• Finally we discuss the possible application of these results to typhoon intensity prediction.

    最后讨论这些结果台风强度预测方面可能应用

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  • Typhoon intensity is an exponent distribution in given restrained conditions when typhoon entropy has gotten maximum.

    给定约束条件下台风极大值时,台风强度一种指数分布

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  • The results show that typhoon intensity can have influence on the water vapor transport to mid-latitude area by the southeasterly jet on the east of the typhoon.

    低层水汽输送,造成中纬度暴雨水汽辐合和不稳定能量积聚,故槽前降雨强度与其南方台风东侧水汽输送有着相当密切的关系。

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  • As of March 29, 2010, the U.S. Navy's Joint Typhoon Warning Center forecast that the storm would maintain its current intensity for several hours before slowly dissipating.

    2010年3月29日,美国海军联合台风警报中心预报风暴继续维持现有强度小时,稍后将逐渐消失。

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  • Weak vertical shear and warm sea surface are other reasons to remain the intensity of typhoon.

    垂直切变和暖洋面的存在也是台风强度维持原因之一

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  • Tropical cyclone tracks and intensity change are two important aspects in typhoon forecast.

    热带气旋路径强度变化台风预测两个主要方面

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  • The output of sensitivity experiment of moist show that moist could exercise a great influence on typhoon center intensity, typhoon motion and precipitation.

    水汽敏感性试验结果表明,水汽的输送台风中心强度、台风的移动路径台风降水明显的影响

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  • The recurrence interval of typhoon is the average time interval of arising typhoon of some intensity in the future.

    台风重现未来某一强度台风出现平均时间间隔

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  • Since the 1990s, the physical mechanism of tropical cyclone intensity change has been a forward topic of typhoon dynamics.

    二十世纪九十年代以来热带气旋强度变化物理机制成为国际台风动力学一个研究热点。

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  • Peculiar in geographic position, Guangdong is subject to flood, drought and typhoon calamities with high frequency, wide ex-tent and great intensity, thus causing great losses.

    由于地理位置特殊广东省遭受水旱风灾频率范围广、强度、损失重。

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  • The result was compared with another typhoon (8406) whose early path and intensity were similar to 8509 but not developed when it entered the westerly belt.

    矢量散度、旋度特征锋生锋消现象的联系,并和台风前期路径及强度相似、但进入西风带后很快消失了的8406号台风的诊断结果进行了对比。

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  • The result was compared with another typhoon (8406) whose early path and intensity were similar to 8509 but not developed when it entered the westerly belt.

    矢量散度、旋度特征锋生锋消现象的联系,并和台风前期路径及强度相似、但进入西风带后很快消失了的8406号台风的诊断结果进行了对比。

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