upwell [ʌp'wel]

upwell的基本解释

vi.

(水等)上涌

与upwell相关的网络例句 [注：此内容来源于网络，仅供参考]

When surface waters are cold, deeper depths are allowed to upwell, bringing these essential nutrients toward the surface where the phytoplankton may use them.

当海水表面温度下降时，较深一些的海水就会上浮，同时把这些必须营养成分带到水面处，供生活在那里的浮游植物生长的需要。

The upwell ing brings the thermocline—the boundary layer between deep, cold water and the warm water of the surface—up as high as 30 feet from the top.

上升流使得局部温越层(深处的冰冷海水和表面的温暖海水交界处的水层)可鼓出10米之高。

However, when surface waters are warm (as during an El Ni?o), they do not allow the colder, deeper currents to upwell and effectively block the flow of life-sustaining nutrients.

可是，如果海面水温较高，深层海水就无法上流，从而大大阻断了这些生命必须营养的正常循环。

There are high-velocity density layers in the lower crust, which would be represent crust-mantle mixing layer formed by mantle material upwell The model of lithosphere subduction and underplating of mafic magma is supported by all geophysic data

在下地壳下部存在高速致密物质层，可能代表了上地幔物质上涌形成的壳-幔混合层，上述地球物理资料均支持岩石圈消减作用和玄武岩浆底侵作用。

Cloud-like lower velocity materials in upper mantle upwell from depth of 150km, and flow along mantle weak zones at about 60～130km Upwelling of lower velocity materials are most obvious along the Tan-Lu faults and Yanshan area.

从地幔内低速体的宏观形态上看，呈现"蘑菇云状"，好象是低速体从150km深度以下沿幔内薄物带呈不规则柱状体上升，并在65-130km处向四周平流延展所致，而郯庐断裂带以及太行山以东的燕山地区附近，低速体的上升最为明显。

与upwell相关的网络解释 [注：此内容来源于网络，仅供参考]

upwell：向上流

upwarping /向上挠曲/ | upwell /向上流/ | upwind /逆风地/