warm current

warm current的基本解释

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暧流, 热流, 暖流

与warm current相关的网络例句 [注：此内容来源于网络，仅供参考]

The wind forcing is the most important factor(80%) for generating the JB cyclonic gyre In addition the wind forcing drives the Liman Current and damos the East Korean warm Current in the Winter , and generates the UTB eddies along the Japan Nearshore Branch in all seasons .

风强迫是产生日本海盆气旋性式涡旋的最重要的因素(80％)。此外，风强迫在冬季驱动了Liman Cold Current流，抑制了东朝鲜暖流，并且在全年都产生UTB涡旋和沿着日本近岸分支的一些涡旋。

The wind forcing is the most important factor(80%) for generating the JB cyclonic gyre In addition the wind forcing drives the Liman Current and damos the East Korean warm Current in the Winter , and generates the UTB eddies al ong the Japan Nearshore Branch in all seasons .

风强迫是产生日本海盆气旋性式涡旋的最重要的因素(80％)。此外，风强迫在冬季驱动了Liman Cold Current流，抑制了东朝鲜暖流，并且在全年都产生UTB涡旋和沿着日本近岸分支的一些涡旋。

In this paper, a general description of circulation in the Japan Sea is made, some controversial issues including the origin and structure of the Tsushima Warm Current are summarized, and some scientific problems with the Japan Sea remain un solved, these problems include the long-term variations and variation causes of volume transport of the Tsushima Warm Current, the disappearance of the East Korean Warm Current and its mechanism, the transport path and affecting factors of the Japan Sea Proper Water, and the causes for some variations in the Japan Sea and their responses to the global changes.

概述了日本海环流状况，着重介绍了对马海峡、郁陵海盆环流情形和日本海特征水团；总结了目前仍存在的争议问题，如对马暖流源头、对马暖流空间结构等；指出了目前日本海尚待解决的科学问题，如对马暖流流量的长期变化及其原因、东韩暖流消失现象及其机制、日本海特征水的传播路径及其影响因素、日本海的某些变化产生原因及其与全球变化的响应等。

与warm current相关的网络解释 [注：此内容来源于网络，仅供参考]

precipitous sea：怒涛

鸟足[形]三角洲|bird-foot delta | 怒涛|precipitous sea | 暖流|warm current

cyphonautes larva：苔藓虫幼体

索饵洄游|feeding migration | 苔藓虫幼体|cyphonautes larva | 台湾暖流|Taiwan Warm Current

upwelling current：涌升流,上升流

upward current of air 上升气流 | upwelling current 涌升流,上升流 | warm current 暖流