A case study of a polar low development over the Barents Sea
A case study of a polar low development over the Barents Sea
复制标题
巴伦支海极地低压发展的案例研究
DOI：
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发表时间：
1985
期刊：
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通讯作者：
E. Rasmussen
中科院分区：
文献类型：
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作者：
E. Rasmussen
本文研究了挪威海和巴伦支海之间熊岛地区极地低压的发展。极地低压的发展，当上层冷芯涡从东北平流穿过冰边缘和极端的海面温度梯度在斯瓦尔巴德熊岛地区的区域。强对流被认为在高层低涡转变为近地面强度最大的极地低压的过程中起着重要的作用。DOI：10.1111/j.1600-0870.1985.tb00440.x
The development of a polar low in the Bear Island region between the Norwegian Sea and the Barents Sea is studied. The polar low develops when an upper-level cold core vortex from the northeast is advected across the ice edge and the region of extreme sea surface temperature gradients in the Svalbard–Bear Island region. Strong convection is believed to play an important role in the transformation of the upper-level vortex into a polar low with greatest intensity near the surface. DOI: 10.1111/j.1600-0870.1985.tb00440.x