Term 术语 Definition 定义
current: gradient
梯度流
A current due to the horizontal component of the hydrostatic pressure gradient.
由于流体静压力梯度水平分量的作用而产生的水流。
current: mixed
混合潮流
The type of TIDAL CURRENT characterized by a con­spicuous difference in SPEED and duration between the two FLOOD CURRENTS or two EBB CURREN... more
The type of TIDAL CURRENT characterized by a con­spicuous difference in SPEED and duration between the two FLOOD CURRENTS or two EBB CURRENTS occurring each TIDAL DAY.
每个潮汐日出现的两次涨潮或落潮之间,在速度和持续时间上存在明显差别的潮流。
current: nontidal
非潮汐流
Any CURRENT that is caused by other than TIDE PRODUCING FORCES. See also STREAM.
非引潮力引起的海流。亦见stream(水流)。
current: ocean/sea
洋流/海流
A movement of ocean water characterized by regularity, either of a cyclic nature or as a continuous STREAM flowing along a definable PATH.
具周期性规律特点或沿确定路线持续流动的海水运动。
current: periodic
周期电流
An oscillating CURRENT the values of which recur at somewhat regular intervals.
电流值以规律间隔重现的振荡电流。
current: permanent
稳定海流,恒流
A CURRENT which continues with relatively little periodic or seasonal change.
周期性或季节性变化相对较小的海流。
current: rectilinear
往复(潮)流,直线电流
See CURRENT: REVERSING.
参见reversing current(往复流)。
current: residual
剩余电流,残流,余流
The mean CURRENT without periodic components.
没有周期分量的平均流。
current: reversing
往复流
A TIDAL CURRENT which flows alternately in approximately opposite directions, with SLACK WATER at each reversal. Such CURRENTS occur princip... more
A TIDAL CURRENT which flows alternately in approximately opposite directions, with SLACK WATER at each reversal. Such CURRENTS occur principally in areas where motion is largely restricted to relatively narrow CHANNELS. Also called rectilinear current or rectilinear stream.
潮流的一种。这种潮流大致互成相反方向交替流动,转流时憩流。这种流主要发生在水流运动基本被限制... more
潮流的一种。这种潮流大致互成相反方向交替流动,转流时憩流。这种流主要发生在水流运动基本被限制在相对狭窄水道内的区域。亦称rectilinear current(往复流) 或 rectilinear stream(直线流)。
current: rip
回流,离岸流,激流
The return flow of water piled up on SHORE by incoming WAVES and WIND.
受风浪作用冲上海岸的海水的回流。
current: rotary
回转潮流
A TIDAL CURRENT that flows continually, with the direction of FLOW changing through 360° during a TIDAL CYCLE. Called rotary stream in Brit... more
A TIDAL CURRENT that flows continually, with the direction of FLOW changing through 360° during a TIDAL CYCLE. Called rotary stream in British terminology.
在一次潮汐周期中流向变化360°的一种连续潮流。英国术语称之为rotary stream。
current: seasonal
季节性海流流,季凤流
A CURRENT which has large changes in SPEED or direction due to seasonal WINDS.
由季风引起的一种速度或方向变化很大的海流。
current: semidiurnal
半日潮流
The type of TIDAL CURRENT having two flood and two ebb periods of nearly the same duration during a TIDAL DAY.
潮流的一种。这种潮流在一个潮日的两次涨潮和两次落潮所持续的时间几乎相同。
current: stream
海洋急流
A narrow, deep, and fast-moving CURRENT as opposed to a relatively wide and weak DRIFT CURRENT.
相对于较宽而弱的漂移水流而言,是一个狭窄的、深的并快速移动的水流。
current: subsurface
次表层流
A CURRENT usually flowing below the THERMOCLINE generally at slower SPEEDS and frequently in a different direction from the CURRENTS near th... more
A CURRENT usually flowing below the THERMOCLINE generally at slower SPEEDS and frequently in a different direction from the CURRENTS near the surface.
通常在温跃层下流动的海流。这种海流一般流速较慢,流向通常与接近海面的海流不同。
current: surface
表层流
A CURRENT that does not extend more than a few (2-3) METRES below the surface.
离水面不超过2-3米的海流。
current: surge
浪涌海流
The coastal CURRENT influenced by remote waves.
被遥远的波浪所影响的沿海海流。
current(s): telluric
NULL
Natural electric currents that flow on or near the EARTH's surface in large sheets. Also called earth current.
NULL
current: tidal
潮(汐)流
The alternating horizontal movement of water associated with the RISE and fall of the TIDE caused by TIDE-PRODUCING FORCES. Also called tida... more
The alternating horizontal movement of water associated with the RISE and fall of the TIDE caused by TIDE-PRODUCING FORCES. Also called tidal stream.
海水在引潮力的作用下伴随落潮所产生的交替水平运动。亦称tidal stream。
current: turbidity
浑浊流
A highly turbid, relatively dense CURRENT carrying large quantities of CLAY, SILT and SAND in suspension which flows down a submarine SLOPE ... more
A highly turbid, relatively dense CURRENT carrying large quantities of CLAY, SILT and SAND in suspension which flows down a submarine SLOPE through less dense SEA WATER.
携带着大量悬浮粘土、泥沙的一种密度较大非常浑浊的海流。它沿水下斜坡穿过密度较小的海水向下流动... more
携带着大量悬浮粘土、泥沙的一种密度较大非常浑浊的海流。它沿水下斜坡穿过密度较小的海水向下流动。