较薄的等温线使下面温暖的海水快速流转，从而加快冰融化。

A thinner isotherm allows faster turnover of warmer waters from below, which speeds ice-melt. The process is self-perpetuating: as ice melts, the ocean absorbs more heat and melts more ice, and so on.

youdao

如果要写出描述这条等温线的方程，它的压强和体积，就通过常数C相联系起来。

If you want to write a function that describes this line here, it's pressure as a function of volume related to each other with this constant.

youdao

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.

youdao

So there's going to be a line that's going to connect the initial point to the final point, and that line mathematically is not going to be the same as this one here.

连接绝热过程,初末态的曲线的方程，和等温线的方程,也不会相同。

麻省理工公开课 - 热力学与动力学课程节选

That's the isotherm here.

等温线的方程了。

麻省理工公开课 - 热力学与动力学课程节选

If you want to write a function that describes this line here, it's pressure as a function of volume related to each other with this constant.

如果要写出描述这条等温线的方程,它的压强和体积,就通过常数C相联系起来。

麻省理工公开课 - 热力学与动力学课程节选