风暴轴 meaning in Chinese

storm axis
storm track

Influence on northern pacific storm track of okhotsk sea ice during winter
冬季鄂霍次克海海冰对北太平洋风暴轴年际变化的影响
Based on the arctic sea ice concentration data and the ncep / ncar reanalysis data , the contemporaneous relationship of the winter sea ice in the sea of okhotsk and its adjacent sea areas with the northern pacific storm track is investigated by statistical analysis methods
摘要利用北极海冰密集度资料和ncep / ncar再分析资料，运用统计方法讨论了冬季鄂霍次克海及其邻近海区海冰异常与同期北太平洋风暴轴的联系。
It is found that the anomalous sea ice area over the southwest part of the sea of okhotsk , together with the associated northern pacific sst anomaly , can exert crucial influence on the variability in the vigor and nw - se extension ( contraction ) of the pacific storm track , while the sea ice area anomalies over the area of northeastern part of the sea of okhotsk and the gulf of shelikhow , together with its associated north pacific ssta , mainly impact the strength and south - north movement of the storm track
结果发现：冬季鄂霍次克海西南部海区海冰面积异常与北大平洋海温异常共同作用对北大平洋风暴轴在西北东南方向的伸缩及强度的年际变化有重要影响；鄂霍次克海东北部及舍列霍夫海海区海冰面积异常与海温异常的共同作用主要影响风暴轴的南北位移和强弱。