 Before storms they appear lower and denser, and usually in the quarter opposite to that from which the storm arises. Steady high winds are also pre. ceded and attended by streaks running quite across the sky, in the direction they blow in.  The Complete Weather Guide, &c - Page 31by Joseph Taylor - 1816Full view - About this book
 | 1805 - 948 pages
...usually in the quarter opposite to that from which the storm arises. Steady high winds are also preceded and attended by streaks running quite across the sky in the direction they blow in. " The relations of this modification with the state of the barometer, thermometer, hygrometer, and... | |
 | 1803 - 922 pages
...usually in the quarter opposite to that from which the storm arises. Steady high winds are also preceded and attended by streaks running quite across the sky in the direction they blow in. The relations of this modification with the state of the barometer, barometer, thermometer, hygrometer,... | |
 | Joseph Taylor - 1812 - 184 pages
...oblique cirrus, which frequently come on from the leeward, and the direction of their in. crease is (o the windward. Continued wet weather is attended with...of fine weather. 5. If the sky, after being for a Ipng time serene and blue, become fretted and spotted with small undulated clouds, not unlike the waves... | |
 | Joseph Taylor - 1813 - 264 pages
...usually in the quarter opposite to that from which the storm arises. Steady high winds are also preceded and attended by streaks running quite across the sky,...of wind. 4. If clouds appear gradually to diminish, grnd dissolve into the air, so as to become in. T;isiblc, it is an indication of fine weather. t 5.... | |
 | Andrew Ure - 1821 - 436 pages
...opposite to that from which the storm arises. Steady high winds are also preceded and attended by cirrus streaks, running quite across the sky in the direction they blow in. The cumulus has the densest structure, is formed in the lower atmosphere, and moves along with the... | |
 | George G. Carey - 1825 - 274 pages
...cirrostratus. quarter opposite to that from which the storm arises. Steady high winds are also preceded and attended by streaks running quite across the sky in the direction they blow in. The relations of this modification with the state of the barometer, thermometer, hygrometer, and electrometer,... | |
 | John Claudius Loudon - 1826 - 1252 pages
...opposite to that from which the storm antes. Steady high winds are also preceded and attended by cirrous streaks, running quite across the sky in the direction they blow in. 2ЯН. Thr cumulus has the densest structure, is formed in the tower atmosphere, and moves along with... | |
 | Thomas Curtis - 1829 - 828 pages
...opposite to that from which the storm arises. Steady high winds are also preceded and attended by cirrus streaks, running quite across the sky in the direction they blow in. The cvimulus has the densest structure, is formed in the lower atmosphere, and moves along with the... | |
 | Andrew Ure - 1831 - 980 pages
...opposite to that from which the 'storm arises. Steady high winds are also preceded and attended by cirrus streaks, running quite across the sky in the direction they blow in. The cumulus has the densest structure, is formed in the lower atmosphere, and moves along with the... | |
 | Luke Howard - 1833 - 462 pages
...usually in the quarter opposite to that from which the storm arises. Steady high winds are also preceded and attended by streaks running quite across the sky in the direction they blow in. OF THE CUMULUS. Clouds in this Modification are commonly of the most dense structure : they are formed... | |
| |
