一个坑道周围的等温线可以理解为原始温度场的叠加。
The geoisotherms around a gallery can be explained as a superposition of the original temperature field.
这两个平均温度场没有什么差异，除了右图等温线的坡度似乎略为大一些之外。
There is little difference between the two mean temperature fields, except that the slope of the isotherms appears to be somewhere greater in the right panel.
结果表明，高空急流区温度平流分布的不均匀性，会在急流附近等温线密集区边缘激发出空气垂直运动和湍流，引起飞机颠簸。
The results show that the inhomogeneous distribution of temperature advection in upper jet stream trigger vertical currents in the marginal area of upper jet stream and cause airplane turbulence.
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