...影响深度不超过100m,深部洋流可达深海底 4,海水运动及地质作用-洋流 一,海洋环境的基本特征 1, 1,定期到来信风(trade wind)是引起表层洋流的主要原因 各种海水的温度差对表层洋流的形成有重要影响。
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trade wind inversion [气象] 信风逆温
trade wind climate 信风气候
trade wind front 信风锋
trade-wind zone 信风带
trade-wind desert 信风区沙漠 ; 信风沙漠
trade wind belt 信风带
trade wind current [海洋] 信风海流
N a wind blowing obliquely towards the equator either from the northeast in the N hemisphere or the southeast in the S hemisphere, approximately between latitudes 30° N and S, forming part of the planetary wind system 信风
Travel is on the slow side, despite the trade wind, but we are generally making some 40 miles a day.
尽管有贸易风,我们的航行缓慢,但一般说来我们每天能前进40英里。
It was due to this limitation that the great trade wind sailing routes around the world were developed centuries ago.
环球大航海的信风路线就是几百年前由于这种限制而建立的。
He's mad, "said Buckland in as low a voice as the northeast trade wind would allow."
“他疯了。”布克兰压低了嗓音说,那可是东北信风所能允许的最低的声音了。
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