Water Movements in lakes during Summer Stratification; Evidence from the Distribution of Temperature in Windermere: Appendix: Oscillations in a Three-Layered Stratified Basin
Water Movements in lakes during Summer Stratification; Evidence from the Distribution of Temperature in Windermere: Appendix: Oscillations in a Three-Layered Stratified Basin
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夏季分层期间湖泊中的水运动；
DOI：
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发表时间：
1952
期刊：
影响因子：
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通讯作者：
M. Longuet
中科院分区：
文献类型：
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作者：
M. Longuet
考虑一个长度为l、深度为h的矩形盆地，在平衡状态下，该盆地包含三个水平流体层，流体层的密度分别为p1、p2和p3，深度分别为h1、h2和h3。(The后缀1、2和3分别指上层、中层和下层。取直角坐标（x，y，z），原点位于盆地一端的上表面，x轴水平，z轴垂直向下。假设运动是二维的，与y坐标无关。
Consider a rectangular basin of length l and depth h which, in equilibrium, contains three horizontal layers of fluid of different densities p 1, p 2 and p 3 and of depths h 1, h 2 and h 3. (The suffixes 1, 2 and 3 refer to the upper, middle and lower layers respectively.) Let rectangular co-ordinates ( x , y , z ) be taken with the origin in the upper surface at one end of the basin, the x -axis horizontal and the z -axis vertically downwards. The motion will be assumed to be two-dimensional and independent of the y -co-ordinate.