英语翻译After SW or W gales,a set towards the mouth of the Chann
英语翻译
After SW or W gales,a set towards the mouth of the Channel may be expected,at a rate depending on the locality,strength,and duration of the gale.In winter,sets of up to 1° knots are sometimes recorded,mainly in directions between ENE and SE,but the tidal streams are responsible for most of the water movement within the 200 m line.
Off the mouth of the Bay of Biscay the current is trending SE and S to form the beginning of the Portugal Current (2.15).A branch enters the bay and recurves W along the N coast of Spain,but over most of the bay the currents are highly variable with a tendency for directions between E and S to predominate.The speeds for the most part do not exceed I knot and very rarely reach 2 knots.
Following W or NW gales E-going sets occur off the N coast of Spain,sometimes attaining a rate of 3 knots off Bilbao and 4-5 knots at the head of the bay particularly when current and tidal stream are in the same direction.
The following brief account of ice in the North Atlantic Ocean is by no means comprehensive.
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After SW or W gales,a set towards the mouth of the Channel may be expected,at a rate depending on the locality,strength,and duration of the gale.In winter,sets of up to 1° knots are sometimes recorded,mainly in directions between ENE and SE,but the tidal streams are responsible for most of the water movement within the 200 m line.
Off the mouth of the Bay of Biscay the current is trending SE and S to form the beginning of the Portugal Current (2.15).A branch enters the bay and recurves W along the N coast of Spain,but over most of the bay the currents are highly variable with a tendency for directions between E and S to predominate.The speeds for the most part do not exceed I knot and very rarely reach 2 knots.
Following W or NW gales E-going sets occur off the N coast of Spain,sometimes attaining a rate of 3 knots off Bilbao and 4-5 knots at the head of the bay particularly when current and tidal stream are in the same direction.
The following brief account of ice in the North Atlantic Ocean is by no means comprehensive.
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在这股西南风或西风之后,预期又有一股大风吹向海峡口地区,它的速度主要受它持续的时间,位置,强度影响.在冬天,有时会记录到很多时速大于1海里的风,主要在东北偏东和西南方向,这潮水流主要受海水运动200米线内的影响.
Biscay湾口现时开始形成葡萄牙潮流((2.15),该潮流的倾向是东南部和南部.一个新水流进入海湾转向西班牙的西海岸和北海岸,但过了海湾后,现时水流方向改变了,主要趋向西部和南部.大部分地区的风速少于1海里,很少地区达到2海里.
随着西部或西北部大风在西班牙北海岸向东移,有时在Bilbao海岸录得3海里的速度,当潮流和水流同方向的时候,特别在海湾前部录得4-5海里的流速.
下面简要说明一下北大西洋的部分,不是全面报告.
Biscay湾口现时开始形成葡萄牙潮流((2.15),该潮流的倾向是东南部和南部.一个新水流进入海湾转向西班牙的西海岸和北海岸,但过了海湾后,现时水流方向改变了,主要趋向西部和南部.大部分地区的风速少于1海里,很少地区达到2海里.
随着西部或西北部大风在西班牙北海岸向东移,有时在Bilbao海岸录得3海里的速度,当潮流和水流同方向的时候,特别在海湾前部录得4-5海里的流速.
下面简要说明一下北大西洋的部分,不是全面报告.
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