APPLIED STUDY ON ATMOSPHERE-OCEAN-WAVE COUPLED MODEL IN SOUTH CHINA SEA

Based on MM5,POM,and WW3,a regional atmosphere-ocean-wave coupled system is developed in this work under the environment of Message Passing Interface.The coupled system is applied in a study of two typhoon processes in the South China Sea(SCS).The results show that the coupled model operates steadily and efficiently and exhibits good capability in simulating typhoon processes.It improves the simulation accuracy of the track and intensity of the typhoon.The response of ocean surface to the typhoon is remarkable,especially on the right side of the typhoon track.The sea surface temperature(SST)declines,and the ocean current and wave height are intensified.In the coupling experiment,the decline of SST intensifies and the inertial oscillation amplitude of the ocean current increases when the ocean-wave effect is considered.Therefore,the atmosphere-ocean-wave coupled system can help in the study of air-sea interaction and improve the capability of predicting and preventing weather and oceanic disasters in SCS.     

Dynamic Linkage between the North Pacific and the Tropical Pacific: Atmosphere-Ocean Coupling

In this study, dynamic linkage of atmosphere-ocean coupling between the North Pacific and the tropical Pacific was demonstrated using a large number of ensemble perturbed initial condition experiments in a fully coupled fast ocean-atmosphere model (FOAM). In the FOAM model, an idealized mixed layer warming was initiated in the Kuroshio-Oyashio extension region, while the ocean and atmosphere remained fully coupled both locally and elsewhere. The modeling results show that the warm anomalies are associated with anomalous cyclonic winds, which induce initial warming anomalies extending downstream in the following winter. Then, the downstream warming spreads southwestward and induces SST warming in the equatorial Pacific via surface wind-evaporation-SST feedback. Warming in the tropical Pacific is further reinforced by Bjerknes’ feedback.     

Evaluation of the Ocean Feedback on Height Characteristics of the Tropical Cyclone Boundary Layer

In this study, the interaction between the tropical cyclone（TC） and the underlying ocean is reproduced by using a coupled atmosphere-ocean model. Based on the simulation results, characteristics of the TC boundary layer depth are investigated in terms of three commonly used definitions, i.e., the height of the mixed layer depth（HVTH）, the height of the maximum tangential winds（HTAN）, and the inflow layer depth（HRAD）. The symmetric height of the boundary layer is shown to be cut down by the ocean response, with the decrease of HVTH slightly smaller than that of HTAN and HRAD. The ocean feedback also leads to evident changes in asymmetric features of the boundary layer depth. The HVTH in the right rear of the TC is significantly diminished due to presence of the cold wake, while the changes of HVTH in other regions are rather small. The decreased surface virtual potential temperature by the cold wake is identified to be dominant in the asymmetric changes in HVTH. The impacts of ocean response on the asymmetric distributions of HTAN are nonetheless not distinct, which is attributed to the highly axisymmetric property of tangential winds. The HRAD possesses remarkable asymmetric features and the inflow layer does not exist in all regions, an indication of the inadequacy of the definition based on symmetric inflow layer depth. Under influences of the cold wake, the peak inflow area rotates counterclockwise distinctly. As a consequence, the HRAD becomes deeper in the east while shallower in the west of the TC.     

海洋对大气反馈的研究进展及其诊断方法讨论

回顾了近10 a海洋对大气反馈作用的研究进展,讨论待解决的一个关键问题——怎样在观测研究中有效分离不同海区对大气异常的独立贡献.一般常用方法为利用线性回归或偏相关方法扣除外来主要干扰因子(事先已知),但该方法对解决外来未知海区影响有很大的局限性.广义平衡反馈分析方法(generalized equilibrium feedback assessment,GEFA)可以避免传统方法受未知海区影响的困扰,自动把各海区对大气异常的单独贡献分离出来.它的有效性在简单模式和观测分析中得到了初步验证.GEFA为提高海洋对大气反馈作用的认识提供了一种简单有效的统计工具.     

瞬变电磁法圆形线圈自感计算

在瞬变电磁法（TEM）中,圆形回线的自感参数用于局部导体晚期瞬变电磁场的等效计算、接收线圈固有过渡过程计算、关断时间的计算以及瞬变电磁仪器研制等。目前,在瞬变电磁法教科书中,圆形线圈自感计算均使用近似公式。这里根据毕奥-萨伐尔定律推导出单匝圆形线圈磁感应强度及自感的积分表达式,利用MATLAB软件进行数值计算。结果表明,目前使用的自感近似公式,在用于计算半径为0.5 m和1 m的圆形接收回线自感时,误差分别为-18.978%和-26.542%。用于计算发射回线的自感时,当回线半径从2.821 0 m～112.837 9 m时,自感近似公式的误差从-35.84%～-55.65%,且单匝正方形回线与等面积单匝圆形回线的自感值之间存在5.12%～8.11%的偏差。     

带反馈优先的M/M/c排队在通信网络中的应用

在具有Bernoulli反馈的单队列单服务台排队模型的基础上，考虑通信网络中赋予反馈信元优先权的情况，将单个服务台推广到多个服务台，建立了具有反馈优先的M／M／c排队模型．在该排队模型中，信元的到达遵循泊松过程，服务时间服从指数分布，通过构造拟生灭过程和运用谱展开方法给出了平稳队长分布的算法，具体给出了C=2时平稳队长分布的显式表达式，以及在反馈优先和反馈非优先两种策略下的排队指标，并作出了相应的指标性能分析，得出信元在反馈优先策略下的平均逗留时间较短，进而说明了该排队模型在通信网络中有广泛的应用价值。     

改进型GA算法在大气环境质量评价中的应用

为了建立一种对多项指标都能普遍适用的大气环境质量评价模型，利用反馈式突变进化算法对幂函数加和型指数评价公式中参数进行优化，并用优化后的综合评价指数公式对大气环境进行综合评价。通过对武汉市大气环境质量状况的评价实例研究，表明了综合指数公式的实用性和可行性。     

盘状星系形成中的角动量问题

目前的星系形成理论认为，盘状星系由暗晕中的重子物质冷却并坍缩而成。在这一演化图像中，重子物质的角动量及其分布起着关键作用，它直接决定了盘状星系的结构。然而，在盘状星系形成和演化的各种解析、半解析模型及数值模拟中，出现了一系列与角动量有关的问题。其中包括角动量灾变(angular momentum catastrophe)及角动量分布不匹配(mismatch of angulamomentum profile)等。近年来，为解决此类问题，人们进行了大量的研究，引入并建立了各种机制和模型。详细表述了星系形成与演化中两类主要的角动量问题，并系统地综述了目前针对此类问题所提出的各种可能的解决方法和途径。     

一种基于ABEL-HDL语言的反馈算法在PLD设计中的应用

介绍了一种在PLD(可编程逻辑器件)设计中引入原本用在模拟电子系统中反馈的概念,利用输出信号来控制输入信号,从而得到最小的系统时延的反馈算法,使器件性能得到最大优化.     

瞬变电磁测深快速拟地震解释方法及应用效果

详细讨论了电磁波与地震波在介质中的传播规律.根据瞬变电磁测深(TEMS)中心回线装置观测成果与大地电磁测深(MTS)成果的一致性,提出了瞬变电磁资料拟地震解释的思路.大量理论模型的正、反演计算结果表明方法理论是正确的,野外实测资料处理结果进一步说明了该方法的实用性.