 On either side of this zone and converging toward it are the trade winds, which blow from the northeast in the Northern Hemisphere and from the southeast in the Southern Hemisphere. The...  Complete Geography - Halaman 24oleh Henry Justin Roddy - 1902 - 166 halamanTampilan utuh - Tentang buku ini
 | 398 halaman
...revolutionary rapidity of the air-stream, the latter appears to have an opposite motion, and seems to blow from the north-east in the northern hemisphere, and from the south-east in the southern half of the earth. AVhile the cold currents from the poles are thus creating the tradewinds towards... | |
 | Joseph Dalton Hooker, Thomas Thomson - 1855 - 604 halaman
...its revolution round its own axis) is a maximum. They therefore lag behind, as it were, and appear to blow from the north-east in the northern hemisphere, and from the south-east in the southern hemisphere. The presence of land interferes with the regularity of the trade- winds; and where it occurs... | |
 | Joseph Dalton Hooker, Thomas Thomson - 1855 - 308 halaman
...its revolution round its own axis) is a maximum. They therefore lag behind, as it were, and appear to blow from the north-east in the northern hemisphere, and from the south-east in the southern hemisphere. The presence of land interferes with the regularity of the trade- winds; and where it occurs... | |
 | 1858 - 396 halaman
...revolutionary rapidity of the air-stream, the latter appears to have an opposite motion, and seems to blow from the north-east in the northern hemisphere, and from the south-east in the southern half of the earth. While the cold currents from the poles are thus creating the tradewinds towards... | |
 | Home tutor - 1862 - 532 halaman
...revolutionary rapidity of the air-stream, the latter appears to have an opposite motion, and seems to blow from the north-east in the northern hemisphere, and from the south-east in the southern half of the earth. While the cold currents from the poles are thus creating the trade winds towards... | |
 | 1867 - 632 halaman
...real course of nature. The streams in the upper half of the globe represent the trade winds, which blow from the north-east in the northern hemisphere, and from the south-east in the southern hemisphere of the globe. At the equator they are exactly opposed to one another, and blow due north... | |
 | Elias Loomis - 1868 - 326 halaman
...must be produced on the south side of the equator, and thus originates a system of currents flowing from the northeast in the northern hemisphere, and from the southeast in the southern hemisphere. 146. Upper Current in the Equatorial Regions. — The mean temperature of the surface air... | |
 | William Stanley Jevons - 1870 - 376 halaman
...then to blow from east to west. These tendencies are combined together, and cause the trade-winds to blow from the NorthEast in the northern hemisphere, and from the South-East in the southern hemisphere. The law according to which the temperature of the air is governed in any part of the earth... | |
 | WILLIAM BLASIUS - 1875 - 360 halaman
...suddenly but gradually over us, it will assume a westerly direction gradually, and appear thus to come from the north-east in the northern hemisphere and from the south-east in the southern hemisphere. The farther from the north it comes, the more easterly will it appear to us. If such a... | |
 | William Blasius - 1875 - 386 halaman
...suddenly but gradually over us, it will assume a westerly direction gradually, and appear thus to come from the north-east in the northern hemisphere and from the south-east in the southern hemisphere. The farther from the north it comes, the more easterly will it appear to us. If such a... | |
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