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本文对1982年以来我国东部海域登陆再发展台风进行统计分析,选取其中15个个例进行对比分析,根据其移动路径和增强幅度分为3类,研究表明:台风如果移向东北方向则再发展较弱,而向北移动则发展较深,且向北越深发展越强,这与副热带高压(副高)的位置和强度以及上游高空槽存在一定的关系(整体偏向于正相关),在北上的过程中,如果与高空正位涡发生耦合,则增强越大,但非绝热加热所占的比重越小。同时动能收支分布显示,台风加强越深,动能转换越强,两者成正比,但在能量转化的方向和位置上,三者又存在差异。 相似文献
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The Webb-Resio-Tracy (WRT) method for exact computation of the non-linear energy transfer rate was implemented in MASNUM-WAM, which is a third-generation wave model solving the discrete spectral balance equation. In this paper, we describe the transformation of the spectral space in the original WRT method. Four numerical procedures were developed in which the acceleration techniques in the original WRT method, such as geometric scaling, pre-calculating, and grid-searching, are all reorganized. A series of numerical experiments including two simulations based on real data were performed. The availability of such implementation in both serial and parallel versions of the wave model was proved, and a comparison of computation times showed that some of the developed procedures provided good efficacy. With exact computation of non-linear energy transfer, MASNUM-WAM now can be used to perform numerical experiments for research purposes, which augurs well for further developments of the model. 相似文献
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Temporal variations in multimodal structures of diurnal (D 1) and semidiurnal (D 2) internal tides were investigated on the continental slope of the Dongsha Plateau, based on 2-month moored acoustic Doppler current profiler observations. Harmonic analysis indicated that the D 1 components (K 1 and O 1) dominated the internal tide field. The vertical structure of the K 1 constituent presented a first-mode structure while the M 2 constituent seemed to exhibit a high-mode structure. Amplitude spectra analysis of the current data revealed differences in baroclinic current amplitudes between different water depths. Temporal variations in modal structures ware analyzed, based on the D 1 and D 2 baroclinic tides extracted from the baroclinic velocity field with band-pass filters. Analysis showed that the magnitude of the D 1 internal tide current was much larger than the D 2 current, and temporal variations in the modal structure of the D 1 internal tide occurred on an approximately fortnightly cycle. The EOF analyses revealed temporal transformation of multimodal structures for D 1 and D 2 internal tides. The enhancement of the D 1 internal tide was mainly due to the superposition of K 1 and O 1, according to the temporal variation of coherent kinetic energy. 相似文献
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根据龙口海洋站观测得到的2007年逐时10分钟平均风速、风向资料,对平均风速风向、大风风速风向、大风日数等方面进行了分析,得出结论:龙口海洋站的风具有典型的季风性气候特征,冬夏季主风向有180°的变化,平均风速的月际变化出现两峰两谷的趋势;常风向为S向和NE向,强风向为偏北向;偏东风的平均风速和出现频率最小;大风风力以6级为主,大风的年平均风速为13.3 m/s,出现大风的月最高概率为63.3%;大风年主导风向为NW-NE以及S,风速以偏北大风较大,偏东风最小;秋冬季节以偏北大风为主,春季偏南大风与偏北大风交替出现,夏季是大风最少的季节。 相似文献
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