Weak vertical shear and warm sea surface are other reasons to remain the intensity of typhoon.
弱的垂直切变和暖洋面的存在也是台风强度维持的原因之一。
This is due to year-round warm sea surface temperatures, which keep the overlying atmosphere warm as well.
这主要是由于全年温暖的海洋表面温度,使整个环境都非常温暖。
Higher air temperatures can increase surface melting, but warm ocean currents accelerate ice loss more when glaciers flow into the sea.
气温升高能够加速冰川表面的融化,但是当冰川漂移入海之后,温暖的洋流对冰雪消融发挥了更重要的推动作用。
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