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台湾海峡地区地面风场数值试验和数值模拟
引用本文:胡瑞金,刘秦玉.台湾海峡地区地面风场数值试验和数值模拟[J].中国海洋大学学报(自然科学版),1992(1).
作者姓名:胡瑞金  刘秦玉
作者单位:青岛海洋大学物理海洋与海洋气象系 (胡瑞金),青岛海洋大学物理海洋与海洋气象系(刘秦玉)
摘    要:利用修改的一层原始方程模式(Danard模式),对台湾海峡地区地面风场进行了数值试验和数值模拟。首先在一些理想情况下,研究了地面气压场、地形、摩擦和加热对地面风场的影响。指出:地面气压场决定了地面风场的基本分布;摩擦对海陆风速差异有重要作用;地形作用表现为弱的分流和阻流作用,加热作用使风场趋于紊乱。并在东北气流控制下的实际风场进行了数值模拟,效果良好。

关 键 词:台湾海峡  地面风场  数值试验

NUMERICAL EXPERIMENTS AND SIMULATIONS FOR THE SURFACE WINDS IN THE AREAS OF THE TAIWAN STRAIT
Hu Ruijin Liu Qinyu.NUMERICAL EXPERIMENTS AND SIMULATIONS FOR THE SURFACE WINDS IN THE AREAS OF THE TAIWAN STRAIT[J].Periodical of Ocean University of China,1992(1).
Authors:Hu Ruijin Liu Qinyu
Institution:Department of Physical Oceanology & Marine Meteorology
Abstract:In this paper,using a modified one-level primitive equation model ( the Danard model),some numerical experiments and numerical simulations for the surface winds in the areas of the Taiwn Strair are made First,we discuss the effects of many factors such as surface pressure fields,topography,friction and heating on the surface wind fields in some ideal cases It is shown that surface pressure fields determine the elementary distribution of the surface winds,friction has a very important impact on the variety between sea breeze and land breeze,the influence of ropgraphy is in the form of a weak airflow dctouring and blocking effect,and the wind fields become complex due to heating.Finally,we make a numerical simulation for a real wind which is controled by a northeastern airflow The results are satisfactory
Keywords:Triwan Strait  surface winds  numerical experiments
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