分析海浪方向谱的EEV方法的一种迭代形式

将Pawka为改进最大似然方法（MLM）而提出的迭代方案应用于扩展本征关方法（EEV），作为EEV的一种迭代形式（IEEV）。用模拟数据检验了IEEV的合理性，并与EEV作了比较。计算结果表明，IEEV的估计性状较EEV有改善。最后将IEEV及EEV用于分析仪器阵列的外海观测数据。     

正倒锥体结构上冰力谱分析实验研究

利用研制的新型非冻结可破碎合成模型冰材料，进行了冰排与正倒锥体结构物作用的物理模拟试验研究，试验中观察记录了冰排的破碎过程并测定了作用于锥体结构物上的冰力，通过快速傅立叶变换方法由所测得的冰力时程曲线得到冰力频谱，分析并讨论了冰排速度，本结构物的水线直径，锥角以及冰排弯曲破坏方向等对冰力频谱对冰力频谱因子的影响。     

Turbulent momentum and salt transport in the mixing zone of the Elbe estuary

Measurements in the mixing zone of the Elbe estuary were performed during three consecutive tidal cycles with three types of instruments—a moored tripod with velocity and temperature/conductivity/light attenuation sensors, a profiling sonde with similar sensors lowered from an anchored vessel, and instrumented moorings. Acoustic-travel-time sensors were used for velocity measurements.Spectral analysis of 12·8 min pieces of the obtained time series gives results that are consistent with isotropic turbulence for part of the frequency space. Temporal changes of turbulent kinetic energy are correlated with tidal current velocity. A retardation is found between changes in tidal current and turbulent energy. Not all shear stress terms are in similar phase with tidal flow. Mean gradients, Reynolds stress terms, and turbulent salt flux terms are combined to determine eddy viscosity and eddy diffusion coefficients.     

长江中下游地区7500—5000aB.P.气候变化序列的初步研究

孢粉分析方法可以比较客观地反映古植被类型,而各植被类型只能在一定的气候指标范围内生长。本文根据这一基本原理,利用现代植被生长的基本气候指标和有关气象资料,对长江中下游地区7500—5000aB.P.的孢粉资料进行处理、转化,从而得出这一阶段每500年一个时间段的气候变化序列。研究结果表明,研究区在7500—5000aB.P.时间内,年平均温度偏暖于今日-0.1—1.5℃,最高温出现在6500—6000aB.P.,气温高于现在1.5℃。     

太湖北岸风浪谱的特征分析

利用１９９２年在太湖北岸马迹山地区测得的浅水风风浪资料，采用ＦＦＴ方法求算风浪频谱，对谱结构特征的分析表明，观测到的风浪谱在平衡范围谱值按－４．０幂指数衰减，风浪谱形状与文圣常给出的理论结果比较接近。另外，分析以风要素为参量得到的无因次化频谱可以看出，观测谱基本满足谱的相似律。     

水下压力阵列的测波方法

本文介绍了ＨＤＬ—２１７６底压式测波仪的基本特性，给出了水下压力阵列进行波浪方向谱估计的数据计算方法。     

Verification of linear theory for particle velocities in wind waves based on field measurements

Analyses are presented of field measurements of spectral transfer functions between surface elevation and subsurface three-dimensional particle velocity in wind-generated waves, in conditions ranging from young seas to old swells. The results are in agreement with the linear theory predictions to within the measurement error margin, which is estimated to be ± 5% for the gain functions and ± 4° in phase as far as the possible systemic errors are concerned. No correlation is found of the degree of agreement between measurements and linear theory with wave age or wave sleepness.     

深水风浪相关函数的研究

本文以风浪频谱和其相关函数的关系为基础,应用积分中值定理,给出了风浪相关函数的理论模型。进而以文氏等人的理论风浪频谱为原型,通过数值积分和待定系数法,给出了以风浪频谱的零阶矩m_0、峰频率ω_0和峰度因子P为参数的深水风浪相关函数式。最后把该式与数值计算值、实测值作了对比,证明本文所提出的深水风浪相关函数式较好地反映了各种不同成长状态的实际的相关函数。