冬季北太平洋风暴轴存在明显的年际、年代际差异。
In winter, the north Pacific storm track experience significant annual and decadal variability.
能量分析表明，斜压转换的正值中心位于风暴轴及其上游区域。
The energy budget analysis shows that the baroclinic conversions are positive over the storm tracks and their upstream regions.
利用观测资料分析了冬季太平洋海表温度异常对风暴轴和急流的影响。
Observational analysis is conducted of the effects of winter Pacific SSTA on the storm track and jet stream.
英国位于大西洋边缘，处于风暴轴的末端。所谓“风暴轴”，即海洋上暴风经过的相对狭长的地带。
Britain's position at the edge of the Atlantic places it at the end of a storm track - relatively narrow zones over oceans that storms travel down, driven by the prevailing winds.
英国位于大西洋边缘，处于风暴轴的末端。所谓“风暴轴”，即海洋上暴风经过的相对狭长的地带。
Britain's position at the edge of the Atlantic places it at the end of a storm track-relatively narrow zones over oceans that storms travel down, driven by the prevailing winds.
采用T＿21L＿5大气环流模式，详细探讨了冬季西北太平洋海表温度异常对太平洋风暴轴的影响。
The winter NW Pacific SSTA effect on the Pacific storm track is investigated in detailing the context of the T_21L_5 GCM.
根据风暴轴的变化规律，制定合理的航线对于保障我国航海作业、科学考察等海上事业也具有十分重要的意义。
Furthermore, according to the storm track variation, people may design more reasonable oceanic navigation route. Therefore, study of storm track is of great importance.
风暴轴与每日天气图上的气旋和反气旋路径紧密联系，对天气演变、天气预报和短期气候预测具有重要的指示意义。
Storm track is associated with tracks of cyclones and anticyclones in daily synoptic chart, thus it may impact weather change and short-term climate variation.
通过动三轴试验模拟波浪荷载作用下地基的变化情况，试验结果显示，沉箱的过度沉陷和侧移是由于强风暴使得软黏土强度弱化所致。
The results show that the excessive settlement and lateral movement of the caissons are due to the strength weakening of the soft clay during the strong storm, and also show that the ability of thes.
通过动三轴试验模拟波浪荷载作用下地基的变化情况，试验结果显示，沉箱的过度沉陷和侧移是由于强风暴使得软黏土强度弱化所致。
The test results reveal that the excessive settlement and lateral movement of the caissons are due to strength weakening of soft clay during the strong storm.
通过动三轴试验模拟波浪荷载作用下地基的变化情况，试验结果显示，沉箱的过度沉陷和侧移是由于强风暴使得软黏土强度弱化所致。
The test results reveal that the excessive settlement and lateral movement of the caissons are due to strength weakening of soft clay during the strong storm.
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