...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。
基于7581个网页-相关网页
anti-trade wind 反季候风
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
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
The trade wind is a kind of natural cold source in spring, autumn and winter.
新风在春、秋、冬季是一种天然的冷源。
I'm tireder than I have ever been, he thought, and now the trade wind is rising.
我从来没有这样疲乏过，他想，而现在刮起贸易风来了。
The trade wind cell is, on the average, confined to 30 degrees poleward of the equator.
平均来说，信风圈限于离赤道(向极地方向)30度的纬度带里。
应用推荐