter change Of fierce extremes, extremes by change more fierce, From beds of raging fire to starve in ice...
Side 147 - Stray Leaves from an Arctic Journal ; or, Eighteen Months in the Polar Regions in Search of Sir John Franklin's Expedition in 1850-51.
Side 79 - It remains for a short time when formed in the lower parts of the atmosphere and near other clouds, and longest when alone in the sky, and at a great height. When streaks of cirrus run quite across the sky in the direction in which a light wind happens to blow, the wind will probably...
Side 138 - Through the high wood echoing shrill; Sometime walking, not unseen, By hedge-row elms, on hillocks green, Right against the eastern gate Where the great Sun begins his state Robed in flames and amber light, The clouds in thousand liveries dight...
Side 150 - HANDY HORSE-BOOK; or, Practical Instructions in Riding, Driving, and the General Care and Management of Horses. By 'MAGENTA.
Side 4 - AM, when evaporation is most rapid, the vapour is accumulated or pent up in the lower stratum of the atmosphere, and being impeded in its ascent its elastic force is increased by the reaction, and the barometer consequently rises. When the air falls below the temperature of the dew-point, part of its moisture is deposited in dew, and since some time must elapse before the...