 | 1861 - 500 стор.
...towards the pole of the hemisphere in which it is. While between the equator and the tropical calm belt, it is carried •westward by the general westward...the atmosphere there, but after passing the tropical calm belt, the general motion of the atmosphere carries it eastward, and hence the parabolic form of... | |
 | John Daniel Runkle - 1860 - 590 стор.
...towards the pole of the hemisphere in which it is. While between the equator and the tropical calm belt, it is carried westward by the general westward motion...the atmosphere there, but after passing the tropical calm belt, the general motion of the atmosphere carries it eastward, and hence the parabolic form of... | |
 | 1860 - 462 стор.
...towards the pole of the hemisphere in which it is. While between the equator and the tropical calm belt, it is carried westward by the general westward motion...the atmosphere there, but after passing the tropical calm belt, the general motion of the atmosphere carries it eastward, and hence the parabolic form of... | |
 | 1882 - 84 стор.
...and the contrary in the southern, must always gradually move towards the pole of the hemisphere in which it is. While it is between the equator and the...motions of the atmosphere, and of its gradual motion toward the pole. « - ihi« jnarnal. \m ' i. .in Journnl o ,] iMi'ond nerien. vol. i., rhart i. IV.... | |
 | 1861 - 968 стор.
...towards the pole of the hemisphere in which it is. While between the equator and the tropical calm belt, it is carried westward by the general westward motion...the atmosphere there, but after passing the tropical calm belt, the general motion of the atmosphere carries it eastward, and hence the parabolic form of... | |
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... considerable. Hence the interior and most violent portion of a cyclone, always gyrating from right to left in the northern hemisphere, and the contrary in the southern, must always gradually move towards the pole of the hemisphere in which it is.... 