东风带

The third wind belt develops as cold polar air sinks and moves south, is deflected to the right, and is therefore called the polar easterlies.

当冷的极地的空气下沉并且移动南方，受科氏力影响偏向右边，因此被称为极地东风带。

And the westward ISO is usually the low-frequency low and high pressure systems from the Bay of Alaska in northeastern Pacific and the Okhotsk in the northwestern Pacific of mid high latitudes, and the ISO evolving in subtropical easterlies.

进一步分析发现，经向风ISO的纬向传播对应着大气经向型环流系统的移动，向西传影响东亚夏季风区降水的ISO有来自低纬中东太平洋东风流中的低频气旋（如副热带东风带中ISO的演变）；也有来自中高纬度阿拉斯加湾及鄂霍次克海一带低频低压和高压(如阻塞高压和东北太平洋高压)的向南向西频散。

While not shown in CIRA-86, there is a clear easterly band extending from the equator to high latitudes at the altitude of lower thermosphere in autumn.

在冬季，东亚区域中间层西风急流中心位于25°N-35°N之间的75km高度，与CIRA-86相比，该中心纬度偏南5°，高度偏高10km；在秋季，东亚区域低热层高度存在一个显著的从赤道到高纬度的东风带，而CIRA-86不存在。

In the region, the winter mesospheric westerly jet lies at 75km altitude and in between 25°-35°N, which is 10km higher and 5°farther south in latitude that of the CIRA-86. While not shown in CTRA-86, there is a clear easterly band extending from the equator to high latitudes at the altitude of lower thermosphere in autumn.

在冬季，东亚区域中间层西风急流中心位于25°-35°N之间的75 km高度，与CIRA-86相比，该中心纬度偏南5°，高度偏高10km；在秋季，东亚区域低热层高度存在一个显著的从赤道到高纬度的东风带，而CIRA-86不存在。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。