< p >。事实上,许多飓风登陆。在一个海洋的世界里我可以看到三个命运发生:< / p > < ol > <李> < p >飓风消散由于动力特性或气候特征。< / p > < p >通过动力特性,我的意思是两个相互剪切的飓风或产生一个无法持续的环境。后者的一个例子是< a href = " https://www.alabamawx.com/?p = 174525 " rel = " noreferrer " >上升流< / >,生成水冷却器,削弱了飓风的能量。气候特征,可能阻止飓风发展下去可能是亚速尔高压。,有飓风似乎不去的地方。< / p > < p > < a href = " https://i.stack.imgur.com/hWF8P.png " rel = " noreferrer " > < img src = " https://i.stack.imgur.com/hWF8P.png " alt = "在这里输入图像描述" / > < / > < / p > < /李> <李> < p >飓风发生温带过渡。< / p > < p >通知在上图中,飓风就消失在两极附近吗?当他们接近两极,温差变大。最终他们不再像热带气旋/飓风(没有温差),而是像一个温带气旋(见< a href = " https://www.alabamawx.com/?p = 195936 " rel = " noreferrer " > < / >的联系一些差异)。 This process is called Extratropical transition. Chavas and Reed (2019)
While looking up papers for this question, I stumbled upon this paper. It implies that we would get longer lived hurricanes spreading the entire planet. I'd be a little skeptical of this result though, since it ignores the fact that the earth is heated unevenly, which drives most of the climate.
On a side note, such simulations do exist. These are called Aquaplanet simulations. Some studies I found include:
And for kicks and giggles, if you want to consider what the worst-case scenario for a hurricane could be, such a thing has been named a "Hypercane" (see here, too).