...研究表明 [11] , 风、 浪、 流、 潮与近岸地形的耦 合作用形成了复杂的海滩-碎波带地形动力过程 (morphodynamic processes)和岸滩侵蚀方式, 愈趋近 岸滩, 近岸地形动力过程愈趋于复杂 位于内碎波 带和冲流带的前滨是砂质海岸侵蚀/ 堆积过程的主 要地...
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长周期动力地形模型是模拟长时间尺度地形演变过程的一种过程模型,其代表性输入条件是模型输入的一个关键问题。
The long-term morphodynamic model is used to simulate morphologic evolution process in a long time scale, its key is to define the model representative input condition.
本文在上海台风研究所无地形的业务数值予报模式中引入地形,用实际天气过程进行了地形动力效应的予报试验。
Orography is properly introduced in the operational numerical model of Shanghai Institute of Typhoon and some real synoptic weather processes are used to test the dynamic effects of orography.
毫无疑问,在层结流体中波和地形间相互作用的动力学过程要复杂的多。
There is no doubt that the dynamics between wave and topography interaction is considerably more complicated a stratified fluid.
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