自然界各种物体,都有表征其自然属性的光谱特性。地物的光谱特性是遥感图象定性判读的依据之一,它作为一种遥感信息也直接用于定量测定和制图。
海水中悬浮物质的数量和性质影响海水的颜色和海水的光谱特性。反之,根据海水的光谱特性可以测定水中悬浮物质的数量和性质。1974年, S. D. Duntley首先从海洋叶绿素的光谱效应,提出根据海水的光谱反射率曲线,用卫星传感器测定水中叶绿素a 浓度的理论。1978年, R. W. Johnson 建立了航空遥感的光谱数据与沿岸带海洋叶绿素a 浓度之间的数学关系,并绘制了叶绿素a的分布图。1979年, R. W. Johnson建立了光谱数据与悬浮泥沙含量之间的数学关系,并绘制了悬浮泥沙的定量分布图,等等。本文的目的即是要建立一种方法,用国产101W光谱辐射计记录的遥感数据,计算海域悬浮泥沙、叶绿素a 浓度、水色等水质参数。
1980年5月16日至19日,由中国科学院组织,有中国科学院海洋研究所、国家海洋局第一海洋研究所、第二海洋研究所、交通部天津水运科学研究所、水利部天津水利科学研究所等单位参加,在天津塘沽的海河和蓟运河口进行津、渤地区第一次环境污染航空遥感监测联合试验。在此次试验中用机载101W光谱辐射计记录海水的光谱辐射曲线,作者以此计算海水的光谱反射率曲线,用逐次回归分析法建立海洋实测数据(悬浮泥沙、叶绿素a浓度、水色等)与海水光谱反射率数据之间的数学关系。实验基本是成功的,由回归方程计算的结果与海洋实测数据之间的相关系数约为0.7。如果对研究海域的每一个子域的辐射值作光谱扫瞄,作出定量的分布图也是可行的。 相似文献
Presented here is a compact explicit difference scheme of high accuracy for solving the extended Boussinesq equations.For time discretization,a three-stage explicit Runge-Kutta method with TVD property is used at predicting stage,a cubic spline function is adopted at correcting stage,which made the time discretization accuracy up to fourth order;For spatial discretization,a three-point explicit compact difference scheme with arbitrary order accuracy is employed.The extended Boussinesq equations derived by Beji and Nadaoka are solved by the proposed scheme.The numerical results agree well with the experimental data.At the same time,the comparisons of the two numerical results between the present scheme and low accuracy difference method are made,which further show the necessity of using high accuracy scheme to solve the extended Boussinesq equations.As a valid sample,the wave propagation on the rectangular step is formulated by the present scheme,the modelled results are in better agreement with the experimental data than those of Kittitanasuan. 相似文献
In this paper, the method of operator splitte is applied to simulate the tidal flow in the Hang-zhou Bay. Different schemes of splitting have been devised and compared.Results of the study indicate that good simulation can be achieved. Besides being simpler in form, this method is flexible and allows much freedom in selecting the mode of splitting and the scheme of computation. 相似文献
This paper presents a numerical model study of the propagation of water waves using the parabolic approximation of the mild-slope equation in the orthogonal coordinate system. Two types of coordinate systems are studied: (a) a general form of orthogonal coordinate system and (b) the conformal system, a special form of orthogonal coordinate system. Two typical examples, namely, expanded breakwaters and a circular channel, are studied to validate the model. First, the examples are studied by use of the general orthogonal coordinates. Then the same examples are computed by use of the confonnal system. The computational results show that the confonnal coordinate system generally gives better predictions than the general orthogonal system. A numerical technique for generating the conformal grid is combined with the numerical model to improve the practicability of the model. The comparison between the result from the numerical grid system and that from the analytical grid system shows that reliable computational results can be obtained by use of the numerical confonnal grid system. 相似文献
Data are presented indicating the complexity and highly variable response of beaches to cold front passages along the northern Gulf of Mexico, in addition to the impacts of tropical cyclones and winter storms. Within the past decade, an increase in the frequency of tropical storms and hurricanes impacting the northern Gulf has dramatically altered the long-term equilibrium of a large portion of this coast. A time series of net sediment flux for subaerial and nearshore environments has been established for a section of this coast in Florida, and to a lesser extent, Mississippi. The data incorporate the morphological signature of six tropical storms/hurricanes and more than 200 frontal passages.
Data indicate that (1) barrier islands can conserve mass during catastrophic hurricanes (e.g., Hurricane Opal, a strong category 4 hurricane near landfall); (2) less severe hurricanes and tropical storms can promote rapid dune aggradation and can contribute sediment to the entire barrier system; (3) cold fronts play a critical role in the poststorm adjustment of the barrier by deflating the subaerial portion of the overwash terrace and eroding its marginal lobe along the bayside beach through locally generated, high frequency, steep waves; and (4) barrier systems along the northern Gulf do not necessarily enter an immediate poststorm recovery phase, although nested in sediment-rich nearshore environments. While high wave energy conditions associated with cold fronts play an integral role in the evolution and maintenance of barriers along the northern Gulf, these events are more effective in reworking sediment after the occurrence of extreme events such as hurricanes. This relationship is even more apparent during the clustering of tropical cyclones.
It is anticipated that these findings will have important implications for the longer term evolution of barrier systems in midlatitude, microtidal settings where the clustering of storms is apparent, and winter storms are significant in intensity and frequency along the coast. 相似文献