1) slope current
倾斜流
2) slantwise convection
倾斜对流
1.
Studies of the formation and development mechanism of the slantwise convection are critical to forecasting and warning of severe weathers,such as frontal precipitation,rainstorm,blizzard,typhoon,squall line,burst cyclone and so on.
锋面降水、暴雨、暴雪、台风、飑线和爆发性气旋等灾害性天气的预报预警和倾斜对流发生发展机理的研究密切相关。
3) tilted flame plume profile
倾斜羽流
4) slant circulation
倾斜环流
1.
The results show that: The symmetrical instability does not have to be stirred by horizontal disturbance of correspondent scale of the symmetrical instability; the slant circulations, which are stirred by disturbances of different scales, have different specialties; there may be a minimum critical scale in symmetrical instability slant c.
结果表明:虽然对称不稳定是β-中尺度的不稳定,但其不一定必须由β-中尺度的扰动来激发;由不同水平尺度的扰动所激发的倾斜环流有不同的特点;对称不稳定倾斜环流可能存在最小临界尺度;对称不稳定的发展存在最优扰动水平尺度,而扰动的垂直尺度对于对称不稳定的发展影响不大。
5) Sloping frontal air velocity distribution
倾斜来流
6) NW-SE oriented jet axis
倾斜急流轴
补充资料：倾斜流
又称“坡面流”。由于风力、气压变化、降水或大量河水注入造成海面倾斜所引起的洋流。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条